ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 1970-1974  (755,910)
Collection
Language
Years
Year
  • 1
    Publication Date: 2024-04-20
    Keywords: Atlantic Ocean; Atomic absorption spectrometry (AAS); Cobalt; Copper; Discoverer (1966); DISTANCE; Distance, maximum; Distance, minimum; Dredge; Dredge, chain bag; DRG; DRG_C; Event label; Iron; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; T3-71D 254-15; T3-72D 253-13; T3-72D 255-19; TAG1971; TAG1971-15; TAG1972; TAG1972-13; TAG1972-19; Trans-Atlantic Geotraverse 1971; Trans-Atlantic Geotraverse 1972
    Type: Dataset
    Format: text/tab-separated-values, 68 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-04-19
    Type: Report , NonPeerReviewed
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2024-04-18
    Type: Thesis , NonPeerReviewed
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2024-04-16
    Keywords: Atomic absorption spectrometry (AAS); Calculated from weight loss after ignition at 450 °C; Carlsberg Ridge; Chromium; Cobalt; Copper; D16; D6249; D6252; D6253; D6256; D6257; D6263; D6269; D6271; D6273; Deposit type; DEPTH, sediment/rock; Discovery (1962); Dredge, rock; DRG_R; Event label; Grab; GRAB; Identification; Indian Ocean, Carlsberg Ridge; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Lead; Loss on ignition; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample code/label; Silicon dioxide; Titanium; Vanadium; X-ray fluorescence (XRF); Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 3111 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2024-04-16
    Keywords: 2P-50; 5-37; ABR_Cruise7; ABR7_375-G; Agassiz; AMPH-006D; AMPH-007D; AMPH-009D; AMPH01AR; AMPH01AR-006D; AMPH02AR-007D; AMPH02AR-009D; AMPHITRITE; ANTIPODE; Anton Bruun; ANTP04MV-058D; ANTP-058D; Argo; Cerium; Cobalt; Deposit type; DEPTH, sediment/rock; Description; DNWB0ABD; DODO; DODO-009D-1; DODO-011D; DODO-015D-1; DODO-113D; DODO-127D; DOWNWIND-B1; DOWNWIND-H; Dredge; Dredge, chain bag; Dredge, rock; DRG; DRG_C; DRG_R; DRILL; Drilling/drill rig; DWBD4; DWHD16; DWHD47; DWHD72; Elevation of event; Europium; Event label; FANB01BD; FANBD-20D; FANBD-25D; FANFARE-B; File name; GC; Glomar Challenger; Grab; GRAB; Gravity corer; GSS_537_551; Horizon; Identification; Indian Ocean; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Lanthanum; Latitude of event; Leg5; Longitude of event; Lutetium; MDPC02HO-036P; MDPC03HO-MP-043D; Melville; Method/Device of event; MIDPAC; MPC-36P; MPC-43D; Neodymium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/HILL; Pacific Ocean; PC; PIP-MUS-11; PIP-MUS-21; PIP-NNN; Piston corer; PROA; PROA-072D; Prospector; Prospector-63; Samarium; SAN_JUAN_1963; SB930001; SB930001-1D; SCAN; SCAN-035D; SCAN04AR-035D; Silas Bent; SNJ-DH5; SNJ-DH6; SNJ-DH9; Spencer F. Baird; STYX_I; STYX01AZ; STYX01AZ-003FF; STYXI-3FF; Terbium; Thomas G. Thompson (1964); TT028; TT028-17; TT028-3; Uniform resource locator/link to image; Western Pacific Ocean; Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 429 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2024-04-16
    Keywords: 71022; Aluminium; Arsenic; Calcium carbonate; DEPTH, sediment/rock; Description; Event label; FFGR; Free-fall grab; HUD71/22; HUD71/22-343; HUD71/22-355; HUD71/22-389; HUD71/22-397; HUD71/22-403; HUD71/22-412; HUD71/22-414; HUD71/22-426; HUD71/22-434; HUD71/22-450; HUD71/22-457; HUD71/22-462; HUD71/22-468; HUD71/22-482; HUD71/22-491; Hudson; Identification; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Manganese; Mercury; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic; Sediment type; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 135 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2024-04-16
    Keywords: CHA-252; CHA-281; Challenger1872; Cobalt; Copper; Description; Event label; Grab; GRAB; H.M.S. Challenger (1872); Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Sample ID; Silicon; Titanium; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2024-04-16
    Keywords: Arabian Sea; Atomic absorption spectrometry (AAS); Beryllium; Boron oxide; Calcium oxide; Calculated from weight/volume; Carbon, organic, total; Carbon dioxide; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Gallium; Gravity corer (Kiel type); IIOE - International Indian Ocean Expedition; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Machhera; Magnesium oxide; Manganese oxide; MH_3; MH_3SK; MH65; Niobium; Nitrogen, total; Phosphorus pentoxide; Quartz; Silicon dioxide; SL; Strontium oxide; Titanium dioxide; Vanadium; Water content, wet mass; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 203 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi vol. 7 no. 2, pp. 281-288
    Publication Date: 2024-04-02
    Description: Verschiedene Arten, die in der Literatur mit Leptonia babingtonii in Beziehung gebracht worden sind, werden hier aufs neue geprüft.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-25
    Description: research
    Keywords: Data Analysis ; Data Synthesis ; Forest Ecosystems
    Language: English
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 11
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-25
    Description: research
    Keywords: Hochschulschrift
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 12
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-25
    Description: research
    Keywords: Modelling of Bioelement Cycling ; Beech Forest ; Solling District ; Ecosystem Models ; Input of Chemical Elements
    Language: English
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 13
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-22
    Description: research
    Keywords: Fotochemische Reaktion ; Fotochemie Hydroxyzimtsäuren ; Fotochemische Reaktion ; Hydroxyzimtsäuren
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 14
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-22
    Description: Die Frage des oberirdischen Abbaues von Ernterückständen und der natürlichen Inkorporation organischer Reste in den Boden ist in verschiedener Hinsicht von Bedeutung: 1.) Besonders in schluffigen Böden mit geringer Luftversor gung kann es bei mechanischer Einarbeitung von organische.n Massen - und zwar sowohl von Rübenblatt wie von Stroh - zur Auslösung reduzierender Milieubedingungen mit sehr nachteiligen Folgen für den C- und N-Haushalt und den biologischen Zustand des Bodens kommen.Durch oberflächliche Vorrotte oder Totalabbau ließen sich u.U. derartige nachteilige Wirkungen umgehen. 2.) Durch oberflächliche Verrettung kann u.u. die für sandige Böden wichtige Bildung von Moderhumus - d.h. koprogenen Humusköpern - gefördert werden, da die Moderhumus erzeugenden Organismen (z.B. Oribatiden) bevorzugt in organischen Auflagedecken tätig sind . 3.) Im bearbeitungsfreien Ackerbau stellen d·ie oberflächliche Verrettung organischer Reste und ihre natürliche Inkorporation in den Boden einen der wenigen Wege für die Beseitigung von Ernterückständen dar. Zu untersuchen, ob er gangbar und nutzbringend ist und wie und mit welcher Geschwindigkeit Abbau bzw. Bodeninkorporation erfolgen, ist Aufgabe der nachfolgenden Untersuchungen.
    Description: research
    Keywords: natürliche Bodeninkorporation ; Ertrags- wirkungen von Ernterückstandsdecken
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 15
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-22
    Description: research
    Keywords: Eigenschaften und Dynamik eines Waldstandortes ; immergrünen tropischen Regenwaldes ; mittleren Magdalenatal ; Kolumbien
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 16
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-11
    Description: research
    Keywords: Aue ; Bodengesellschaft ; Physikochemische Bodeneigenschaft ; Bodenanalyse ; Bodenentwicklung ; Leinegraben
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 17
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-11
    Description: research
    Keywords: Niederschlagswasser ; Bioelement-Transport ; Kalkanreicherungs-Horizonten
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 18
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-11
    Description: research
    Keywords: Landschaft bei Hildesheim ; Haushalt der Löss-Schwarzerde ; Bodenwasser
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 19
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-11
    Description: research
    Keywords: Latosol ; Physikochemische Bodeneigenschaft ; Stoffübergang ; Wechselfeuchte Tropen ; Immerfeuchte Tropen ; Nigeria ; Sudan ; Afrika
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 20
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-11
    Description: research
    Keywords: LATEINAMERIKA ; HAUPTNÄHRSTOFFE ; BÖDEN DER TROPEN
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 21
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-10
    Description: research
    Keywords: Physikochemische Bodeneigenschaft ; Schwarzpappel ; Zuwachs
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 22
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-10
    Description: research
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 23
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-10
    Description: research
    Keywords: Feldversuch ; Humusboden ; Bodenbearbeitung Ackerboden ; Umbruch ; Ungesättigte Zone ; Parabraunerde ; Lössboden ; Niedersachsen
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 24
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-10
    Description: research
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 25
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-10
    Description: Für die quantitative Aufschlüsselung der verschiedenen Stickstoff-fraktionen des Bodens bieten sich u. a. die von BREINER et al. (1,2,3,8,18) ausgearbeiteten metheden en, die auf dem Destillations- Verfahren nach Kjeldahl beruhen. Oie vorliegende Arbeit soll diese metheden einer kritischen experimentellen Prüfung und Erweiterung unterwerfen mit dem Ziel, sie für die Erfassung des jah~eezeitlichen Ganges der N-Umverteilung, des N-Haushaltes und der N-Bilanz im Boden anwendbar zu machen. Dabei soll insbesondere die methodische Kombination der chemischen fraktionierung mit der msseenspektrometrischen Analyse markierter N-Verbindungen im Vordergrund stehen.
    Description: research
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 26
    Publication Date: 2024-03-08
    Description: Über einen 60 Jahre laufenden Feldversuch zur Frage der Optimierung des pH−Wertes in Hochmoorböden bei Grünlandnutzung wird berichtet. Wesentliche Ergebnisse sind: 1. Für einen nachhaltig optimalen Ertrag und gute Futterqualität sind pH-Werte (CaCl2) zwischen 4,0-4,5 anzustreben und durch Nachkalkungen zu erhalten. Durch physiologisch alkalische Düngung entwickeln sich die pH-Werte auch ohne Kalkung in diesem pH-Bereich und bleiben langfristig stabil. Physiologisch saure Düngung dagegen führt innerhalb weniger Jahre zu pH-Absenkungen, die − auch wenn sie die Torfsubstanz besser schonen − zu Grünlandumbruch mit periodischen Nachkalkungen zwingen. 2. Physiologisch alkalische Düngung bewirkt über alle pH-Stufen hinweg eine annähernd gleich hohe, im Vergleich zur physiologisch sauren Düngung aber stärkere Humifizierung. Um 10% höhere Torfschwundraten werden über erhöhte Aschegehalte, engeres C/N-Verhältnis und höhere Kationenaustauschkapazität nachgewiesen. Insgesamt entstehen humuschemische Eigenschaften, wie sie von Niedermooren bekannt sind. Mit der erhöhten Düngeintensität sind die Torfverluste auch beim Dauergrünland ähnlich hoch wie beim Ackerbau. 3. Bei der Phosphat-Düngung ist es langjährig gelungen, eine bilanzierte Düngung nach Entzug einzurichten. Phosphate werden mit abnehmendem pH-Wert mobiler und damit auswaschungsgefährdet. Die Kaliumbilanz ist deutlich negativ. Eine PK-Anreicherung im Boden ist durch Düngung nicht möglich. Entzugsdüngung ist zu empfehlen. 5-7 mg P2O5/100 ml und 5-7 mg K2O/1OO ml sind als Versorgungsstufe C anzusehen.
    Description: Results of a 60 years long field trial on cultivated raised-bog under grassland are discussed: The pH-value of cultivated raised-bog should be rised to 4,0-4,5 (CaCl2) when grassland farming. Best effects are given by alkaline fertilizing, thereby the pH-value can be nearly conserved, on the other hand acid fertilizing effects sinking of the pH-value. Alkaline fertilizing causes more intense humification rates up to 10% compared with acid fertilizing. The peat soil of the crumb becomes similar to fen peat and the decomposition increases. The sorption capacity of these peat soils is very high. A content of 5-7 mg P2O5 and 5-7 mg K2O per 100 ml is sufficient for the top soil; when fertilizing more phosphate and potassium their leaching increases.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:631.4 ; ddc:900 ; Moor ; Torf
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 27
    facet.materialart.
    Unknown
    In:  Herausgeberexemplar
    Publication Date: 2024-03-07
    Description: Anläßlich der Jahreshauptversammlung 1973 in Bad Wurzach wird erstmals Mitgliedern der DGMT die C.A.WEBER-Medaille verliehen. Mit dieser Verleihung werden die hervorragenden Verdienste des weltweit anerkannten Moorforschers Prof. Dr. WERNER BADEN gewürdigt, der sich im Sinne der DGMT-Satzung "um die Moor- und Torfkunde verdient gemacht hat".
    Description: editorial
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:554 ; Laudatio ; Moor ; Torf
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 28
    Publication Date: 2024-03-06
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:630.914 ; ddc:333 ; ddc:631.4 ; ddc:581.7 ; Moor ; Torf ; Landnutzung ; Bodenkunde ; Vegetation ; peatland ; peat ; land use ; soil
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 29
    facet.materialart.
    Unknown
    In:  Herausgeberexemplar
    Publication Date: 2024-03-06
    Description: Grünland auf kultiviertem Hoch- und Niedermoor wurde auf seine unterirdische Pflanzenmasse (Wurzeln, Rhizome) untersucht. Dabei zeigte sich insgesamt gesehen eine sehr geringe Durchwurzelungsintensität bei allen untersuchten Arten (Poa trivialis, Poa pratensis, Holcus lanatus, Juncus effusus, Ranunculus acer), die 1% nicht überschreitet. Eine Ausnahme macht nur die oberste Schicht (0-2 cm) des Hochmoorgrünlandes, in dem Wurzelvolumina von 9,6% erreicht werden. Mögliche Ursachen dieses Phänomens werden diskutiert.
    Description: The underground biomass (roots, rhizomes) of grassland situated in a fen and a bog was investigated. Only few roots were found. The content was generally less than 1%. An exception made the surface layer (0-2 cm) of the bog-grassland. There the root content was 9,6%. Possible reasons of this phenomenon were discussed.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:581.7 ; Moor ; Torf ; Vegetation ; Wurzeln ; peatland ; peat ; roots
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 30
    facet.materialart.
    Unknown
    In:  Herausgeberexemplar
    Publication Date: 2024-03-06
    Description: In den oberflächennahen Schichten eines Nieder- und eines Hochmoores wurden die Wurzelvolumina (Rhizome eingeschlossen) von zwei dort jetzt wachsenden Pflanzenarten bestimmt. Hierbei handelte es sich um Deschoampsia caespitosa (Niedermoor) und Narthecium ossifragum (Hochmoor). Dabei ergab sich für jede Art ein typisches Wurzelbild. Besonders auffällig war, daß gerade eine Art des unkultivierten Hochmoores besonders umfangreiche Wurzelanteile aufwies. Die Abnahmen der unterschiedlichen Pflanzenmassen vollziehen sich nicht nur kontinuierlich von oben nach unten, sondern verlaufen auch teilweise unregelmäßig. Die Maxima erscheinen in den beiden obersten Schichten. Bei Deschampsia caespitosa wird für die oberste Schicht ein überwiegend waagerechter Verlauf der Wurzeln sichtbar; Narthecium ossifmgum zeigt mit vorwiegend senkrechter Durchwurzelung in dieser Lage das Gegenteil. In die Untersuchungen wurden nur lebende Wurzeln einbezogen.
    Description: Roots investigations of surface layer were made in a fen and a bog. The volume of the roots of species Deschampsia caespitosa and Narthecium ossifragum were determined. A typical root-distribution was found for each species. The greatest volume of the roots showed Narthecium ossifragum, which growed in a bog. The decrease of the roots occures both proportionately and disproportionately. The maximum appears in the uppermost layer. In this layer prevailed roots in horizontal direction of Descbampsia caespitosa and in vertical direction of Narthecium ossifmgum. Only living rotts were inquired.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:581.7 ; Moor ; Torf ; Wurzeln ; Vegetation ; peatland ; peat ; roots
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 31
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-03-06
    Keywords: Abies; Acer negundo; Acer rubrum-type; Acer saccharum-type; Alnus; Ambrosia; Amorpha; Apiaceae undifferentiated; Arceuthobium; Artemisia; Asteraceae undifferentiated; Betula; Boraginaceae; Botrychium; Brasenia schreberi; Brassicaceae; Bupleurum-type; Carya; Caryophyllaceae; Castanea; Celtis; Cephalanthus; Chenopodiaceae; Cornus amomum-type; Cornus undifferentiated; Corylus; Counting, palynology; Cupressaceae-type; Cyperaceae; DEPTH, sediment/rock; Elaeagnus; Ephedra trifurca-type; Ericaceae; Eriogonum; Euphorbia subgen. Chamaesyce-type; Euphorbia-type; Fabaceae undifferentiated; Fagus; Fraxinus nigra-type; Fraxinus pennsylvanica-type; Gleditsia; Heteranthera; Humulus; Illinois, United States of America; Indeterminata; Iva annua-type; Juglans; Larix; Liquidambar; Livingstone piston sampler; LPS; Lycopodiaceae; Lysimachia; Lythrum; Mentha-type; Morus; Myrica; Myriophyllum; Nuphar; Nymphaea; Nyssa; Onagraceae; Osmunda cinnamomea; Ostrya; Parnassia; Parthenocissus; PBBVANDA; Petalostemum; Picea; Pinus; Pittsburg_Basin; Plantago major-type; Plantago undifferentiated; Platanus; Poaceae undifferentiated; Polemonium; Pollen and spores, other; Polygonella; Polygonum amphibium-type; Polygonum aviculare-type; Polygonum persicaria-type; Polypodiophyta undifferentiated; Potamogeton subgen. Potamogeton-type; Potentilla-type; Pteridium; Quercus; Ranunculaceae undifferentiated; Ranunculus subgen. Batrachium-type; Ranunculus-type; Rhus; Rosaceae undifferentiated; Rubiaceae undifferentiated; Rumex; Sagittaria; Salix; Sarcobatus vermiculatus; Scrophulariaceae; Shepherdia canadensis; Sparganium-type; Thalictrum; Tilia; Tsuga; Typha latifolia-type; Ulmus; Urtica; Utricularia; Viburnum lentago; Viburnum undifferentiated; Vitis; Xanthium; Zea mays
    Type: Dataset
    Format: text/tab-separated-values, 8112 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 32
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-03-06
    Keywords: Alismataceae; Brasenia; Carex subgen. Eucarex; Carex subgen. Vignea; Ceratophyllum demersum; Characeae; Chenopodium rubrum-type; Counting, palynology; Cyperus erythrorhizos; Cyperus odoratus-type; Cyperus strigosus; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eleocharis obtusa; Eupatorium; Gramineae undifferentiated; Hemicarpha micrantha; Heteranthera dubia; Illinois, United States of America; Livingstone piston sampler; LPS; Lycopus; Najas flexilis; Najas gracillima; Najas guadalupensis; Nuphar; PBBVANDA; Physalis; Pittsburg_Basin; Polygonum lapathifolium; Polygonum pennsylvanicum; Potamogeton; Scirpus acutus-type; Scirpus fluviatilis; Setaria glauca; Typha; Zannichellia palustris
    Type: Dataset
    Format: text/tab-separated-values, 2232 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 33
    Publication Date: 2024-03-06
    Keywords: Alismatcaceae; Brasenia; Carex sect. Eucarex; Chara; Compositae undifferentiated; Counting, palynology; Cyperus cf. strigosus; Cyperus erythrorhizos; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eleocharis; Epilobium; Eupatorium; Glyceria; Illinois, United States of America; Livingstone piston sampler; LPS; Najas guadalupensis; Nymphaea; Polygonum lapathifolium; Polygonum pennsylvanicum; Pontederia cordata; Populus, bud scales; Potamogeton friesii; Potamogeton pusillus; Potamogeton sp.; Ranunculus; Rubus; Scirpus acutus-type; Scirpus fluviatilis; SEMBASIN; Seminary_School_Basin; Typha; Verbena
    Type: Dataset
    Format: text/tab-separated-values, 1032 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 34
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-03
    Description: research
    Keywords: Biologische Abwasserreinigung ; Seebinse ; Bodenchemie ; Volumenmessung ; Ton
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 35
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Horn, D R; Delach, M N; Horn, B M (1973): Metal content of ferromanganese deposits of the oceans. Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York, Technical Report, Office for the International Decade of Ocean Exploration, National Science Foundation, Washington, D. C. 20050 (unpublished manuscript) https://www.ngdc.noaa.gov/mgg/geology/data/multiple_platforms/0199/01995002/01995002.pdf, 3 (NSF GX-33616), 78 pp (pdf 3 MB), https://store.pangaea.de/Projects/NOAA-MMS/Horn-etal_1973.pdf
    Publication Date: 2024-02-29
    Description: A compilation of published and unpublished chemical analyses of samples of ferromanganese deposits from the ocean floor reveals that only in relatively few areas of the world are the copper and nickel contents sufficiently high for the nodules to represent a potential source of metals. The North and South Atlantic and Indian Oceans are characterized by deposits whose metal content (Cu, Ni, Mn and Co) are well below the minimum values necessary for economic exploitation. The situation is more favorable in the Pacific Ocean and most encouraging in the North Pacific. In the South Pacific, nodules containing over 1% Ni and lesser amounts of copper occur in the Peru Basin, in deep waters east of the Marquesas Islands and Tuamotu Plateau, and within the Southwest Pacific Basin. The relatively low Cu and Ni values obtained in these areas may eliminate them as prospective mining sites. Only in the North Pacific do the analyses consistently show values greater than 1% Cu and 1% Ni, and these nodules, therefore, are the immediate target of the ocean mining industry. The deposits of interest lie north of the equator in a broad band between 6° 30' N and 20° N and stretching from 110° W to 180° W. Maximum copper and nickel values occur along a line 8° N to 10° 30'N and 131°3 0'W to 145° W.
    Keywords: Atlantic Ocean; Dredge; Dredge, rock; DRG; DRG_R; Indian Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; RC05; RC05-1RD; RC08; RC08-143; RC08-82; RC08-83; RC08-84; RC08-8RD; RC08-99; RC09; RC09-123; RC09-88; RC10; RC10-110; RC10-153; RC10-176; RC10-5; RC10-76; RC10-91; RC10-93; RC11; RC11-100; RC11-102; RC11-104; RC1112; RC11-12RD; RC11-132TW; RC11-13RD; RC11-14RD; RC11-15RD; RC11-17RD; RC11-18RD; RC11-19RD; RC11-206; RC11-20RD; RC11-21RD; RC11-22RD; RC11-24RD; RC11-25RD; RC11-39; RC11-39TW; RC11-3RD; RC11-5RD; RC11-98; RC12; RC12-129; RC12-187; RC12-188; RC12-193; RC12-195; RC12-197; RC12-198; RC12-200; RC12-216; RC12-218; RC12-220; RC12-224; RC12-228; RC12-302; RC12-47; RC12-50; RC12-58; RC12-59; RC12-69; RC12-79; RC13; RC13-15; RC13-18; RC13-19; RC13-279; RC13-58; RC13-5RD; RC13-66; RC13-70; RC13-72; RC13-73; RC13-74; RC13-75; RC14; RC14-49; RC14-4RD; RC15; RC15-1RD; Robert Conrad; Southern Ocean; TC; TRAWL; Trawl net; Trigger corer; V15; V15-119SBT; V15-120SBT; V15-121SBT; V15-122SBT; V15-135SBT; V15-72SBT; V16; V16-19SBT; V16-29SBT; V16-35SBT; V16-3SBT; V17; V17-40SBT; V17-83SBT; V17-84SBT; V18; V18-10RD; V18-11RD; V18-1BBD; V18-29RD; V18-30RD; V18-32RD; V18-4BBD; V18-5BBD; V18-6RD; V19; V19-11RD; V19-166; V19-1RD; V19-2RD; V19-305; V19-80; V20; V20-178; V20-180; V20-31; V20-36; V20-44; V20-48; V20-4RD; V20-5RD; V20-72; V21; V21-10RD; V21-199; V21-2RD; V21-8RD; V22; V22-102; V22-111; V22-118; V22-122; V22-123; V22-127; V22-136; V22-139; V22-147; V22-148; V22-150; V22-151; V22-184; V22-50; V22-52; V22-54; V22-7RD; V23; V23-135; V24; V24-100; V24-102; V24-199; V24-1BT; V24-210; V24-214; V24-218; V24-237; V24-250; V24-251; V24-77; V25; V25-13RD; V25-14RD; V25-6; V25-9RD; V26; V26-159; V26-1RD; V26-27; V26-3; V26-66; V27; V27-133; V27-138; V27-202; V27-222; Vema
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 36
    Publication Date: 2024-02-29
    Keywords: Aluminium; Atlantic Ocean; Barium; Boron; Cadmium; Calcium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; Identification; Indian Ocean; Iron; Latitude of event; Lead; Longitude of event; Magnesium; Manganese; Method/Device of event; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Phosphorus; Piston corer; Potassium; RC05; RC05-1RD; RC08; RC08-143; RC08-82; RC08-83; RC08-84; RC08-8RD; RC08-99; RC09; RC09-123; RC09-88; RC10; RC10-110; RC10-153; RC10-176; RC10-5; RC10-91; RC10-93; RC11; RC11-100; RC11-102; RC11-104; RC1112; RC11-12RD; RC11-132TW; RC11-13RD; RC11-14RD; RC11-15RD; RC11-17RD; RC11-18RD; RC11-19RD; RC11-206; RC11-20RD; RC11-21RD; RC11-22RD; RC11-24RD; RC11-25RD; RC11-39TW; RC11-3RD; RC11-5RD; RC11-98; RC12; RC12-129; RC12-187; RC12-188; RC12-195; RC12-197; RC12-198; RC12-200; RC12-216; RC12-218; RC12-220; RC12-224; RC12-228; RC12-47; RC12-50; RC12-58; RC12-59; RC12-69; RC12-79; RC13; RC13-18; RC13-58; Robert Conrad; Scandium; Shape; Silicon; Sodium; Southern Ocean; Strontium; TC; Thallium; Thorium; Tin; Titanium; TRAWL; Trawl net; Trigger corer; V15; V15-119SBT; V15-120SBT; V15-121SBT; V15-122SBT; V15-135SBT; V15-72SBT; V16; V16-19SBT; V16-29SBT; V16-35SBT; V16-3SBT; V17; V17-40SBT; V17-83SBT; V17-84SBT; V18; V18-10RD; V18-11RD; V18-1BBD; V18-29RD; V18-30RD; V18-32RD; V18-4BBD; V18-5BBD; V18-6RD; V19; V19-166; V19-1RD; V19-2RD; V19-305; V19-80; V20; V20-178; V20-180; V20-36; V20-44; V20-48; V20-4RD; V20-5RD; V20-72; V21; V21-10RD; V21-199; V21-2RD; V21-8RD; V22; V22-102; V22-111; V22-118; V22-122; V22-123; V22-127; V22-136; V22-139; V22-147; V22-148; V22-150; V22-151; V22-184; V22-50; V22-52; V22-54; V22-7RD; V23; V23-135; V24; V24-100; V24-102; V24-199; V24-1BT; V24-210; V24-214; V24-218; V24-237; V24-250; V24-251; V24-77; V25; V25-6; V26; V26-159; V26-27; V26-3; V26-66; Vema; Wet chemistry; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 1892 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 37
    Publication Date: 2024-02-29
    Keywords: Atlantic Ocean; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; Identification; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; RC10; RC10-5; RC11; RC11-100; RC11-102; RC11-104; RC1112; RC11-12RD; RC11-132TW; RC11-13RD; RC11-14RD; RC11-15RD; RC11-17RD; RC11-18RD; RC11-19RD; RC11-206; RC11-20RD; RC11-21RD; RC11-22RD; RC11-24RD; RC11-25RD; RC11-39; RC11-39TW; RC11-3RD; RC11-5RD; RC11-98; RC12; RC12-129; RC12-187; RC12-188; RC12-193; RC12-195; RC12-197; RC12-198; RC12-200; RC12-216; RC12-218; RC12-220; RC12-224; RC12-228; RC12-302; RC12-47; RC12-50; RC12-58; RC12-59; RC12-69; RC12-79; RC13; RC13-15; RC13-18; RC13-19; RC13-279; RC13-58; RC13-5RD; RC13-66; RC13-70; RC13-72; RC13-73; RC13-74; RC13-75; RC14; RC14-49; RC14-4RD; RC15; RC15-1RD; Robert Conrad; Sediment type; Size; Southern Ocean; Substrate type; TC; Trigger corer; V15; V15-121SBT; V15-72SBT; V17; V17-40SBT; V17-83SBT; V17-84SBT; V18; V18-1BBD; V18-4BBD; V18-5BBD; V20; V20-178; V20-180; V20-31; V20-36; V20-44; V20-48; V20-4RD; V20-5RD; V20-72; V21; V21-10RD; V21-199; V21-2RD; V21-8RD; V22; V22-102; V22-111; V22-118; V22-122; V22-123; V22-127; V22-136; V22-139; V22-147; V22-148; V22-150; V22-151; V22-184; V22-50; V22-52; V22-54; V22-7RD; V23; V23-135; V24; V24-100; V24-102; V24-199; V24-1BT; V24-210; V24-214; V24-218; V24-237; V24-250; V24-251; V24-77; V25; V25-13RD; V25-14RD; V25-6; V25-9RD; V26; V26-159; V26-1RD; V26-27; V26-3; V26-66; V27; V27-133; V27-138; V27-202; V27-222; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 3074 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 38
    Publication Date: 2024-02-29
    Keywords: Aluminium; Atlantic Ocean; Atomic absorption spectrometry (AAS); Barium; Calcium; Carbon, total; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; Identification; Indian Ocean; Iron; Latitude of event; Lead; Longitude of event; Magnesium; Manganese; Method/Device of event; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Phosphorus; Piston corer; Potassium; RC05; RC05-1RD; RC08; RC08-8RD; RC10; RC10-76; RC10-91; RC10-93; RC11; RC11-102; RC1112; RC11-3RD; RC12; RC12-129; RC12-193; RC12-302; RC13; RC13-15; RC13-19; RC13-279; RC13-5RD; RC13-66; RC13-70; RC13-72; RC13-73; RC13-74; RC13-75; RC14; RC14-49; RC14-4RD; Robert Conrad; Shape; Silicon; Sodium; Southern Ocean; Strontium; Thallium; Tin; Titanium; TRAWL; Trawl net; V15; V15-120SBT; V15-135SBT; V15-72SBT; V16; V16-19SBT; V16-3SBT; V17; V17-40SBT; V17-83SBT; V17-84SBT; V18; V18-10RD; V18-11RD; V18-6RD; V19; V19-11RD; V19-305; V20; V20-31; V21; V21-2RD; V22; V22-118; V22-123; V22-139; V22-147; V22-148; V22-150; V22-151; V22-184; V22-50; V22-52; V22-54; V22-7RD; V24; V24-210; V24-218; V24-250; V24-251; V25; V25-13RD; V25-14RD; V25-9RD; V26; V26-159; V26-1RD; V26-27; V26-3; V27; V27-133; V27-138; V27-202; V27-222; Vema; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 872 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 39
    Publication Date: 2024-02-28
    Description: Am Schluß einer Tagung stellen sich Veranstalter und Teilnehmer immer die Frage: waren Thema, Ort und Programme so, dass der gesamte Aufwand und manches persönliche Opfer gelohnt haben? Bei allen gegensätzlichen Auffassungen über die Nutzung eines Moores - sei es landwirtschaftlich, forstwirtschaftlich und torfwirtschaftlich oder auch für die zunehmenden Ansprüche des Naturschutzes und der Landschaftspflege - muß immer das Kennenlernen des anderen Standpunktes an erster Stelle stehen. In Papenburg ging es um die Frage, ob Moore in einer relativ waldarmen Niederungslandschaft nach ihrer Teilabtorfung oder bei ihrer Aufgabe als landwirtschaftliche Nutzfläche nicht besser aufgeforstet als sich selber überlassen werden sollten. Diese Fragestellung ist bei wachsendem Umweltbewußtsein der Bevölkerung höchst aktuell. Papenburg - als eine alte bäuerliche Fehnkolonie und heute Standort mehrerer Torfwerke - bot sich deshalb als Tagungsort an. [...]
    Description: conference
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:333.72 ; ddc:631.4 ; Moor ; Torf ; Tagungsbericht ; peatland ; peat ; conference report
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 40
    facet.materialart.
    Unknown
    In:  Herausgeberexemplar
    Publication Date: 2024-02-28
    Description: Die Bodenentwicklung aus Niedermoortorfen und Hochmoortorfen verläuft abhängig von der Kultivierung unterschiedlich schnell. Sie hat physikalisch ungünstige, chemisch günstige Eigenschaften der Moorböden zur Folge. Deshalb sind nach der 1. Kultivierung in zeitlichen Abständen weitere Maßnahmen der Rekultivierung erforderlich, damit ein modernen Nutzungsansprüchen zugänglicher Pflanzenstandort erhalten bleibt. Geeignete Rekultivierungsverfahren werden vorgestellt: Für flachgründige Niedermoore die Tiefpflugsanddeckkultur, die Deutsche Sandmischkultur für gealterte Deutsche Hochmoorkulturen und für Leegmoore nach industrieller Abtorfung. Beide Verfahren haben Mehrung und Sicherung der Ackererträge zum Ziel. Für vorübergehenden Einsatz ist pflugloser Ackerbau im Versuchsstadium. Zur Beseitigung von Staunässe haben sich Moorschlitzdränung und Maulwurfdränung bewährt.
    Description: The development of peat soils out of low moor peat and high moor peat depends on the method of cultivation and runs different quickly. It results at least in unfavourable physical conditions and favourable chemical conditions. Therefore after a first cultivation Within several years other methods of recultivation are necessary to keep a stand for plants with modern way of agricultural produce. Suitable methods of recultivation are presented: For flat low moor soils deep ploughing and sand covering method (,,Tiefpflugsanddeckkultur“), the German Cultivation of peat by mixing With sand („Deutsche Sandmischkultur“) for aged German High bog cultivation as well as for industrial cut off bogs. Both methods of recultivation aim at the increase of yield and security of arable land. For transitory use the minimum tillage is to be proved. To avoid water surplus caused by insufficient draining of gravitational water a special method of slitting crumbs of peat soils and forming a mole drain have been approved.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:631.4 ; Moor ; Torf ; Bodenkunde ; peatland ; peat
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 41
    facet.materialart.
    Unknown
    In:  Herausgeberexemplar
    Publication Date: 2024-02-28
    Description: Die im Vergleich zu den alten Moorschutzgesetzen erweiterten Auflagen des neuen niedersächsischen Bodenabbaugesetzes werden in ihren Auswirkungen auf die Abtorfung dargelegt. Über erste Erfahrungen in der Anwendung dieses neuen Gesetzes wird berichtet. Für die noch nicht veröffentlichten Richtlinien für die Durchführung von Abbau und Herrichtung nach dem Bodenabbaugesetz werden für Abtorfungen Vorschläge gemacht. Dabei wird im Hinblick auf die unterschiedlichen Forderungen nach Folgenutzungen unterschieden in Teilabbau und vollständigen Abbau von Hochmooren. Beispiele für Abbau- und Entwässerungstiefe bei nachfolgender Rekultivierung für land- und forstwirtschaftliche Nutzung sowie für die Erholungslandschaft oder die Möglichkeit der Regeneration durch Wiedervernässung und Vermoorung werden diskutiert.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:333.72 ; ddc:631.4 ; ddc:333.7313 ; Moor ; Torf ; Naturschutz ; Landnutzung ; peatland ; peat ; nature conservation ; land use
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 42
    Publication Date: 2024-02-28
    Description: Am 30./3l.5.l972 hatte die Sektion III unter Mitwirkung der Sektionen II und V zu einer weiteren Arbeitstagung Mitglieder und Gäste nach Papenburg eingeladen, um die auf der 2. Sektionssitzung in Heide/Holstein 1971 bereits begonnene Diskussion über die zukünftige Nutzung der Moore fortzusetzen. [...]
    Description: conference
    Description: DFG, SUB Göttingen, DGMT
    Keywords: ddc:553.21 ; ddc:631.4 ; Moor ; Torf ; Tagungsbericht ; peatland ; peat ; conference report
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 43
    facet.materialart.
    Unknown
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 6 no. 9, pp. 156-156
    Publication Date: 2024-02-22
    Description: Spiranthes spiralis (L.) Chevall. op Goeree. Ook in 1972 heeft Spiranthes spiralis op de bekende groeiplaats op Goeree weer rijk gebloeid. Op 2 september 1972 telden wij 993 bloeistengels. Opvallend was een lichte teruggang van het aantal bloeiende exemplaren ten opzichte van 1971 (1142 exx.), alsmede het feit dat de planten in hun ontwikkeling niet zover waren als op 22 augustus 1971, toen dus 11 dagen eerder werd geteld. Voor wijze van telling en beschrijving van het gebied zie Gorteria 5(11), 1971, p. 266\xe2\x80\x94267.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 44
    Call number: AWI G3-24-95571-5
    In: Tektonika Sibiri, Tom 5
    Description / Table of Contents: Сборник докладов VI сессии Научного совета по тектонике Сибири и Дальнего Востока (Новосибирск, декабрь, 1968 г.) включает статьи представителей более 30 научно исследовательских и производственных организаций СССР и состоит из трех разделов. Первый посвящен наиболее общим проблемам тектонического районирования; второй - актуальным вопросам усовершенствования тектонической терминологии и номенклатуры, а также принципов типизации и систематики тектонических объектов разной природы; третий - результатам новейших разработок в области тектонического моделирования.
    Description / Table of Contents: Translation of the abstract The collection of reports of the VI session of the Scientific Council on Tectonics of Siberia and the Far East (Novosibirsk, December, 1968) includes articles by representatives of more than 30 research and production organizations of the USSR and consists of three sections. The first is devoted to the most general problems of tectonic zoning; the second - topical issues of improving tectonic terminology and nomenclature, as well as the principles of typification and systematics of tectonic objects of different nature; the third - the results of the latest developments in the field of tectonic modeling.
    Type of Medium: Monograph available for loan
    Pages: 230 Seiten , Illustrationen
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 5
    Language: Russian
    Note: CONTENTS Principles of Tectonic Zonation On principles of tectonic zonation / Yu. A. Kosygin Methodics of tectonic zonation and mapping / T. N. Spizsharsky Paragenetic analysis of structures, as a base of tectonic mapping and of middle-scale structural mapping of folded regions / A. V. Lukyanov, I. G. Scherba On principles of compiling of middle- and large-scale tectonic maps / I. N. Kazakov On methodics of compiling of regional tectonic maps / A. I. Olly, V. A. Romanov, P. N. Mikhailov To methodics of tectonic mapping of platform oil and gas bearing regions / F. G. Gurary, K. I. Mikulenko, V. S. Staroseltsev Principles of compiling of tectonic map of oil and gas bearing regions of USSR / L. N. Rosanov Notes on tectonic zonation / Ch. B. Borukayev, L. M. Parfyonov Peculiarities of structure of development of arc uplifts, as a base for tectonic and metallogenic zonation / N. A. Fogelman Principles of compiling of tectonic map of Arctic and Subarctic / I. P. Atlasov Principles and methods of tectonic mapping of epypaleozoic platforms / V. S. Bochkarev Some questions of genesis of main fault systems in the south of East Siberia / P. M. Khrenov On problems of zonation of fundament of platforms / L. Ya. Provodnikov, D. V. Puchkova Tectonic terminology, systematics and nomenclature Principles of constructing of tectonic systems of notions, terms and symbols / Yu. A. Kosygin, A. M. Borovikov, V. A. Solovyov Some problems of tectonic nomenclature and systematics / L. I. Krasny The main principles and systems of concepts in the theory of geosynclines / G. S. Gnibidenko, K. S. Shashkin The typification and nomenclature of folded systems in connection with their cyclic development / V. A. Amantov On the evolution of the main types of Earth crust / E. N. Petrov Some regularities of patterns of platform structures, and their systems / V. V. Zabaluev Scheme of morphogenetic classification of deep faults and their terminology / V. A. Dedeev, A. K. Zapol'nov To the problem of classification of deep faults on geological and geophysical indications (on example of the main zones of deep faults in Siberia and Far East) / G. A. Mourzina Typification of fold structures and geotectonic zonation / G.S.Senchenko Types of local structures of geosynclinal and intermediate zones on example of west end of Large Caucasus / A. I. Dyakonov, F. K. Baydov, Yu. D. Kuzmenko Morphogenetic types of local structures of Kempendyay region of salt dislocations / M. K. Weinberg , P. K. Mazaeva, G. S. Fradkin About the terms: "graben", "graben-shape depression", "taphrogeosyncline", "avlakogene" / V. S. Bochkarev Experimental reproduction of tectonic dislocation forms About modern methods of tectonic experiments / I. V. Luchitsky, P. M. Bondarenko, V. I. Gromin, G. D. Ushakov Experimental investigation of conditions of appearing of flow cleavage, in equivalent material / E. I. Patalakha About the possible thermic effect of tectonic deformation of rocks / E. I. Patalakha, V. G. Lee Experimental investigation of deformations, with increasing of volume of the deformations masses / I. V. Kyrillova, E. I. Chertkova Modeling of process of forming of salt structures by solid plastic materials in centrifuge / A. M. Sycheva-Mikhailova New methods of deformation estimations in the models / A. V. Mikhailova About one experiment with investigation of fault systems of globe / V. M. Bourmistenko The mechanizm of forming of Caledonian fundament structure of Minusa depression and its framing (on experimental data) / O. M. Zavgorodsky The stress fields and geologic structures in the south part of Siberian platform and its framing (on modeling data) / V. G. Gladkov, V. P. Nikittn, P. M. Khrenov Deformation of sedimentary rocks under high pressures and temperatures / G. M. Avchan, A. A. Matveenko, Z. B. Stephankevich About tectonophysic analyses of mechanisms of forming of system jointing, on example of Aldan schield / R. I. Grishkyan , СОДЕРЖАНИЕ Принципы тектонического районирования О принципах тектонического районирования / Ю. А. Косыгин Методика составления тектонических карт и принципы тектонического районирования / Т. Н. Спижарский Парагенетический анализ структур как основа тектонического районирования и составления среднемасштабных структурных карт складчатых областей / А. В. Лукьяпов, И. Г. Щерба О принципах еоставления средне- и крупномасштабных тектонических карт / И. Н. Казаков О методике составления региональных тектонических карт / А. И. Олли, В. А. Ромапов, П. Н. Михайлов К методике составления тектонических карт платформенных нефтегазоносных областей / Ф. Г. Гурари, К. И. Микулеико, В. С. Старосельцев Принципы составления тектонической карты нефтегазоносных областей СССР / Л. Н. Розанов Заметки о тектоническом районировании / Ч. Б. Борукаев, Л. М. Парфенов Особенности строения и развития сводовых поднятий как основа для тектонического и металлогенического районирования / Н. А. Фогельман Принципы составления тектонической карты Арктики и Субарктики / И. П. Атласов Принципы и методы тектонического районирования эпипалеозойских платформенных областей / В. С. Бочкарев О некоторых вопросах генезиса главнейших систем разрывов юга Восточной Сибири / П. М. Хренов К проблеме районирования фундамента платформенных областей / Л. Я. Проводпиков, Д. В. Пучкова Тектоническая терминология, систематика и номенклатура Принципы построения систем тектонических понятий, терминов и знаков / Ю. А. Косыгин, А. М. Боровиков, В. А. Соловьев Некоторые проблемы тектонической систематики / Л. И. Красный Основные принципы и системы понятий теории геосинклиналей / Г. С. Гнибидепко, К. С. Шашкин Типизация и номенклатура складчатых систем в связи с цикличностью их развития / В. А. Амантов Об эволюции главных типов земной коры / Е. Н. Петров Некоторые закономерности пространственного размещения платформенных структур и их систематика / В. В. Забалуев Схема морфогенетической классификации глубинных разломов и их терминология / В. А. Дедеев, А. К. Запольиов К проблеме классификации глубинных разломов по геолого-геофизическим признакам (на примере главнейших зон глубинных разломов Сибири и Дальнего Востока) / Г. А. Мурзина Типизация складчатых структур и геотектоническое районирование / Г. С. Сенченко Типы локальных структур геосинклинальной и переходной областей (на примере западного окончания Большого Кавказа) / А. И. Дьяконов, Ф. К. Байдов, Ю. Д. Кузъменко Морфогенетические типы локальных структур Кемпендяйской впадины / М. К. Вейнберг, П. К. Мазаева, Г. С. Фрадкин О терминах "грабен", "грабенообразная впадина", "тафрогеосинклиналь" и "авлакоген" / В. С. Бочкарев Экспериментальное воспроизведение тектонических форм О современных методах тектонического эксперимента / И. В. Лучицкий, П. М. Бондаренко, В. И. Громин, Г. Д. Ушаков Экспериментальное изучение условий возникновения кливажа течения в эквивалентном материале / Е. И. Паталаха О возможном термическом эффекте тектонического деформирования горных пород / Е. И. Паталаха, В. Г. Ли Экспериментальное исследование деформаций связанных сувеличением объема деформируемых масс / И. В. Кириллова, Е. И. Черткова Моделирование процесса формирования соляных структур на твердых пластичных материалах с применением центрифуги / А. М. Сычева-Михайлова Новое в методике оценки деформаций в моделях / А. В. Михайлова Об одном опыте экспериментального изучения разломных структур земного шара / В. М. Бурмистенко Механизм формирования структуры каледонского фундамента Минусинского прогиба и его обрамления (по экспериментальным данным) / О. М. Завгородский Поля напряжений и геологические структуры южной части Сибирской платформы и ее обрамления (по данным моделирования) / В. Г. Гладков. В. П. Никитин, П. М. Хренов Деформации осадочных горных пород под действием высоких давлений и температур / Г. М. Авчян, А. А. Матвеенко, 3. Б. Стефанкевич О тектонофизическом анализе механизма образования системной трещиноватости (на примере Алданского щита) / Р. И. Гришкян , In kyrillischer Schrift
    Location: AWI Reading room
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 45
    facet.materialart.
    Unknown
    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht vol. 395 no. 1, pp. 243-245
    Publication Date: 2024-02-08
    Description: First record of Bryum gemmiparum de Not. from The Netherlands. The taxonomy and distribution of the species are discussed. Bryum gemmiparum was collected in a clay-pit along the river Maas in the north of the province of Limburg. This locality seems to be the northernmost one known of the species. Bryum gemmiparum was found growing on steep, rather humid, loamy soils in a luxuriant cover of bryophytes characterized by Anisothecium varium, Riccardia sinuata, Riccardia pinguis, Bryum bicolor, Didymodon tophaceus, and Mniobryum wahlenbergii. A floristical and ecological investigation of this highly interesting bryophyte vegetation in The Netherlands is needed.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 46
    facet.materialart.
    Unknown
    In:  Flora Malesiana - Series 1, Spermatophyta vol. 7 no. 1, pp. 239-263
    Publication Date: 2024-02-08
    Description: Perennial (rarely annual) herbs, or undershrubs, terrestrial or aquatic, sometimes stoloniferous ( Gunnera). Leaves opposite, spiral, or verticillate, in the terrestrial species nearly always simple, in the aquatic ones always partly pinnately divided, pinnately nerved or (in Gunnera) palmately nerved. Stipules 0, but the leaves often flanked by small, subulate and caducous enations. Flowers mostly in spike-like inflorescences, sometimes in a compound panicle, mostly solitary or (sometimes) in clusters of up to a dozen flowers in the axil of a bract or reduced leaf, \xe2\x99\x80 monoecious, dioecious or polygamous, perigynous, actinomorphous, mostly 4-merous, or 2-, or (not in Mal.) 3-merous. Sepals 4 or 2, rarely (not in Mal.) 3, in \xe2\x99\x80 flowers sometimes much reduced to 0, free or little connate, mostly persistent. Petals alternisepalous, 4, 2 or 0, rarely 3 (not in Mal.), free, in \xe2\x99\x80 flowers absent or strongly reduced, often soon caducous, mostly more or less unguiculate and cochleariform, longer than the sepals. Stamens as many as sepals and then epi- or alternisepalous, or twice as many, 8, 4 or 2, rarely (not in Mal.) 3 fertile and 3 sterile, or 1, in \xe2\x99\x80 flowers completely reduced; filaments mostly filiform, long and very thin, rarely (not in Mal.) short and thick; anthers 2-celled, basifixed, latrorse, mostly oblong to linear, rarely \xc2\xb1 elliptic. Disk 0. Ovary 1- or 4-, rarely 2- or (not in Mal.) 3-celled, in the \xe2\x99\x82 flowers 0 or reduced; style alternisepalous, free, mostly short, grading into the globose or subulate stigmas which spread in fruit, the stigmatic, more-celled papillae hair-like elongating towards the end of the anthesis (except in Gunnera). Ovules as many as styles, or (in Gunnera) single, apical, pendulous, anatropous and apotropous. Fruit nut-like or (in Gunnera) a drupe, variously sculptured, indehiscent 1-seeded or breaking up into 4(-2) 1- seeded mericarps. Seed with a thin testa; embryo cylindrical, surrounded by a thick, white, oily albumen, or (in Gunnera) obcordate and in top of a very copious and oily albumen.\nDistribution. Genera 7, with c. 150 spp., nearly all over the world, but rather rare in the tropics.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 47
    facet.materialart.
    Unknown
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 18 no. 2, pp. 392-392
    Publication Date: 2024-02-08
    Description: In his paper on the peat swamp forests of Sarawak and Brunei (Gard. Bull. 20, 1963, 152) Dr. J. A. R. Anderson made notice of a distinctive Xanthophyllum species which he was not able to identify. In 1968, Mr. F. S. P. Ng, revising the genus for the Manual of Malayan Timber Trees, recognized it as a new species, but did not describe it. Working now on a monograph of the genus, and having examined all collections Dr. Anderson kindly sent on loan to me, I am able to describe it here as a new species.\nI am much indebted to Dr. H. Sleumer for rendering the diagnosis in Latin.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 48
    facet.materialart.
    Unknown
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 18 no. 1, pp. 53-63
    Publication Date: 2024-02-08
    Description: In about 10\xe2\x80\x9415 % of the cases a sharp distinction between Atriplex hastata L., patula L., littoralis L., and glabriuscula Edm. is not possible, both in the field and in the herbarium. In order to establish the status of the \xe2\x80\x98intermediates\xe2\x80\x99 a karyological examination was undertaken of 95 samples collected in the Netherlands including both typical specimens and intermediates. It appeared that the specimens clearly representing A. hastata, littoralis, or glabriuscula are diploid (n = 9), but those representing A. patula tetraploid (n = 18). The \xe2\x80\x98intermediates\xe2\x80\x99 between A. hastata and patula are either diploid or tetraploid. Hence a sharp distinction between the latter two taxa is only possible on the chromosome number. A similar result was found for the \xe2\x80\x98intermediates\xe2\x80\x99 between A. patula and littoralis. It depends on the specific concept one adheres to whether these four taxa should be ranked as species; European botanists usually give them specific rank, their American colleagues infraspecific rank. Autogamy seems to be the rule in these species. This as well as the chromosome numbers found rule out the possibility of hybridization as an explanation for the occurrence of intermediates. I have strong doubts as to the artificial hybrids reported in literature because of the technical difficulties involved and apparently not solved. Special attention has been paid to possible characters to be derived from the leaves, the phyllotaxis, and the bracts. The variation in the leaves of the four species examined is overlapping. The same holds true for the phyllotaxis and the ripe fruits and fruiting bracteoles. An account is given of some abnormalities which have been found during the chromosome countings. An attempt was made to correlate morphological characters of the leaf, especially the leaf-base and leaf-index, and the chromosomes in A. hastata and patula. The results presented in the scatter diagrams show that, though on the whole there is a marked correlation between leafshape and chromosome number, no sharp distinction can be made. Finally a provisional key is given.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 49
    facet.materialart.
    Unknown
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 5 no. 4, pp. 54-60
    Publication Date: 2024-02-08
    Description: Three new adventitious species of Amaranthaceae are recorded for the Netherlands: Gomphrena celosioides Mart., Alternanthera ficoidea (L.) R. Br. ex Grisebach var. bettzickiana (Regel) Backer and an unidentified species of Alternanthera. Of the latter a description is given and the identification is requested. Gomphrena and Alternanthera can be separated as follows: 1. Stigma capitate or shortly ................... 2-lobed Alternanthera 1\xe2\x80\x99. Stigma branches 2, filiform to subulate ................... Gomphrena Gomphrena globosa and G. celosioides are easily recognized by the dorsal crest of the bracteoles. The species of Alternanthera here described can be fitted in the key given by VAN OOSTSTROOM & REICHGELT (1961) in the following manner: 0. Anthers lanceolate to linear; pseudostaminodes ligular with laciniate apex. 00. Bracts and bracteoles ca. \xc2\xbe times as long as the tepals. Outer tepals with 3\xe2\x80\x945 thick nerves at base. Pseudostaminodia \xc2\xb1 as long as the stamens. A. ficoidea var. bettzickiana 00\xe2\x80\x99. Bracts and bracteoles longer than the tepals. Outer tepals at most faintly nerved. Pseudostaminodia shorter than the stamens .................. A. spec. 0\xe2\x80\x99. Anthers ellipsoid; pseudostaminodia narrowly triangular to linear-subulate, entire. 1. Tepals etc.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 50
    facet.materialart.
    Unknown
    In:  Zoologische Verhandelingen vol. 130 no. 1, pp. 1-396
    Publication Date: 2024-02-08
    Description: A systematic study has been made of the Paguridea (exclusive of the Lithodidae) from northwestern North America. In addition to the redescriptions of all known species, two subgenera are herein raised to generic rank and a new genus is described. Several systematic problems have been resolved, and have resulted in the suppression of several specific names familar to North American carcinologists.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 51
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Schrader, Hans-Jürgen (1972): Kieselsäure-Skelette in Sedimenten des ibero-marokkanischen Kontinentalrandes und angrenzender Tiefsee-Ebenen. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C8, 10-36
    Publication Date: 2024-02-03
    Description: Siliceous skeletons were investigated in two core profiles (9 cores), one off Cap de Sines, Portugal and the other off Cap de Mazagan, Morocco. Total number of skeletons was determined per gram of dried sediment at different core depths of the fraction 〉21 µ. Results are compared with a core profile from the Arabian Sea. Diatoms are of four groups: (A) marine-planktonic, B) marine-benthic, (C) freshwater and (D) Tertiary species (Trinacria e.g.). Species from groups (B), (C) and (D) are redeposited in all cores taken at a water depth of greater than 100 m. Small numbers of Silicoflagellates and Radiolarians were found throughout the cores from the Ibero-Moroccan shelf. In the Arabian Sea core, Radiolarians were concentrated in distinct horizons in which Tertiary material was redeposited (40-50, 140-150, 250-260 cm). The number of siliceous skeletons per gram of dried sediment decreases more or less rapidly with increasing depth in all cores. Whereas about 2500 skeletons were found in sediments close to the surface, approximately 100 skeletons only were found in deeper (〉40 cm) layers. Deeper horizons with more than 100 specimens were interpreted as redeposited material. This sediment contained robust skeletons, resistant against dissolution, as well as benthic and Tertiary material. The decrease of siliceous skeletons relative to core depth depends upon the sedimentation rate. Where the sedimentation rate is high, the opal dissolution zone extends down to 30-60 cm, where the sedimentation rate is low, it is located at 10-30 cm. Below these depths opals disappears. These zones also have approximately the same age (4000 years) everywhere. Siliceous skeletons dissolve differentially, first the Silicoflagellates disappear, second the Diatoms, third the Radiolarians, and fourth the Sponge Spicules. Surface structure of skeletons from near the opal dissolution zones are similar to those of skeletons treated with NaOH. Tertiary diatoms (Trinacria e. g.) and benthic diatoms (Campylodiscus e.g.) dissolve less rapidly than skeletons of modern planktonic diatoms (Coscinodiscus e.g.). The time control of the opal dissolution zones appeared rather independent of various oceanic influences. No evidence was found for effects from upwelling either off Portugal or off Morocco. No difference in dissolution rates was recorded between the abyssal plains lying off these two areas. Likewise, there was no change in solution rates from Pleistocene to Holocene within either one of the abyssal plains. The Mediterranean outflow, which is enriched in dissolved silica, apparently had no effect on dissolution rates of siliceous skeletons in the sediment.
    Keywords: Atlantische Kuppenfahrten 1967/1-3; Cape Blanc/Meteor Bank/Portugal; GIK/IfG; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M1048B; M8; M8_004-2; M8_008-3; M8_016-2; M8_017-2; M8_018-4; M8_020-2; M8_031-2; M8_057-2; M8_058-2; M8/16-2 M8016B; M8004B; M8008C; M8017B; M8018B; M8031A; M8057B; M8058B; Meteor (1964); North Atlantic; SL; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 10 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 52
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Thiede, Jörn (1971): Planktonische Foraminiferen in Sedimenten vom ibero-marokkanischen Kontinentalrand. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C7, 15-102
    Publication Date: 2024-02-03
    Description: Recent clays cover the East Atlantic continental slopes. They are gray and poor in sand off Portugal (Cape Sines), but reddish brown to reddish gray and richer in sand off Morocco (Cape Mazagan). The majority of the 19 sediment cores, which were taken mainly on two profiles (Fig. 3), can be correlated by means of planktonic foraminifera (Figs. 27, 28). The following parameters seem to be well suited for this purpose: qualitative and quantitative distribution of the planktonic foraminiferal species and faunas, coiling ratios of three Globorotalia-species: G. crassaformis, G. hirsuta and G. truncatulinoides. Sediments from about 2000 m water depth show highest sedimentation rates off Portugal (〉 20 cm/1000 yrs.), but off Morocco the lowest sedimentation rates (about 3 cm/1000 yrs.). The sediments are dated with planktonic foraminifera and 31 radiocarbon analyses and the stratigraphic interpretation is supported by the lithostratigraphy. Holocene faunas are distinguished from the Pleistocene ones by differences in species composition, lower dominances and higher diversities. The Holocene sediments show smaller differences of the foraminiferal numbers than the Pleistocene ones. During Holocene and Pleistocene the temperatures of the surface water masses (indicated by the planktonic foraminiferal faunas) show similar values nearshore and offshore off Morocco. Likewise, there is no apparent temperature gradient in the Pleistocene off Portugal; whereas here values increase offshore during the Holocene. The proportion of species indicating warmer water masses is generally higher off Morocco. The plankton/benthos ratio increases with water depth and reaches maximum values already at about 1000 m. The production rate for planktonic foraminifera is higher in the continental slope regions than in the open ocean, but their shells show typical solution phenomena already in water depths of less than 1000 m. A higher solutional rate was found in sediments from the Tagus Abyssal Plain, while sediments from Horse Shoe and Seine Abyssal Plain seem to be better preserved. In the Tagus Abyssal Plain solution is less important during late Pleistocene than during Holocene.
    Keywords: Atlantische Kuppenfahrten 1967/1-3; Cape Blanc/Meteor Bank/Portugal; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M8; M8_016-2; M8_017-2; M8_057-2; M8_058-2; M8_066-2; M8/16-2 M8016B; M8017B; M8057B; M8058B; M8066B; Meteor (1964); South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 14 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 53
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hartmann, Martin; Lange, Heinz; Seibold, Eugen; Walger, Eckart (1971): Oberflächensedimente im Persischen Golf und Golf von Oman. I. Geologisch-hydrologischer Rahmen und erste sedimentologische Ergebnisse. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C4, 1-76
    Publication Date: 2024-02-03
    Description: 1. Morphology and sedimentation The deepest parts of the Persian Gulf lie off the Iranian coast. Several swells separate the Persian Gulf into the Western Basin, the Central Basin and the Strait of Hormuz, which leads without noticeable morphological interruption onto the Biaban Shelf; the latter gradually drops off towards the continental slope, which itself has a strongly subdivided morphology. The sediment distribution in the Western Basin runs parallel to the basin's axis to a depth of 50 -60 m. This is caused by the shallow and uniform slope of the Iranian coast into the Western Basin, by clear exposure of the area to the Shamal-Winds and by tidal currents parallel to the basin's axis. Most other parameters also show isolines parallel to the coast line. Data from the sediment analyses show a net transport which extends out along the Central Swell: coarse fraction 〉 63 µ, total carbonate content, carbonate in fine fractions 〈 2 µ, 2-6 µ and 20-63 µ, calcite-aragonite ratios in the fine fractions 2-6 µ and 20-63 µ and quartz-dolomite ratios in fine fraction 2-6 µ. At least the uppermost 10-40 m of this sediment is late Holocene. This implies sedimentation rates of several meters per 1000 years. The slope from the Iranian coast into the Central Basin (max. depth 100 m) is generally steeper, with interspersed islands and flats. Both facts tend to disturb a sediment dustribition parallel to the basin's axis over extensive areas and may preclude any such trend from being detected by the methods and sample net used. The spatial distribution of the coarse fraction, however, seems to indicate sediment transport at greater water depths perpendicular to the basin's long axis and along the steepest gradients well into the Central Basin. The flats of the Central Basin have a sediment cover distinctly different from those of the deeper basin areas. Characteristic parameters are the extremely high percentages of coarse grained sediments, total content of carbonate CO2 over 40, low total organic carbon content, (however values are high if calculated on the basis of the 〈 63 µ fraction), low total N-content, and low C/N ratios. These characteristics probably result from the absence of any terrigenous material being brought in as well as from exposure to wave action. Finest terrigenous material is deposited in the innermost protected part of the Hormuz Bay. In the deep channel cut into the Biaban Shelf which carries the Persian Gulf out-flow water to the Indian Ocean, no fine grained sediment is deposited as shown by grain size data. 2. Geographic settings and sedimentation Flat lands border the Arabian coast of the Persian Gulf except for the Oman region. The high and steep Zagros Mountains form the Iranian coastline. Flat topography in combination with generally low precipitation precludes fluviatile sediment being added from the South. Inorganic and biogenic carbonates accumulating under low sedimentation rates are dominant on the shallow Arabic Shelf and the slopes into the Western and Central Basins. The fluviatile sediment brought in from the Iranian side, however decisively determine the composition of the Holocene sediment cover in the Persian Gulf and on the Biaban Shelf. Holocene sediments extend 20-30 km seaward into the Western Basin and about 25 km on to the Biaban Shelf. As mentioned before, sedimentation rates are of several meters/1000 years. The rocks exposed in the hinterland influence the sediments. According to our data the Redbeds of the Zagros Mountains determine the colour of the very fine grained sediments near the Iranian Coast of the Persian Gulf. To the West of Hormuz, addition of carbonate minerals is particularly high. Dolomite and protodolomite, deposited only in this area, as well as palygorskite, have proven to be excellent trace minerals. To the East of Hormuz, the supply of terrigenous carbonates is considerably lower. Clay minerals appear to bring in inorganically bound nitrogen thus lowering the C/N ratio in these sediments especially off river mouths. 3. Climate and sedimentation The Persian Gulf is located in a climatically arid region. This directly affects sedimentation through increased wind action and the infrequent but heavy rainfalls which cause flash floods. Such flash floods could be responsible for transporting sedheats into the Central Basin in a direction perpendicular to the Gulf's axis. Eolian influx is difficult to asses from our data; however, it probably is of minor importance from the Iranian side and may add, at the most, a few centimeters of fine sediment per 1000 years. 4. Hydrology and sedimentation High water temperatures favor inorganic carbonate precipitation in southern margin of the Gulf, and probably on the flats, as well as biogenic carbonate production in general. High evaporation plus low water inflow through rivers and precipitation cause a circulation pattern that is typical for epicontinental seas within the arid climate region. Surface water flows in from the adjoining ocean, in this case the Indian Ocean and sinks to the bottom of the Persian Gulf mainly in the northern part of the Western Basin, on the "Mesopotamischer Flachschelf" ard probably in the area of the "Arabischer Flachschelf". This sinking water continually rejuvenates the bottom out-flow water. The inflowing surface water from the Indian Ocean brings organic matter into the Persian Gulf, additional nutrients are added by the "fresh" upwelling waters of the Gulf of Oman. Both nutrients and organic matter diminish very rapidly as the water moves into the Persian Gulf. This depletion of nutrients and organic matter is the reasonfor generally low organic carbon contents of the Persian Gulf sediments. The Central Swell represents a distinct boundary, to the west of which the organic carbon content are lower than to the east when sediment samples of similar grain size distribution are compared. The outflow carries well oxygenated water over the bottom of the Persian Gulf and the resulting oxidation further decreases the content of organic matter. In the Masandam-Channel and in the Biaban-Shelf channel, the outflowing water prevents deposition of fine material and transports sediment particles well beyond the shelf margin. The outflowing water remains at a depth of 200-300 m depending on its density and releases ist suspending sediment load to the ocean floor, irrespectative of the bottom morphology. This is reflected in several parameters in which the sediments from beneath the outflow differ from nearby sediments not affected by the outflowing water. High carbonate content of total samples and of the individual size fraction as well as high aragonite and dolomite contents of individual size fractions characterize the sediment beneath the outflowing water. The tidal currents, which avt more or less parallel to the Gulf's axis, favor mixing of the water masses, they rework sediments at velocities reported here. This fact enlarges to a certain degree the extent of our interfaces which are based on only a few sample points (Persian Gulf and Biaban Shelf one sample per 620 km**2, continental slope one sample per 1000 km**2). The water on the continental slope shows and oxygen minimum at 200-1200 m which favors preservation of organically-bound carbon in the sediment. The low pH-values may even permit dissolution of carbonate minerals.
    Keywords: BC; Box corer; CTD/Rosette; CTD-RO; GIK/IfG; GIK01049; GIK01051; GIK01052; GIK01054; GIK01055; GIK01056; GIK01057; GIK01058; GIK01059; GIK01060; GIK01061; GIK01062; GIK01063; GIK01064; GIK01065; GIK01066; GIK01067; GIK01068; GIK01069; GIK01070; GIK01071; GIK01072; GIK01073; GIK01074; GIK01075; GIK01076; GIK01077; GIK01078; GIK01079; GIK01080; GIK01081; GIK01082; GIK01083; GIK01084; GIK01085; GIK01086; GIK01087; GIK01088; GIK01089; GIK01090; GIK01091; GIK01092; GIK01093; GIK01094; GIK01095; GIK01096; GIK01097; GIK01098; GIK01099; GIK01100; GIK01101; GIK01102; GIK01103; GIK01104; GIK01105; GIK01106; GIK01107; GIK01108; GIK01109; GIK01110; GIK01111; GIK01112; GIK01113; GIK01114; GIK01115; GIK01116; GIK01117-2; GIK01118; GIK01119; GIK01120; GIK01121; GIK01122; GIK01123; GIK01124; GIK01125; GIK01126; GIK01127; GIK01128; GIK01129; GIK01130; GIK01131; GIK01132; GIK01133; GIK01134; GIK01135; GIK01136; GIK01137; GIK01138; GIK01139; GIK01140; GIK01141; GIK01142; GIK01143; GIK01144; GIK01145; GIK01146; GIK01147; GIK01148; GIK01149; GIK01150; GIK01151; GIK01152; GIK01153; GIK01154; GIK01155; GIK01156; GIK01157; GIK01158; GIK01159; GIK01160; GIK01161; GIK01162; GIK01163; GIK01164; GIK01165; GIK01166; GIK01167; GIK01168; GIK01169; GIK01170; GIK01171; GIK01172; GIK01173; GIK01174; GIK01175; GIK01176; GIK01177; GIK01178; GIK01179; GIK01180; GIK01181; GIK01182; GIK01183; GIK01184; GIK01185; GIK01186; GIK01187; GIK01188; GIK01189; GIK01190; GIK01191; GIK01192; GIK01193; GIK01194; GIK01195; GIK01196; GIK01197; GIK01198; GIK01199; GIK01200; GIK01201; GIK01202; GIK01203; GIK01204; Gravity corer (Kiel type); IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M1; M1_243; M1_245 01051-B; M1_246; M1_249; M1_250; M1_251; M1_252 01057-C; M1_253; M1_254 01059-B; M1_255; M1_256; M1_257; M1_258; M1_259; M1_260; M1_261; M1_262; M1_263; M1_264; M1_265; M1_266; M1_267; M1_268; M1_269; M1_270; M1_271; M1_272; M1_273 01078-A; M1_274; M1_275; M1_276; M1_277; M1_278 01083-B; M1_279 01084-B; M1_280A; M1_280B; M1_280C 01087-B; M1_281 01088-C; M1_282; M1_283; M1_284; M1_285; M1_286 01093-B; M1_287; M1_288; M1_289 01096-B; M1_290; M1_290B; M1_290C; M1_291; M1_292 11101-2; M1_293 11102-3; M1_294; M1_295 11104-2; M1_296 11105-3; M1_297 11106-2; M1_298; M1_299; M1_300; M1_301 11110-2; M1_302 11111-2; M1_303 11112-1; M1_304 11113-2; M1_305 11114-2; M1_306; M1_307; M1_308 11117-2; M1_309; M1_310 11119-2; M1_311 11120-2; M1_312 11121-2; M1_313 11122-2; M1_314; M1_315; M1_316; M1_317; M1_318 01127-B; M1_319 01128-B; M1_320 01129-B; M1_321 01130-B; M1_322; M1_323 11132-1; M1_324; M1_324 11134-1; M1_326 01135-B; M1_327 01136-B; M1_328A 01137-B; M1_328B 01138-B; M1_329; M1_329C 01141-B; M1_330A 01142-B; M1_330B 01143-B; M1_330C 01144-B; M1_331 01145-C; M1_332 01146-B; M1_333; M1_334 01148-B; M1_335 01149-B; M1_336 01150-B; M1_337 01151-B; M1_338 01152-B; M1_339 11053-1; M1_340 01154-B; M1_341 01155-B; M1_342; M1_342A 01156-B; M1_343; M1_344; M1_345; M1_346 01161-B; M1_347A 01162-B; M1_347B 01163-B; M1_347C; M1_348 01165-A; M1_349 01166-B; M1_350; M1_351; M1_352 01173-C; M1_353 01174-B; M1_354 01175-B; M1_355A 01176-B; M1_355B 01177-C; M1_356 01178-C; M1_357 11079-2; M1_358 01180-C; M1_359 11081-2; M1_360 01182-B; M1_361 01183-B; M1_362; M1_363 11085-2; M1_364; M1_365 01187-C; M1_366 11088-1; M1_367; M1_368 01190-C; M1_369; M1_370 11092-2; M1_371; M1_372; M1_373; M1_374 01196-C; M1_375; M1_376 01198-B; M1_377 01199-G; M1_378 01200-B; M1_379; M1_380; M1_381; M1_382; M1_CTD372; M1_CTD373; M1_CTD380; M1_CTD381; Meteor (1964); Northern Arabian Sea; Persian Gulf; Req_1; Req_12; Req_13; Req_14; Req_17; Req_18; Req_2; Req_20; Req_22; Req_23; Req_25; Req_29; Req_30; Req_31; Req_33; Req_34; Req_35; Req_36; Req_40; Req_5; Req_7; Req_9; SL
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 54
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Sarnthein, Michael (1971): Oberflächensedimente im Persischen Golf und Golf von Oman. II. Quantitative Komponentenanalyse der Grobfraktion. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C5, 1-113
    Publication Date: 2024-02-03
    Description: In the Persian Gulf and the Gulf of Oman marl forms the primary sediment cover, particularly on the Iranian side. A detailed quantitative description of the sediment components 〉 63 µ has been attempted in order to establish the regional distribution of the most important constituents as well as the criteria governing marl sedimentation in general. During the course of the analysis, the sand fraction from about 160 bottom-surface samples was split into 5 phi° fractions and 500 to 800 grains were counted in each individual fraction. The grains were cataloged in up to 40 grain type catagories. The gravel fraction was counted separately and the values calculated as weight percent. Basic for understanding the mode of formation of the marl sediment is the "rule" of independent availability of component groups. It states that the sedimentation of different component groups takes place independently, and that variation in the quantity of one component is independent of the presence or absence of other components. This means, for example, that different grain size spectrums are not necessarily developed through transport sorting. In the Persian Gulf they are more likely the result of differences in the amount of clay-rich fine sediment brought in to the restricted mouth areas of the Iranian rivers. These local increases in clayey sediment dilute the autochthonous, for the most part carbonate, coarse fraction. This also explains the frequent facies changes from carbonate to clayey marl. The main constituent groups of the coarse fraction are faecal pellets and lumps, the non carbonate mineral components, the Pleistocene relict sediment, the benthonic biogene components and the plankton. Faecal pellets and lumps are formed through grain size transformation of fine sediment. Higher percentages of these components can be correlated to large amounts of fine sediment and organic C. No discernable change takes place in carbonate minerals as a result of digestion and faecal pellet formation. The non-carbonate sand components originate from several unrelated sources and can be distinguished by their different grain size spectrum; as well as by other characteristics. The Iranian rivers supply the greatest amounts (well sorted fine sand). Their quantitative variations can be used to trace fine sediment transport directions. Similar mineral maxima in the sediment of the Gulf of Oman mark the path of the Persian Gulf outflow water. Far out from the coast, the basin bottoms in places contain abundant relict minerals (poorly sorted medium sand) and localized areas of reworked salt dome material (medium sand to gravel). Wind transport produces only a minimal "background value" of mineral components (very fine sand). Biogenic and non-biogenic relict sediments can be placed in separate component groups with the help of several petrographic criteria. Part of the relict sediment (well sorted fine sand) is allochthonous and was derived from the terrigenous sediment of river mouths. The main part (coarse, poorly sorted sediment), however, was derived from the late Pleistocene and forms a quasi-autochthonous cover over wide areas which receive little recent sedimentation. Bioturbation results in a mixing of the relict sediment with the overlying younger sediment. Resulting vertical sediment displacement of more than 2.5 m has been observed. This vertical mixing of relict sediment is also partially responsible for the present day grain size anomalies (coarse sediment in deep water) found in the Persian Gulf. The mainly aragonitic components forming the relict sediment show a finely subdivided facies pattern reflecting the paleogeography of carbonate tidal flats dating from the post Pleistocene transgression. Standstill periods are reflected at 110 -125m (shelf break), 64-61 m and 53-41 m (e.g. coare grained quartz and oolite concentrations), and at 25-30m. Comparing these depths to similar occurrences on other shelf regions (e. g. Timor Sea) leads to the conclusion that at this time minimal tectonic activity was taking place in the Persian Gulf. The Pleistocene climate, as evidenced by the absence of Iranian river sediment, was probably drier than the present day Persian Gulf climate. Foremost among the benthonic biogene components are the foraminifera and mollusks. When a ratio is set up between the two, it can be seen that each group is very sensitive to bottom type, i.e., the production of benthonic mollusca increases when a stable (hard) bottom is present whereas the foraminifera favour a soft bottom. In this way, regardless of the grain size, areas with high and low rates of recent sedimentation can be sharply defined. The almost complete absence of mollusks in water deeper than 200 to 300 m gives a rough sedimentologic water depth indicator. The sum of the benthonic foraminifera and mollusca was used as a relative constant reference value for the investigation of many other sediment components. The ratio between arenaceous foraminifera and those with carbonate shells shows a direct relationship to the amount of coarse grained material in the sediment as the frequence of arenaceous foraminifera depends heavily on the availability of sand grains. The nearness of "open" coasts (Iranian river mouths) is directly reflected in the high percentage of plant remains, and indirectly by the increased numbers of ostracods and vertebrates. Plant fragments do not reach their ultimate point of deposition in a free swimming state, but are transported along with the remainder of the terrigenous fine sediment. The echinoderms (mainly echinoids in the West Basin and ophiuroids in the Central Basin) attain their maximum development at the greatest depth reached by the action of the largest waves. This depth varies, depending on the exposure of the slope to the waves, between 12 to 14 and 30 to 35 m. Corals and bryozoans have proved to be good indicators of stable unchanging bottom conditions. Although bryozoans and alcyonarian spiculae are independent of water depth, scleractinians thrive only above 25 to 30 m. The beginning of recent reef growth (restricted by low winter temperatures) was seen only in one single area - on a shoal under 16 m of water. The coarse plankton fraction was studied primarily through the use of a plankton-benthos ratio. The increase in planktonic foraminifera with increasing water depth is here heavily masked by the "Adjacent sea effect" of the Persian Gulf: for the most part the foraminifera have drifted in from the Gulf of Oman. In contrast, the planktonic mollusks are able to colonize the entire Persian Gulf water body. Their amount in the plankton-benthos ratio always increases with water depth and thereby gives a reliable picture of local water depth variations. This holds true to a depth of around 400 m (corresponding to 80-90 % plankton). This water depth effect can be removed by graphical analysis, allowing the percentage of planktonic mollusks per total sample to be used as a reference base for relative sedimentation rate (sedimentation index). These values vary between 1 and 〉 1000 and thereby agree well with all the other lines of evidence. The "pteropod ooze" facies is then markedly dependent on the sedimentation rate and can theoretically develop at any depth greater than 65 m (proven at 80 m). It should certainly no longer be thought of as "deep sea" sediment. Based on the component distribution diagrams, grain size and carbonate content, the sediments of the Persian Gulf and the Gulf of Oman can be grouped into 5 provisional facies divisions (Chapt.19). Particularly noteworthy among these are first, the fine grained clayey marl facies occupying the 9 narrow outflow areas of rivers, and second, the coarse grained, high-carbonate marl facies rich in relict sediment which covers wide sediment-poor areas of the basin bottoms. Sediment transport is for the most part restricted to grain sizes 〈 150 µ and in shallow water is largely coast-parallel due to wave action at times supplemented by tidal currents. Below the wave base gravity transport prevails. The only current capable of moving sediment is the Persian Gulf outflow water in the Gulf of Oman.
    Keywords: BC; Box corer; GIK/IfG; GIK01054; GIK01055; GIK01056; GIK01057; GIK01058; GIK01059; GIK01060; GIK01061; GIK01062; GIK01063; GIK01064; GIK01065; GIK01066; GIK01067; GIK01068; GIK01069; GIK01070; GIK01071; GIK01072; GIK01073; GIK01074; GIK01075; GIK01076; GIK01077; GIK01078; GIK01079; GIK01080; GIK01081; GIK01082; GIK01083; GIK01084; GIK01085; GIK01088; GIK01089; GIK01090; GIK01091; GIK01092; GIK01093; GIK01094; GIK01095; GIK01096; GIK01097; GIK01098; GIK01099; GIK01100; GIK01101; GIK01102; GIK01103; GIK01104; GIK01105; GIK01106; GIK01107; GIK01108; GIK01109; GIK01110; GIK01111; GIK01112; GIK01113; GIK01114; GIK01115; GIK01116; GIK01117-2; GIK01118; GIK01119; GIK01120; GIK01121; GIK01122; GIK01123; GIK01124; GIK01125; GIK01126; GIK01127; GIK01128; GIK01129; GIK01130; GIK01131; GIK01132; GIK01133; GIK01134; GIK01135; GIK01136; GIK01137; GIK01138; GIK01139; GIK01140; GIK01141; GIK01142; GIK01143; GIK01144; GIK01145; GIK01146; GIK01147; GIK01148; GIK01149; GIK01150; GIK01151; GIK01152; GIK01153; GIK01154; GIK01155; GIK01156; GIK01157; GIK01158; GIK01159; GIK01160; GIK01161; GIK01162; GIK01163; GIK01164; GIK01165; GIK01166; GIK01167; GIK01168; GIK01169; GIK01170; GIK01171; GIK01172; GIK01173; GIK01174; GIK01175; GIK01176; GIK01177; GIK01178; GIK01179; GIK01180; GIK01181; GIK01182; GIK01183; GIK01184; GIK01185; GIK01186; GIK01187; GIK01188; GIK01189; GIK01190; GIK01191; GIK01192; GIK01193-3; GIK01194; GIK01195; GIK01196; GIK01197; GIK01198; GIK01199; GIK01200; GIK01201; GIK01202; GIK01203; GIK01204; Gravity corer (Kiel type); IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M1; M1_249; M1_250; M1_251; M1_252 01057-C; M1_253; M1_254 01059-B; M1_255; M1_256; M1_257; M1_258; M1_259; M1_260; M1_261; M1_262; M1_263; M1_264; M1_265; M1_266; M1_267; M1_268; M1_269; M1_270; M1_271; M1_272; M1_273 01078-A; M1_274; M1_275; M1_276; M1_277; M1_278 01083-B; M1_279 01084-B; M1_280A; M1_281 01088-C; M1_282; M1_283; M1_284; M1_285; M1_286 01093-B; M1_287; M1_288; M1_289 01096-B; M1_290; M1_290B; M1_290C; M1_291; M1_292 11101-2; M1_293 11102-3; M1_294; M1_295 11104-2; M1_296 11105-3; M1_297 11106-2; M1_298; M1_299; M1_300; M1_301 11110-2; M1_302 11111-2; M1_303 11112-1; M1_304 11113-2; M1_305 11114-2; M1_306; M1_307; M1_308 11117-2; M1_309; M1_310 11119-2; M1_311 11120-2; M1_312 11121-2; M1_313 11122-2; M1_314; M1_315; M1_316; M1_317; M1_318 01127-B; M1_319 01128-B; M1_320 01129-B; M1_321 01130-B; M1_322; M1_323 11132-1; M1_324; M1_324 11134-1; M1_326 01135-B; M1_327 01136-B; M1_328A 01137-B; M1_328B 01138-B; M1_329; M1_329C 01141-B; M1_330A 01142-B; M1_330B 01143-B; M1_330C 01144-B; M1_331 01145-C; M1_332 01146-B; M1_333; M1_334 01148-B; M1_335 01149-B; M1_336 01150-B; M1_337 01151-B; M1_338 01152-B; M1_339 11053-1; M1_340 01154-B; M1_341 01155-B; M1_342; M1_342A 01156-B; M1_343; M1_344; M1_345; M1_346 01161-B; M1_347A 01162-B; M1_347B 01163-B; M1_347C; M1_348 01165-A; M1_349 01166-B; M1_350; M1_351; M1_352 01173-C; M1_353 01174-B; M1_354 01175-B; M1_355A 01176-B; M1_355B 01177-C; M1_356 01178-C; M1_357 11079-2; M1_358 01180-C; M1_359 11081-2; M1_360 01182-B; M1_361 01183-B; M1_362; M1_363 11085-2; M1_364; M1_365 01187-C; M1_366 11088-1; M1_367; M1_368 01190-C; M1_369; M1_370 11092-2; M1_371 11093-3; M1_372; M1_373; M1_374 01196-C; M1_375; M1_376 01198-B; M1_377 01199-G; M1_378 01200-B; M1_379; M1_380; M1_381; M1_382; Meteor (1964); Northern Arabian Sea; Persian Gulf; SL
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 55
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Beiersdorf, Helmut (1972): Schwermineraluntersuchungen an Sedimenten aus West-Pakistan sowie vom angrenzenden Schelf. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C9, 74-83
    Publication Date: 2024-02-03
    Description: Sediment samples from the southern West-Pakistan and the adjacent shelf have been studied for their heavy mineral contents and compositions. It is shown that the sediment load of the Indus river has influenced the sedimentation in the shelf areas south, southwest and in front of the Indus delta to a greater extent than in northerly direction. In the northern shelf region the smaller local rivers have dominated the marine sedimentation.
    Keywords: Arabian Sea; BC; Bottom grab (Peterson); Box corer; BP; Geological sample; GEOS; GIK/IfG; IIOE - International Indian Ocean Expedition; INDUS; Indus_1; Indus_10; Indus_12; Indus_13; Indus_14; Indus_2; Indus_21; Indus_23; Indus_24; Indus_25; Indus_26; Indus_27; Indus_28; Indus_29; Indus_3; Indus_30; Indus_31; Indus_32; Indus_33; Indus_34; Indus_37; Indus_38; Indus_40; Indus_41; Indus_5; Indus_6b; Indus_7; Indus_8; Indus_9; Institute for Geosciences, Christian Albrechts University, Kiel; Machhera; MH_1; MH_14; MH_15; MH_16; MH_17; MH_18; MH_19; MH_33; MH_34; MH65; Pakistan
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 56
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Diester, Lieselotte (1972): Zur spätpleistozänen und holozänen Sedimentation im zentralen und östlichen Persischen Golf. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C8, 37-83
    Publication Date: 2024-02-03
    Description: The sandfraction of the sediment was analysed in five cores, taken from 65 m water depth in the central and eastern part of the Persian Gulf. The holocene marls are underlayn by aragonite muds, which are probably 10-11,000 years old. 1. The cores could be subdivided into coarse grained and fine grained layers. Sorting is demonstrated by the following criteria: With increasing median values of the sandfraction - the fine grained fraction decreases within each core; - the median of each biogenic component, benthonic as well as planktonic, increases; - the median of the relict sediment, which in core 1179 was carried upward into the marl by bioturbation, increases; - the percentages of pelecypods, gastropods, decapods and serpulid worms in the sandfraction increase, the percentages of foraminifera and ostracods decrease; - the ratios of pelecypods to foraminifera and of decapods to ostracods increase; - the ratios of benthonic molluscs to planktonic molluscs (pteropods) and of benthonic foraminifera to planktonic foraminifera increase (except in core 1056 and 1179); - the ratio of planktonic molluscs (pteropods) to planktonic foraminifera increases; - the globigerinas without orbulinas increase, the orbulinas decrease in core 1056. Different settling velocities of these biogenic particles help in better understanding the results : the settling velocities, hence the equivalent hydrodynamic diameters, of orbulinas are smaller than those of other globigerinas, those of planktonic foraminifera are smaller than those of planktonic molluscs, those of planktonic molluscs are smaller than those of benthonic molluscs, those of pelecypods are smaller than those of gastropods. Bioturbation could not entirely distroy this “grain-size-stratification". Sorting has been stronger in the coarse layers than in the finer ones. As a cause variations in the supply of terrigenous material at constant strength of tidal currents is suggested. When much terrigenous material is supplied (large contents of fine grained fraction) the sedimentation rates are high: the respective sediment surface is soon covered and removed from the influence of tidal currents. When, however, the supply of terrigenous material is small, more sandy material is taken away in all locations within the influence of terrigenous supply. Thus the biogenic particles in the sediment do not only reflect the organic production, but also the influence of currents. 2. There is no parameter present in all cores that is independently variable from grain size and can be used for stratigraphic correlation. The two cores from the Strait of Hormus were correlated by their sequences of coarse and fine grained layers. 3. The sedimentation rates of terrigenous material, of total planktonic and benthonic organisms and of molluscs, foraminifera, echinoids and ophiuroids are shown in table 1 (total sediment 6.3-75.5 cm/1000 yr, biogenic carbonate 1.9-3.6 cm/1000 yr). The sedimentation rates of benthonic organisms are nearly the same in the cores of the Strait of Hormus, whereas near the Central Swell they are smaller. In the upper parts of the two cores of the Strait of Hormus sedimentation rates are higher than in the deeper parts, where higher median values point to stronger reworking. 4. The sequence of coarse and fine grained intervals in the two cores of the Hormus Strait, attributed to variations in climate, as well as the increase of terrigenous supply from the deeper to the upper parts of the cores, agrees with the descriptions in the literature of the post Pleistocene climate as becoming more humid. The rise of sea level is sedimentologically not measurable in the marly sediments - except perhaps for the higher content of echinoids in the lower part of core 1056. These may be attributed to the influence of a migrating wave-base. 5. The late Pleistocene aragonite mud is very fine grained (〉 50%〈 2 p) and poor in fossils (0.5-1.8%) biogenic particles of total sediment. The sand fraction consists almost entirely of white clumps, c. 0.1 mm in diameter (1177), composed of aragonite needles and of detrital minerals with the same size (1201). The argonite mud was probably not formed in situ, because the water depth at time of formation was at most 35 m at least 12 m. The sorting of the sediment (predominance of the fine grained sand), the absence of larger biogenic components and of pellets, c. 0.2-0.5 mm in diameter, which are typical for Recent and Pleistocene locations of aragonite formation, as well as the sedimentological conditions near the sampling points, indicate rather a transport of aragonite mud from an area of formation in very shallow waters. Sorting as well as lenticular fabric in core 1201 point to sedimentation within the influence of currents. During alternating sedimentation - and reworking processes the aragonitic matrix was separated from the silt - and sand-sized minerals. The lenses grade into touches because of bioturbation. 6. In core 1056 D2 from Hormus Bay the percentages of organic carbon, total nitrogen and total carbonate were determined. With increasing amounts of smaller grain sizes the content of organic matter increases, whereas the amount of carbonate decreases. The amounts of organic carbon and of nitrogen decrease with increasing depth, probably due to early-diagenetic decomposition processes. Most of the total nitrogen is of organic origin, only about 10% may well be inorganically fixed as ammonium-nitrogen. In the upper part of the core the C/N-ratio increases with increasing depth. This may be connected with a stronger decomposition of nitrogen-containing organic compounds. The general decrease of the C/N-ratios in the lower part of the core may be explained by the relative increase of inorganically fixed ammonium-nitrogen with decreasing content of organic matter.
    Keywords: GC; GIK/IfG; GIK01177; GIK01201; Gravity corer; Gravity corer (Kiel type); IIOE - International Indian Ocean Expedition; Indian Ocean; Institute for Geosciences, Christian Albrechts University, Kiel; IOE1056; KAL; Kasten corer; M1; M1_355B 01177-C; M1_379; M1056D; Meteor (1964); Persian Gulf; SL
    Type: Dataset
    Format: application/zip, 8 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 57
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Martini, Erlend; Müller, Carla (1972): Nannoplankton aus dem nördlichen Arabischen Meer. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C10, 63-74
    Publication Date: 2024-02-03
    Description: Recent nannoplankton from the "Meteor”-stations M 242, M 243 and M 245 in the northern Arabian Sea were studied by means of the light and electron microscope, and 19 species were found. The nannoplankton assemblage of the northern Arabian Sea is compared with those of the eastern and western Mediterranean Sea and the Atlantic Ocean. Gephyrocapsa oceanica (Kamptner), Cyclococcolithus leptoporus (Murray & Blackman), Emiliania huxleyi (Lohmann), Helicopontospbaera kamptneri (Hay & Mohler), and Umbilicosphaera mirabilis (Lohmann) are the most common species in the northern Arabian Sea. Reworked nannoplankton and nannoplankton species agglutinated by tintinnids are discussed.
    Keywords: BC; Box corer; GIK/IfG; IIOE - International Indian Ocean Expedition; Indian Ocean Standard Net; Institute for Geosciences, Christian Albrechts University, Kiel; IOSN; M1; M1_242; M1_243; M1_245; M1_MULT242; M1_MULT243; M1_MULT245; M1_NET243; Meteor (1964); Northern Arabian Sea
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 58
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Diester-Haass, Lieselotte; Schrader, Hans-Jürgen; Thiede, Jörn (1973): Sedimentological and paleoclimatological investigations of two pelagic ooze cores off Cape barbas, North-West Africa. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C16, 19-66
    Publication Date: 2024-02-03
    Description: Two box cores taken off Cape Barbas (North-West Africa) have been studied using three methods. The analyses of the coarse fraction, of biogenic opal and of planktonic foraminifera revealed : 1. Core GIK12310-4 penetrates Z, Y, X and upper part of W zone, whereas core GIK12379-1 penetrates Z and upper part of Y zone. 2. Holocene sedimentation rates are 2.5 cm/1000 y for core GIK12310-4 and 6.0 cm/1000 y for core GIK12379-1. During the Y zone 5 cm/l000 y were sedimented incore GIK12310-4 and 〉 10-20 cm/1000 y in core GIK12379-1. 3. Paleoclimatohgical results are: arid climate and relatively warm water temperatures during the Holocene (Z zone) and during X zone; humid climate and relatively cool water temperatures within the Wuerm (Y zone) (with a non-dated more arid interval found in the middle part of the Y zone) and in the upper part of the W zone. 4. Increased contents of benthos and radiolaria in the Y zone indicate upwelling. Upwelling, characterized by high content of biogenic opal and low water temperatures, was found in core GIK12310-4 at 250 to 350 cm in the lower part of the Y zone. The plankton/benthos ratio of foraminifera, the benthos/radiolaria ratio and water temperatures derived from planktonic foraminifera, differ in both cores in the Holocene, and are nearly identical during the Wuerm.
    Keywords: East Atlantic; GIK/IfG; GIK12310-4; GIK12379-1; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964)
    Type: Dataset
    Format: application/zip, 8 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 59
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lutze, Gerhard F (1974): Benthische Foraminiferen in Oberflächen-Sedimenten des Persischen Golfes. Teil 1: Arten. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C17, 1-66
    Publication Date: 2024-02-03
    Description: During "Meteor"cruise 1965 the author collected 134 samples of surface sediments from the Iranian part of the Persian Gulf. Benthic Foraminifera populations have been analysed for determining their depth zonation. These data are supposed to allow detailed depth interpretation of Pleistocene sediments found in cores. In addition, the ecological information might be usefull to reconstruct the depositional environment of fossil sediments in similar shallow epicontinental seas. The investigation is published in two parts: the present part 1 contains the catalogue of species with short discussions of taxonomic problems, notes on the distribution within the Persian Gulf and 11 plates, partly with scanning electron micrographs. The results of the statistical analysis are given in data tables which include number of species, percentages of 2 (and 5) ranked species, standing crop and foraminiferal numbers. The author used "species groups" to avoid ambiguities with species requiring additional taxonomic studies. However, species numbers within these units are estimated to yield applicable diversity information. - A total of 52 species and 7 "species groups" were separated, 2 new species were described.
    Keywords: Giant box corer; GIK/IfG; GIK01056; GIK01073; GIK01074; GIK01075; GIK01076; GIK01077; GIK01078; GIK01079; GIK01080; GIK01081; GIK01082; GIK01083; GIK01084; GIK01085; GIK01086; GIK01087; GIK01088; GIK01090; GIK01092; GIK01093; GIK01094; GIK01096; GIK01097; GIK01098; GIK01099; GIK01100; GIK01101; GIK01102; GIK01103; GIK01104; GIK01105; GIK01106; GIK01107; GIK01108; GIK01109; GIK01110; GIK01111; GIK01112; GIK01113; GIK01114; GIK01115; GIK01116; GIK01117-1; GIK01118; GIK01119; GIK01120; GIK01121; GIK01122; GIK01123; GIK01124; GIK01125; GIK01126; GIK01127; GIK01128; GIK01129; GIK01130; GIK01131; GIK01132; GIK01133; GIK01134; GIK01135; GIK01136; GIK01137; GIK01138; GIK01139; GIK01140; GIK01141; GIK01142; GIK01143; GIK01144; GIK01145; GIK01146; GIK01147; GIK01148; GIK01149; GIK01150; GIK01151; GIK01152; GIK01153; GIK01154; GIK01155; GIK01156; GIK01157; GIK01158; GIK01159; GIK01160; GIK01161; GIK01162; GIK01163; GIK01164; GIK01165; GIK01166; GIK01167; GIK01168; GIK01169; GIK01170; GIK01171; GIK01172; GIK01173; GIK01174; GIK01175; GIK01176; GIK01177; GIK01178; GIK01179; GIK01180; GIK01181; GIK01182; GIK01183; GIK01185; GIK01187; GIK01188; GIK01190; GIK01191; GIK01192; GIK01194; GIK01195; GIK01196; GIK01197; GIK01198; GIK01199; GIK01200; GIK01201; GIK01202; GIK01203; GIK01204; GKG; Gravity corer (Kiel type); IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M1; M1_251; M1_268; M1_269; M1_270; M1_271; M1_272; M1_273 01078-A; M1_274; M1_275; M1_276; M1_277; M1_278 01083-B; M1_279 01084-B; M1_280A; M1_280B; M1_280C 01087-B; M1_281 01088-C; M1_283; M1_285; M1_286 01093-B; M1_287; M1_289 01096-B; M1_290; M1_290B; M1_290C; M1_291; M1_292 11101-2; M1_293 11102-3; M1_294; M1_295 11104-2; M1_296 11105-3; M1_297 11106-2; M1_298; M1_299; M1_300; M1_301 11110-2; M1_302 11111-2; M1_303 11112-1; M1_304 11113-2; M1_305 11114-2; M1_306; M1_307; M1_308 11117-1; M1_309; M1_310 11119-2; M1_311 11120-2; M1_312 11121-2; M1_313 11122-2; M1_314; M1_315; M1_316; M1_317; M1_318 01127-B; M1_319 01128-B; M1_320 01129-B; M1_321 01130-B; M1_322; M1_323 11132-1; M1_324; M1_324 11134-1; M1_326 01135-B; M1_327 01136-B; M1_328A 01137-B; M1_328B 01138-B; M1_329; M1_329C 01141-B; M1_330A 01142-B; M1_330B 01143-B; M1_330C 01144-B; M1_331 01145-C; M1_332 01146-B; M1_333; M1_334 01148-B; M1_335 01149-B; M1_336 01150-B; M1_337 01151-B; M1_338 01152-B; M1_339 11053-1; M1_340 01154-B; M1_341 01155-B; M1_342; M1_342A 01156-B; M1_343; M1_344; M1_345; M1_346 01161-B; M1_347A 01162-B; M1_347B 01163-B; M1_347C; M1_348 01165-A; M1_349 01166-B; M1_350; M1_351; M1_352 01173-C; M1_353 01174-B; M1_354 01175-B; M1_355A 01176-B; M1_355B 01177-C; M1_356 01178-C; M1_357 11079-2; M1_358 01180-C; M1_359 11081-2; M1_360 01182-B; M1_361 01183-B; M1_363 11085-2; M1_365 01187-C; M1_366 11088-1; M1_368 01190-C; M1_369; M1_370 11092-2; M1_372; M1_373; M1_374 01196-C; M1_375; M1_376 01198-B; M1_377 01199-G; M1_378 01200-B; M1_379; M1_380; M1_381; M1_382; Meteor (1964); Persian Gulf; SL
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 60
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hartmann, Martin; Müller, Peter J; Suess, Erwin; van der Weijden, Cornelis H (1973): Oxidation of organic matter in recent marine sediments. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C12, 74-86
    Publication Date: 2024-02-03
    Description: Carbon dioxide, ammonia, and reactive phosphate in the interstitial water of three sediment cores of the West African continental margin result from oxidation of sedimentary organic matter by bacterial sulfate reduction. The proposed model is a modification of one initially suggested by Richards (1965) for processes in anoxic waters: (CH2O)106 (NH3)8 (H3PO4) (0.7-0.2) + 53 SO4**2- =106 CO2 + 106 H20 + 8 NH3 + (0.7 - 0.2) H3PO4 + 53 S**2- The amount of reduced interstitial sulfate, the carbon-to-nitrogen-to-phosphorus atomic ratio of the sedimentary organic matter, as well as small amounts of carbon dioxide, which precipitated as interstitial calcium carbonate, are included in the general oxidation-reduction reaction. Preferential loss of nitrogen and phosphorus from organic matter close to the surface was recorded in both the interstitial water and sediment composition. It appeared that in deeper sections of the core organic carbon compounds were oxidized which were probably in an even lower oxidation state than that indicated by the proposed model. An estimated 2 % of the amount of organic matter still present was oxidized after it became incorporated into the sediment; whereas sulfide sulfur contents indicate that a much larger percentage (15-20%) seemed to have been subject to bacterial oxidation during the Pleistocene period, when a very thin oxidizing layer on the sediment allowed the above decomposition process to start relatively early favoured by almost fresh organic matter, and by almost unrestricted exchange of sulfate with the overlying water.
    Keywords: BCR; Bottle, Niskin; Box corer (Reineck); East Atlantic; GIK/IfG; GIK12307-2; GIK12327-4; GIK12327-5; GIK12379-1; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964); NIS
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 61
    Publication Date: 2024-02-03
    Keywords: Carbon, organic, total; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Element analyser CHN, LECO WR-12; GIK/IfG; GIK10116-2; GIK-cruise; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; Wet combustion
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 62
    Publication Date: 2024-02-03
    Keywords: Atlantische Kuppenfahrten 1967/1-3; Biogenic particles; Counting 200-630 µm fraction; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Foraminifera; GIK/IfG; Grains, counted/analyzed; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M8; M8_057-2; M8057B; Meteor (1964); Ostracoda; South Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 215 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 63
    Publication Date: 2024-02-03
    Keywords: Counting 〉21 µm fraction; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoms; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M8_017-2; M8017B; Radiolarians; Siliceous microfossils; Sponge spiculae; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 89 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 64
    Publication Date: 2024-02-03
    Keywords: Atlantische Kuppenfahrten 1967/1-3; Counting 〉21 µm fraction; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoms; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M8; M8_057-2; M8057B; Meteor (1964); Radiolarians; Siliceous microfossils; South Atlantic Ocean; Sponge spiculae; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 125 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 65
    Publication Date: 2024-02-03
    Keywords: Calculated, see reference(s); Calculated from weight/volume; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK/IfG; GIK01201; Gravity corer (Kiel type); IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Layer thickness; M1; M1_379; Meteor (1964); Persian Gulf; Sedimentation rate; SL
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 66
    Publication Date: 2024-02-03
    Keywords: Age, dated; Age, dated, error to older; Age, dated, error to younger; Age, radiocarbon; Atlantische Kuppenfahrten 1967/1-3; Cape Blanc/Meteor Bank/Portugal; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M8; M8_016-2; M8/16-2 M8016B; Meteor (1964); Sample, optional label/labor no
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 67
    Publication Date: 2024-02-03
    Keywords: Atlantische Kuppenfahrten 1967/1-3; Counting 〉21 µm fraction; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoms; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M8; M8_008-3; M8008C; Meteor (1964); Radiolarians; Siliceous microfossils; South Atlantic Ocean; Sponge spiculae; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 68
    Publication Date: 2024-02-03
    Keywords: Atlantische Kuppenfahrten 1967/1-3; Counting 〉21 µm fraction; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoms; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M8; M8_058-2; M8058B; Meteor (1964); Radiolarians; Siliceous microfossils; South Atlantic Ocean; Sponge spiculae; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 53 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 69
    Publication Date: 2024-02-03
    Keywords: Arabian Sea; Calculated (Trask, 1932, Houston, Gulf Pab. Co 67 pp); Coarse fraction/modal analysis; Event label; Geological sample; GEOS; GIK/IfG; Grain quartile 1; Grain quartile 3; IIOE - International Indian Ocean Expedition; INDUS; Indus_1; Indus_12; Indus_13; Indus_14; Indus_2; Indus_26; Indus_27; Indus_28; Indus_29; Indus_3; Indus_30; Indus_31; Indus_32; Indus_34; Indus_41; Indus_5; Indus_7; Indus_8; Indus_9; Institute for Geosciences, Christian Albrechts University, Kiel; LATITUDE; LONGITUDE; Median, grain size; Pakistan; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 0.200 mm; Size fraction 0.200-0.063 mm, fine sand; Skewness; Sorting
    Type: Dataset
    Format: text/tab-separated-values, 148 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 70
    Publication Date: 2024-02-03
    Keywords: Aggregates; Amphibole; Andalusite; Apatite; Arabian Sea; Disthene; Event label; Garnet; Geological sample; GEOS; GIK/IfG; Heavy minerals; IIOE - International Indian Ocean Expedition; INDUS; Indus_1; Indus_10; Indus_12; Indus_13; Indus_14; Indus_2; Indus_21; Indus_23; Indus_24; Indus_25; Indus_26; Indus_27; Indus_28; Indus_29; Indus_3; Indus_30; Indus_31; Indus_32; Indus_33; Indus_34; Indus_37; Indus_38; Indus_40; Indus_41; Indus_5; Indus_6b; Indus_7; Indus_8; Indus_9; Institute for Geosciences, Christian Albrechts University, Kiel; LATITUDE; LONGITUDE; Opaque minerals; Orthopyroxene; Pakistan; Pyroxene; Rutile; Sillimanite; Size fraction; Staurolite; Titanite; Topaz; Tourmaline; Vesuvianite; Zircon; Zoisite
    Type: Dataset
    Format: text/tab-separated-values, 556 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 71
    Publication Date: 2024-02-03
    Keywords: Abundance estimate; Aspidorhabdus stylifer; BC; Box corer; Calciosolenia cf. sinuosa; Ceratolithus cristatus; Cyclococcolithus leptoporus; DEPTH, sediment/rock; Discoaster perplexus; Discosphaera tubifer; Emiliania huxleyi; Gephyrocapsa oceanica; GIK/IfG; Helicopontosphaera kamptneri; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_242; M1_MULT242; Meteor (1964); Northern Arabian Sea; Oolithotus fragilis; Pontosphaera discopora; Pontosphaera ribosa; Rhabdosphaera clavigera; Scyphosphaera apsteinii; Syracosphaera pulchra; Thoracosphaera albatrosiana; Thoracosphaera heimii; Umbellosphaera irregularis; Umbilicosphaera mirabilis
    Type: Dataset
    Format: text/tab-separated-values, 190 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 72
    Publication Date: 2024-02-03
    Keywords: Arabian Sea; BC; Bichromatic; Biogenic particles; Bottom grab (Peterson); Box corer; BP; Bryozoa; Calcium carbonate; Carbon, organic, total; Coarse fraction/modal analysis; Color description; Counting 〉63 µm fraction; Decapoda; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoms; Eastern Arabian Sea; Echinodermata; Elevation of event; Event label; Fecal pellets; Foraminifera, benthic; Foraminifera, planktic; Gas volumetric; GC; GIK/IfG; Glauconite; Gravity corer; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KL; Latitude of event; Lithology/composition/facies; Longitude of event; M1; M1_180; M1_180SK; M1_181; M1_181SK; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_192; M1_193; M1_194; M1_195; M1_196; M1_196a; M1_197; M1_198; M1_199; M1_200; M1_202; M1_205; M1_207; M1_209; M1_210; M1_211; M1_212; M1_213; M1_215; M1_217; M1_219; M1_220; M1_221; M1_222; M1_223; M1_224; M1_226; M1_227; M1_228; M1_229; M1_230; M1_232; M1_232SK; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_MULT182; M1_MULT183; M1_MULT184; M1_MULT185; M1_MULT186; M1_MULT187; M1_MULT188; M1_MULT189; M1_MULT190; M1_MULT192; M1_MULT193; M1_MULT194; M1_MULT195; M1_MULT196; M1_MULT196a; M1_MULT197; M1_MULT198; M1_MULT199; M1_MULT200; M1_MULT202; M1_MULT205; M1_MULT207; M1_MULT209; M1_MULT210; M1_MULT211; M1_MULT212; M1_MULT213; M1_MULT215; M1_MULT217; M1_MULT219; M1_MULT220; M1_MULT221; M1_MULT222; M1_MULT223; M1_MULT224; M1_MULT226; M1_MULT227; M1_MULT228; M1_MULT229; M1_MULT230; M1_MULT233; M1_MULT234; M1_MULT235; M1_MULT236; M1_MULT237; M1_MULT238; Machhera; Meteor (1964); MH_1; MH_10; MH_11; MH_12; MH_14; MH_15; MH_16; MH_17; MH_18; MH_19; MH_2; MH_20; MH_21; MH_22; MH_23; MH_24; MH_25; MH_26; MH_27; MH_28; MH_29; MH_3; MH_30; MH_31; MH_32; MH_33; MH_34; MH_35; MH_36; MH_37; MH_38; MH_39; MH_4; MH_40; MH_5; MH_6; MH_7; MH_8; MH_9; MH65; Mica; Munsell Color System (1994); Ooids; Ostracoda; PC; Piston corer; Piston corer (BGR type); Plant debris; Pteropoda; Quartz; Radiolarians; Shell debris; Siliciclastics; Size fraction 〉 0.063 mm, sand; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 2195 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 73
    Publication Date: 2024-02-03
    Keywords: Aggregates; Amphibole; Andalusite; Apatite; Arabian Sea; BC; Bottom grab (Peterson); Box corer; BP; Counting 〉25 µm fraction; DEPTH, sediment/rock; Disthene; Elevation of event; Event label; Garnet; GIK/IfG; Heavy minerals; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; Machhera; MH_1; MH_14; MH_15; MH_16; MH_17; MH_18; MH_19; MH_33; MH_34; MH65; Opaque minerals; Orthopyroxene; Pyroxene; Rutile; Sillimanite; Staurolite; Titanite; Topaz; Tourmaline; Vesuvianite; Zircon; Zoisite
    Type: Dataset
    Format: text/tab-separated-values, 140 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 74
    Publication Date: 2024-02-03
    Keywords: Abundance estimate; Aspidorhabdus stylifer; BC; Box corer; Calciosolenia cf. sinuosa; Ceratolithus cristatus; Cyclococcolithus leptoporus; DEPTH, sediment/rock; Discoaster perplexus; Discosphaera tubifer; Emiliania huxleyi; Gephyrocapsa oceanica; GIK/IfG; Helicopontosphaera kamptneri; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_243; M1_MULT243; Meteor (1964); Northern Arabian Sea; Oolithotus fragilis; Pontosphaera discopora; Pontosphaera ribosa; Rhabdosphaera clavigera; Scyphosphaera apsteinii; Syracosphaera pulchra; Thoracosphaera albatrosiana; Thoracosphaera heimii; Umbellosphaera irregularis; Umbilicosphaera mirabilis
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 75
    Publication Date: 2024-02-03
    Keywords: Abundance estimate; Aspidorhabdus stylifer; Calciosolenia cf. sinuosa; Ceratolithus cristatus; Cyclococcolithus leptoporus; DEPTH, water; Discoaster perplexus; Discosphaera tubifer; Emiliania huxleyi; Gephyrocapsa oceanica; GIK/IfG; Helicopontosphaera kamptneri; IIOE - International Indian Ocean Expedition; Indian Ocean Standard Net; Institute for Geosciences, Christian Albrechts University, Kiel; IOSN; M1; M1_243; M1_NET243; Meteor (1964); Northern Arabian Sea; Oolithotus fragilis; Pontosphaera discopora; Pontosphaera ribosa; Rhabdosphaera clavigera; Scyphosphaera apsteinii; Syracosphaera pulchra; Thoracosphaera albatrosiana; Thoracosphaera heimii; Umbellosphaera irregularis; Umbilicosphaera mirabilis
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 76
    Publication Date: 2024-02-03
    Keywords: Abundance estimate; Aspidorhabdus stylifer; BC; Box corer; Calciosolenia cf. sinuosa; Ceratolithus cristatus; Cyclococcolithus leptoporus; DEPTH, sediment/rock; Discoaster perplexus; Discosphaera tubifer; Emiliania huxleyi; Gephyrocapsa oceanica; GIK/IfG; Helicopontosphaera kamptneri; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_245; M1_MULT245; Meteor (1964); Northern Arabian Sea; Oolithotus fragilis; Pontosphaera discopora; Pontosphaera ribosa; Rhabdosphaera clavigera; Scyphosphaera apsteinii; Syracosphaera pulchra; Thoracosphaera albatrosiana; Thoracosphaera heimii; Umbellosphaera irregularis; Umbilicosphaera mirabilis
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 77
    Publication Date: 2024-02-03
    Keywords: Age, 14C AMS; Age, dated; DEPTH, sediment/rock; GIK/IfG; GIK01115; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M1; M1_306; Meteor (1964); Persian Gulf
    Type: Dataset
    Format: text/tab-separated-values, 1 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 78
    Publication Date: 2024-02-03
    Keywords: Age, 14C AMS; Age, dated; Age, dated standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK/IfG; GIK01165; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M1; M1_348 01165-A; Meteor (1964); Persian Gulf
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 79
    Publication Date: 2024-02-03
    Keywords: Age, 14C AMS; Age, dated; Age, dated standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK/IfG; GIK01160; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M1; M1_345; Meteor (1964); Persian Gulf
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 80
    Publication Date: 2024-02-03
    Keywords: Aluminium oxide; Cadmium; Carbon, organic, total; Cobalt; Copper; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eckernförder Bucht; GC; GIK/IfG; GIK-A; GIK-cruise; Gravity corer; Institute for Geosciences, Christian Albrechts University, Kiel; Iron; KI-620; Lead; Manganese; Nickel; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 274 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 81
    Publication Date: 2024-02-03
    Keywords: Aluminium oxide; Baltic Sea; BC; Box corer; Cadmium; Carbon, organic, total; Cobalt; Copper; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK/IfG; GIK-B; GIK-cruise; Institute for Geosciences, Christian Albrechts University, Kiel; Iron; KI-483; Lead; Manganese; Nickel; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 82
    Publication Date: 2024-02-03
    Keywords: Age, 14C conventional; Age, dated; Age, dated standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eckernförder Bucht; GC; GIK/IfG; GIK-A; GIK-cruise; Gravity corer; Institute for Geosciences, Christian Albrechts University, Kiel; Isotope ratio mass spectrometry; KI-620; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 89 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 83
    Publication Date: 2024-02-03
    Keywords: BC; Box corer; Comment; Comment 2 (continued); Comment 3 (continued); Current direction description; DEPTH, water; Elevation of event; Event label; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; Persian Gulf; Req_1; Req_12; Req_13; Req_14; Req_17; Req_18; Req_2; Req_20; Req_22; Req_23; Req_25; Req_29; Req_30; Req_31; Req_33; Req_34; Req_35; Req_36; Req_40; Req_5; Req_7; Req_9; Time in hours
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 84
    Publication Date: 2024-02-03
    Keywords: Age, 14C conventional; Age, dated; Age, dated standard deviation; Baltic Sea; BC; Box corer; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK/IfG; GIK-B; GIK-cruise; Institute for Geosciences, Christian Albrechts University, Kiel; Isotope ratio mass spectrometry; KI-483; SFB95; Wechselwirkung Meer-Meeresboden (Interaction Sea-Sea Bottom); δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 104 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 85
    Publication Date: 2024-02-03
    Keywords: Algae, calcareous; BC; Biogenic total, fractionated; Box corer; Bryozoa; Coral; Crustacea; Decapoda; DEPTH, sediment/rock; Dissolvable fraction; Elevation of event; Event label; Fecal pellets; Foraminifera, benthic agglutinated; Foraminifera, benthic calcareous; Foraminifera, planktic; Gastropoda; GIK/IfG; GIK01054; GIK01055; GIK01056; GIK01057; GIK01058; GIK01059; GIK01060; GIK01061; GIK01062; GIK01063; GIK01064; GIK01065; GIK01066; GIK01067; GIK01068; GIK01069; GIK01070; GIK01071; GIK01072; GIK01073; GIK01074; GIK01075; GIK01076; GIK01077; GIK01078; GIK01079; GIK01080; GIK01081; GIK01082; GIK01083; GIK01084; GIK01085; GIK01088; GIK01089; GIK01090; GIK01091; GIK01092; GIK01093; GIK01094; GIK01095; GIK01096; GIK01097; GIK01098; GIK01099; GIK01100; GIK01101; GIK01102; GIK01103; GIK01104; GIK01105; GIK01106; GIK01107; GIK01108; GIK01109; GIK01110; GIK01111; GIK01112; GIK01113; GIK01114; GIK01115; GIK01116; GIK01117-2; GIK01118; GIK01119; GIK01120; GIK01121; GIK01122; GIK01123; GIK01124; GIK01125; GIK01126; GIK01127; GIK01128; GIK01129; GIK01130; GIK01131; GIK01132; GIK01133; GIK01134; GIK01135; GIK01136; GIK01137; GIK01138; GIK01139; GIK01140; GIK01141; GIK01142; GIK01143; GIK01144; GIK01145; GIK01146; GIK01147; GIK01148; GIK01149; GIK01150; GIK01151; GIK01152; GIK01153; GIK01154; GIK01155; GIK01156; GIK01157; GIK01158; GIK01159; GIK01160; GIK01161; GIK01162; GIK01163; GIK01164; GIK01165; GIK01166; GIK01167; GIK01168; GIK01169; GIK01170; GIK01171; GIK01172; GIK01173; GIK01174; GIK01175; GIK01176; GIK01177; GIK01178; GIK01179; GIK01180; GIK01181; GIK01182; GIK01183; GIK01184; GIK01185; GIK01186; GIK01187; GIK01188; GIK01189; GIK01190; GIK01191; GIK01192; GIK01193-3; GIK01194; GIK01195; GIK01196; GIK01197; GIK01198; GIK01199; GIK01200; GIK01201; GIK01202; GIK01203; GIK01204; Grains, counted/analyzed; Gravity corer (Kiel type); Holothuria; IIOE - International Indian Ocean Expedition; Indeterminata; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; LATITUDE; Light minerals; LONGITUDE; M1; M1_249; M1_250; M1_251; M1_252 01057-C; M1_253; M1_254 01059-B; M1_255; M1_256; M1_257; M1_258; M1_259; M1_260; M1_261; M1_262; M1_263; M1_264; M1_265; M1_266; M1_267; M1_268; M1_269; M1_270; M1_271; M1_272; M1_273 01078-A; M1_274; M1_275; M1_276; M1_277; M1_278 01083-B; M1_279 01084-B; M1_280A; M1_281 01088-C; M1_282; M1_283; M1_284; M1_285; M1_286 01093-B; M1_287; M1_288; M1_289 01096-B; M1_290; M1_290B; M1_290C; M1_291; M1_292 11101-2; M1_293 11102-3; M1_294; M1_295 11104-2; M1_296 11105-3; M1_297 11106-2; M1_298; M1_299; M1_300; M1_301 11110-2; M1_302 11111-2; M1_303 11112-1; M1_304 11113-2; M1_305 11114-2; M1_306; M1_307; M1_308 11117-2; M1_309; M1_310 11119-2; M1_311 11120-2; M1_312 11121-2; M1_313 11122-2; M1_314; M1_315; M1_316; M1_317; M1_318 01127-B; M1_319 01128-B; M1_320 01129-B; M1_321 01130-B; M1_322; M1_323 11132-1; M1_324; M1_324 11134-1; M1_326 01135-B; M1_327 01136-B; M1_328A 01137-B; M1_328B 01138-B; M1_329; M1_329C 01141-B; M1_330A 01142-B; M1_330B 01143-B; M1_330C 01144-B; M1_331 01145-C; M1_332 01146-B; M1_333; M1_334 01148-B; M1_335 01149-B; M1_336 01150-B; M1_337 01151-B; M1_338 01152-B; M1_339 11053-1; M1_340 01154-B; M1_341 01155-B; M1_342; M1_342A 01156-B; M1_343; M1_344; M1_345; M1_346 01161-B; M1_347A 01162-B; M1_347B 01163-B; M1_347C; M1_348 01165-A; M1_349 01166-B; M1_350; M1_351; M1_352 01173-C; M1_353 01174-B; M1_354 01175-B; M1_355A 01176-B; M1_355B 01177-C; M1_356 01178-C; M1_357 11079-2; M1_358 01180-C; M1_359 11081-2; M1_360 01182-B; M1_361 01183-B; M1_362; M1_363 11085-2; M1_364; M1_365 01187-C; M1_366 11088-1; M1_367; M1_368 01190-C; M1_369; M1_370 11092-2; M1_371 11093-3; M1_372; M1_373; M1_374 01196-C; M1_375; M1_376 01198-B; M1_377 01199-G; M1_378 01200-B; M1_379; M1_380; M1_381; M1_382; Meteor (1964); Northern Arabian Sea; Ooids; Ophiuroidea; Ostracoda; Persian Gulf; Plant fragments; Porifera; Pteropoda; Reworked; Sample code/label; Scaphopoda; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 0.063 mm, sand; Size fraction 〉 2 mm, gravel; Size fraction 2.000-0.630 mm, coarse sand; SL; Vertebrata; Worm tubes
    Type: Dataset
    Format: text/tab-separated-values, 5141 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 86
    Publication Date: 2024-02-03
    Keywords: BC; Box corer; Calcium carbonate; Carbon, organic, fraction; Carbon, organic, total; Carbon/Nitrogen ratio; Color code HLS-system; DEPTH, sediment/rock; Dissolvable fraction; Elevation of event; Event label; GIK/IfG; GIK01049; GIK01051; GIK01052; GIK01054; GIK01055; GIK01056; GIK01057; GIK01058; GIK01059; GIK01060; GIK01061; GIK01062; GIK01063; GIK01064; GIK01065; GIK01066; GIK01067; GIK01068; GIK01069; GIK01070; GIK01071; GIK01072; GIK01073; GIK01074; GIK01075; GIK01076; GIK01077; GIK01078; GIK01079; GIK01080; GIK01081; GIK01082; GIK01083; GIK01084; GIK01085; GIK01086; GIK01087; GIK01088; GIK01089; GIK01090; GIK01091; GIK01092; GIK01093; GIK01094; GIK01095; GIK01096; GIK01097; GIK01098; GIK01099; GIK01100; GIK01101; GIK01102; GIK01103; GIK01104; GIK01105; GIK01106; GIK01107; GIK01108; GIK01109; GIK01110; GIK01111; GIK01112; GIK01113; GIK01114; GIK01115; GIK01116; GIK01117-2; GIK01118; GIK01119; GIK01120; GIK01121; GIK01122; GIK01123; GIK01124; GIK01125; GIK01126; GIK01127; GIK01128; GIK01129; GIK01130; GIK01131; GIK01132; GIK01133; GIK01134; GIK01135; GIK01136; GIK01137; GIK01138; GIK01139; GIK01140; GIK01141; GIK01142; GIK01143; GIK01144; GIK01145; GIK01146; GIK01147; GIK01148; GIK01149; GIK01150; GIK01151; GIK01152; GIK01153; GIK01154; GIK01155; GIK01156; GIK01157; GIK01158; GIK01159; GIK01160; GIK01161; GIK01162; GIK01163; GIK01164; GIK01165; GIK01166; GIK01167; GIK01168; GIK01169; GIK01170; GIK01171; GIK01172; GIK01173; GIK01174; GIK01175; GIK01176; GIK01177; GIK01178; GIK01179; GIK01180; GIK01181; GIK01182; GIK01183; GIK01184; GIK01185; GIK01186; GIK01187; GIK01188; GIK01189; GIK01190; GIK01191; GIK01192; GIK01193; GIK01194; GIK01195; GIK01196; GIK01197; GIK01198; GIK01199; GIK01200; GIK01201; GIK01202; GIK01203; GIK01204; Gravity corer (Kiel type); IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; Latitude of event; Longitude of event; M1; M1_243; M1_245 01051-B; M1_246; M1_249; M1_250; M1_251; M1_252 01057-C; M1_253; M1_254 01059-B; M1_255; M1_256; M1_257; M1_258; M1_259; M1_260; M1_261; M1_262; M1_263; M1_264; M1_265; M1_266; M1_267; M1_268; M1_269; M1_270; M1_271; M1_272; M1_273 01078-A; M1_274; M1_275; M1_276; M1_277; M1_278 01083-B; M1_279 01084-B; M1_280A; M1_280B; M1_280C 01087-B; M1_281 01088-C; M1_282; M1_283; M1_284; M1_285; M1_286 01093-B; M1_287; M1_288; M1_289 01096-B; M1_290; M1_290B; M1_290C; M1_291; M1_292 11101-2; M1_293 11102-3; M1_294; M1_295 11104-2; M1_296 11105-3; M1_297 11106-2; M1_298; M1_299; M1_300; M1_301 11110-2; M1_302 11111-2; M1_303 11112-1; M1_304 11113-2; M1_305 11114-2; M1_306; M1_307; M1_308 11117-2; M1_309; M1_310 11119-2; M1_311 11120-2; M1_312 11121-2; M1_313 11122-2; M1_314; M1_315; M1_316; M1_317; M1_318 01127-B; M1_319 01128-B; M1_320 01129-B; M1_321 01130-B; M1_322; M1_323 11132-1; M1_324; M1_324 11134-1; M1_326 01135-B; M1_327 01136-B; M1_328A 01137-B; M1_328B 01138-B; M1_329; M1_329C 01141-B; M1_330A 01142-B; M1_330B 01143-B; M1_330C 01144-B; M1_331 01145-C; M1_332 01146-B; M1_333; M1_334 01148-B; M1_335 01149-B; M1_336 01150-B; M1_337 01151-B; M1_338 01152-B; M1_339 11053-1; M1_340 01154-B; M1_341 01155-B; M1_342; M1_342A 01156-B; M1_343; M1_344; M1_345; M1_346 01161-B; M1_347A 01162-B; M1_347B 01163-B; M1_347C; M1_348 01165-A; M1_349 01166-B; M1_350; M1_351; M1_352 01173-C; M1_353 01174-B; M1_354 01175-B; M1_355A 01176-B; M1_355B 01177-C; M1_356 01178-C; M1_357 11079-2; M1_358 01180-C; M1_359 11081-2; M1_360 01182-B; M1_361 01183-B; M1_362; M1_363 11085-2; M1_364; M1_365 01187-C; M1_366 11088-1; M1_367; M1_368 01190-C; M1_369; M1_370 11092-2; M1_371; M1_372; M1_373; M1_374 01196-C; M1_375; M1_376 01198-B; M1_377 01199-G; M1_378 01200-B; M1_379; M1_380; M1_381; M1_382; Meteor (1964); Nitrogen, total; Northern Arabian Sea; Persian Gulf; Sample code/label; Sand; Size fraction 〈 0.002 mm, clay; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 2 mm, gravel; Size fraction 0.0063-0.002 mm, fine silt; Size fraction 0.020-0.0063 mm, medium silt; Size fraction 0.063-0.020 mm, coarse silt; SL; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 3719 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 87
    Publication Date: 2024-02-03
    Keywords: Algae, calcareous; BC; Biogenic total, fractionated; Box corer; Bryozoa; Coral; Crustacea; Decapoda; DEPTH, sediment/rock; Dissolvable fraction; Elevation of event; Event label; Fecal pellets; Foraminifera, benthic agglutinated; Foraminifera, benthic calcareous; Foraminifera, planktic; Gastropoda; GIK/IfG; GIK01054; GIK01055; GIK01056; GIK01057; GIK01058; GIK01059; GIK01060; GIK01061; GIK01062; GIK01063; GIK01064; GIK01065; GIK01066; GIK01067; GIK01068; GIK01069; GIK01070; GIK01071; GIK01072; GIK01073; GIK01074; GIK01075; GIK01076; GIK01077; GIK01078; GIK01079; GIK01080; GIK01081; GIK01082; GIK01083; GIK01084; GIK01085; GIK01088; GIK01089; GIK01090; GIK01091; GIK01092; GIK01093; GIK01094; GIK01095; GIK01096; GIK01097; GIK01098; GIK01099; GIK01100; GIK01101; GIK01102; GIK01103; GIK01104; GIK01105; GIK01106; GIK01107; GIK01108; GIK01109; GIK01110; GIK01111; GIK01112; GIK01113; GIK01114; GIK01115; GIK01116; GIK01117-2; GIK01118; GIK01119; GIK01120; GIK01121; GIK01122; GIK01123; GIK01124; GIK01125; GIK01126; GIK01127; GIK01128; GIK01129; GIK01130; GIK01131; GIK01132; GIK01133; GIK01134; GIK01135; GIK01136; GIK01137; GIK01138; GIK01139; GIK01140; GIK01141; GIK01142; GIK01143; GIK01144; GIK01145; GIK01146; GIK01147; GIK01148; GIK01149; GIK01150; GIK01151; GIK01152; GIK01153; GIK01154; GIK01155; GIK01156; GIK01157; GIK01158; GIK01159; GIK01160; GIK01161; GIK01162; GIK01163; GIK01164; GIK01165; GIK01166; GIK01167; GIK01168; GIK01169; GIK01170; GIK01171; GIK01172; GIK01173; GIK01174; GIK01175; GIK01176; GIK01177; GIK01178; GIK01179; GIK01180; GIK01181; GIK01182; GIK01183; GIK01184; GIK01185; GIK01186; GIK01187; GIK01188; GIK01189; GIK01190; GIK01191; GIK01192; GIK01193-3; GIK01194; GIK01195; GIK01196; GIK01197; GIK01198; GIK01199; GIK01200; GIK01201; GIK01202; GIK01203; GIK01204; Gravel, mass netto; Gravity corer (Kiel type); Holothuria; IIOE - International Indian Ocean Expedition; Indeterminata; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; LATITUDE; Light minerals; LONGITUDE; M1; M1_249; M1_250; M1_251; M1_252 01057-C; M1_253; M1_254 01059-B; M1_255; M1_256; M1_257; M1_258; M1_259; M1_260; M1_261; M1_262; M1_263; M1_264; M1_265; M1_266; M1_267; M1_268; M1_269; M1_270; M1_271; M1_272; M1_273 01078-A; M1_274; M1_275; M1_276; M1_277; M1_278 01083-B; M1_279 01084-B; M1_280A; M1_281 01088-C; M1_282; M1_283; M1_284; M1_285; M1_286 01093-B; M1_287; M1_288; M1_289 01096-B; M1_290; M1_290B; M1_290C; M1_291; M1_292 11101-2; M1_293 11102-3; M1_294; M1_295 11104-2; M1_296 11105-3; M1_297 11106-2; M1_298; M1_299; M1_300; M1_301 11110-2; M1_302 11111-2; M1_303 11112-1; M1_304 11113-2; M1_305 11114-2; M1_306; M1_307; M1_308 11117-2; M1_309; M1_310 11119-2; M1_311 11120-2; M1_312 11121-2; M1_313 11122-2; M1_314; M1_315; M1_316; M1_317; M1_318 01127-B; M1_319 01128-B; M1_320 01129-B; M1_321 01130-B; M1_322; M1_323 11132-1; M1_324; M1_324 11134-1; M1_326 01135-B; M1_327 01136-B; M1_328A 01137-B; M1_328B 01138-B; M1_329; M1_329C 01141-B; M1_330A 01142-B; M1_330B 01143-B; M1_330C 01144-B; M1_331 01145-C; M1_332 01146-B; M1_333; M1_334 01148-B; M1_335 01149-B; M1_336 01150-B; M1_337 01151-B; M1_338 01152-B; M1_339 11053-1; M1_340 01154-B; M1_341 01155-B; M1_342; M1_342A 01156-B; M1_343; M1_344; M1_345; M1_346 01161-B; M1_347A 01162-B; M1_347B 01163-B; M1_347C; M1_348 01165-A; M1_349 01166-B; M1_350; M1_351; M1_352 01173-C; M1_353 01174-B; M1_354 01175-B; M1_355A 01176-B; M1_355B 01177-C; M1_356 01178-C; M1_357 11079-2; M1_358 01180-C; M1_359 11081-2; M1_360 01182-B; M1_361 01183-B; M1_362; M1_363 11085-2; M1_364; M1_365 01187-C; M1_366 11088-1; M1_367; M1_368 01190-C; M1_369; M1_370 11092-2; M1_371 11093-3; M1_372; M1_373; M1_374 01196-C; M1_375; M1_376 01198-B; M1_377 01199-G; M1_378 01200-B; M1_379; M1_380; M1_381; M1_382; Meteor (1964); Northern Arabian Sea; Ooids; Ophiuroidea; Ostracoda; Persian Gulf; Plant fragments; Porifera; Pteropoda; Reworked; Sample code/label; Scaphopoda; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 0.063 mm, sand; Size fraction 〉 2 mm, gravel; Size fraction 2.000-0.630 mm, coarse sand; SL; Vertebrata; Worm tubes
    Type: Dataset
    Format: text/tab-separated-values, 5143 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 88
    Publication Date: 2024-02-03
    Keywords: CTD/Rosette; CTD-RO; Density, sigma, in situ; DEPTH, water; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_372; M1_CTD372; Meteor (1964); Oxygen; Persian Gulf; pH; Phosphate; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 89
    Publication Date: 2024-02-03
    Keywords: CTD/Rosette; CTD-RO; Density, sigma, in situ; DEPTH, water; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_373; M1_CTD373; Meteor (1964); Oxygen; Persian Gulf; pH; Phosphate; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 90
    Publication Date: 2024-02-03
    Keywords: CTD/Rosette; CTD-RO; Density, sigma, in situ; DEPTH, water; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_380; M1_CTD380; Meteor (1964); Oxygen; Persian Gulf; pH; Phosphate; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 91
    Publication Date: 2024-02-03
    Keywords: CTD/Rosette; CTD-RO; Density, sigma, in situ; DEPTH, water; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_381; M1_CTD381; Meteor (1964); Oxygen; Persian Gulf; pH; Phosphate; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 92
    Publication Date: 2024-02-03
    Keywords: Algae, calcareous; BC; Biogenic total, fractionated; Box corer; Bryozoa; Coral; Crustacea; Decapoda; DEPTH, sediment/rock; Dissolvable fraction; Elevation of event; Event label; Foraminifera, benthic agglutinated; Foraminifera, benthic calcareous; Foraminifera, planktic; Gastropoda; GIK/IfG; GIK01054; GIK01055; GIK01056; GIK01057; GIK01058; GIK01059; GIK01060; GIK01061; GIK01062; GIK01063; GIK01064; GIK01065; GIK01066; GIK01067; GIK01068; GIK01069; GIK01070; GIK01071; GIK01072; GIK01073; GIK01074; GIK01075; GIK01076; GIK01077; GIK01078; GIK01079; GIK01080; GIK01081; GIK01082; GIK01083; GIK01084; GIK01085; GIK01088; GIK01089; GIK01090; GIK01091; GIK01092; GIK01093; GIK01094; GIK01095; GIK01096; GIK01097; GIK01098; GIK01099; GIK01100; GIK01101; GIK01102; GIK01103; GIK01104; GIK01105; GIK01106; GIK01107; GIK01108; GIK01109; GIK01110; GIK01111; GIK01112; GIK01113; GIK01114; GIK01115; GIK01116; GIK01117-2; GIK01118; GIK01119; GIK01120; GIK01121; GIK01122; GIK01123; GIK01124; GIK01125; GIK01126; GIK01127; GIK01128; GIK01129; GIK01130; GIK01131; GIK01132; GIK01133; GIK01134; GIK01135; GIK01136; GIK01137; GIK01138; GIK01139; GIK01140; GIK01141; GIK01142; GIK01143; GIK01144; GIK01145; GIK01146; GIK01147; GIK01148; GIK01149; GIK01150; GIK01151; GIK01152; GIK01153; GIK01154; GIK01155; GIK01156; GIK01157; GIK01158; GIK01159; GIK01160; GIK01161; GIK01162; GIK01163; GIK01164; GIK01165; GIK01166; GIK01167; GIK01168; GIK01169; GIK01170; GIK01171; GIK01172; GIK01173; GIK01174; GIK01175; GIK01176; GIK01177; GIK01178; GIK01179; GIK01180; GIK01181; GIK01182; GIK01183; GIK01184; GIK01185; GIK01186; GIK01187; GIK01188; GIK01189; GIK01190; GIK01191; GIK01192; GIK01193-3; GIK01194; GIK01195; GIK01196; GIK01197; GIK01198; GIK01199; GIK01200; GIK01201; GIK01202; GIK01203; GIK01204; Gravity corer (Kiel type); Holothuria; IIOE - International Indian Ocean Expedition; Indeterminata; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; LATITUDE; LONGITUDE; M1; M1_249; M1_250; M1_251; M1_252 01057-C; M1_253; M1_254 01059-B; M1_255; M1_256; M1_257; M1_258; M1_259; M1_260; M1_261; M1_262; M1_263; M1_264; M1_265; M1_266; M1_267; M1_268; M1_269; M1_270; M1_271; M1_272; M1_273 01078-A; M1_274; M1_275; M1_276; M1_277; M1_278 01083-B; M1_279 01084-B; M1_280A; M1_281 01088-C; M1_282; M1_283; M1_284; M1_285; M1_286 01093-B; M1_287; M1_288; M1_289 01096-B; M1_290; M1_290B; M1_290C; M1_291; M1_292 11101-2; M1_293 11102-3; M1_294; M1_295 11104-2; M1_296 11105-3; M1_297 11106-2; M1_298; M1_299; M1_300; M1_301 11110-2; M1_302 11111-2; M1_303 11112-1; M1_304 11113-2; M1_305 11114-2; M1_306; M1_307; M1_308 11117-2; M1_309; M1_310 11119-2; M1_311 11120-2; M1_312 11121-2; M1_313 11122-2; M1_314; M1_315; M1_316; M1_317; M1_318 01127-B; M1_319 01128-B; M1_320 01129-B; M1_321 01130-B; M1_322; M1_323 11132-1; M1_324; M1_324 11134-1; M1_326 01135-B; M1_327 01136-B; M1_328A 01137-B; M1_328B 01138-B; M1_329; M1_329C 01141-B; M1_330A 01142-B; M1_330B 01143-B; M1_330C 01144-B; M1_331 01145-C; M1_332 01146-B; M1_333; M1_334 01148-B; M1_335 01149-B; M1_336 01150-B; M1_337 01151-B; M1_338 01152-B; M1_339 11053-1; M1_340 01154-B; M1_341 01155-B; M1_342; M1_342A 01156-B; M1_343; M1_344; M1_345; M1_346 01161-B; M1_347A 01162-B; M1_347B 01163-B; M1_347C; M1_348 01165-A; M1_349 01166-B; M1_350; M1_351; M1_352 01173-C; M1_353 01174-B; M1_354 01175-B; M1_355A 01176-B; M1_355B 01177-C; M1_356 01178-C; M1_357 11079-2; M1_358 01180-C; M1_359 11081-2; M1_360 01182-B; M1_361 01183-B; M1_362; M1_363 11085-2; M1_364; M1_365 01187-C; M1_366 11088-1; M1_367; M1_368 01190-C; M1_369; M1_370 11092-2; M1_371 11093-3; M1_372; M1_373; M1_374 01196-C; M1_375; M1_376 01198-B; M1_377 01199-G; M1_378 01200-B; M1_379; M1_380; M1_381; M1_382; Meteor (1964); Northern Arabian Sea; Ooids; Ophiuroidea; Ostracoda; Persian Gulf; Plant fragments; Porifera; Pteropoda; Sample code/label; Scaphopoda; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 0.063 mm, sand; Size fraction 〉 2 mm, gravel; Size fraction 2.000-0.630 mm, coarse sand; SL; Vertebrata; Worm tubes
    Type: Dataset
    Format: text/tab-separated-values, 4338 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 93
    Publication Date: 2024-02-03
    Keywords: BCR; Box corer (Reineck); Carbon, organic, total; Carbonates; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; GIK/IfG; GIK12327-4; Institute for Geosciences, Christian Albrechts University, Kiel; M25; Meteor (1964); Nitrogen, organic; Phosphorus; Sulfur, total
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 94
    Publication Date: 2024-02-03
    Keywords: Carbon, organic, total; Carbonates; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; GIK/IfG; GIK12379-1; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964); Nitrogen, organic; Phosphorus; Sulfur, total
    Type: Dataset
    Format: text/tab-separated-values, 133 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 95
    Publication Date: 2024-02-03
    Keywords: Alkalinity, total; Bottle, Niskin; Calcium; Chloride; DEPTH, water; East Atlantic; GIK/IfG; GIK12307-2; Institute for Geosciences, Christian Albrechts University, Kiel; M25; Meteor (1964); NIS; Phosphorus, total dissolved; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 96
    Publication Date: 2024-02-03
    Keywords: Alkalinity, total; Ammonia; Calcium; Chloride; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; GIK/IfG; GIK12379-1; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964); Phosphorus, total dissolved; Sulfate; Sulfide
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 97
    Publication Date: 2024-02-03
    Keywords: Alkalinity, total; Ammonia; BCR; Box corer (Reineck); Calcium; Chloride; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; Event label; GIK/IfG; GIK12327-4; GIK12327-5; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964); Phosphorus, total dissolved; Sulfate; Sulfide
    Type: Dataset
    Format: text/tab-separated-values, 178 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 98
    Publication Date: 2024-02-03
    Keywords: Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; GIK/IfG; GIK12310-4; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964); Particle number, fractionated
    Type: Dataset
    Format: text/tab-separated-values, 152 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 99
    Publication Date: 2024-02-03
    Keywords: Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; GIK/IfG; GIK12379-1; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964); Particle number, fractionated
    Type: Dataset
    Format: text/tab-separated-values, 231 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 100
    Publication Date: 2024-02-03
    Keywords: Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dry mass; East Atlantic; GIK/IfG; GIK12310-4; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M25; Meteor (1964); Particle number, fractionated; Sand, mass brutto; Sand, mass netto; Volume
    Type: Dataset
    Format: text/tab-separated-values, 354 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...