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  • American Association for the Advancement of Science  (9,752)
  • Cell Press
  • MDPI
  • Molecular Diversity Preservation International
  • PANGAEA
  • 2020-2023  (241)
  • 1955-1959  (9,790)
Collection
Years
Year
  • 1
    Publication Date: 2023-07-09
    Keywords: Abra antwerpiensis; Acamptpgenotia escheri; Acera bellardii; Acirsa lanceolata; Aclaeon inflatus; Actaeonidea terebelloides; Actaeon semistriatus; Admete fusiformis; Alvania antwerpiensis; Alvania belgica; Amusium woodi; Anadara diluvii; Anadara suessi; Ancilla obsoleta; Ancistrosyrinx cometi; Angulus fallax; Angulus posterus; Anomia epphippium; Aphinotoma debilis; Aporrhais alata; Aporrhais speciosa margerini; Aquilofusus beyrichi; Aquilofusus oppenheimi; Aquilofusus virgineus; Arca pectunculoides; Architectonica carocollatum; Architectonica simplex; Astarle triangularis; Astarte goldfussi; Astarte gracilis; Astarte pygmaea; Astarte radiata; Astenotoma pannus; Asthenotoma basteroti; Asthenotoma colus; Asthenotoma festiva; Asthenotoma pannoides; Aturia aturi; Bathytoma cataphracta; Bathytoma mioturbida; Bittium spina; Borsonia uniplicata; Cadulus gadus; Calliostoma laureatum; Calliostoma muelleri; Calyptraea chinensis; Cancellaria aperta; Cancellaria behmi; Cancellaria beyrichi; Cancellaria calais; Cancellaria cancellata praecedens; Cancellaria contorta; Cancellaria mitraeformis parvula; Cancellaria umbilicaris pluricostata; Cancellaria varicosa; Capulus striatulus; Capulus ungaricus; Cardita chamaeformis; Cardita squamulosa; Cardium danubianum; Cardium hanseatum; Cardium papillosum; Cardium straeleni; Cerithella genei; Cerithiopsis subsoluta; Chama gryphaeoides; Chlamys angelonii; Chlamys edegemensis; Chlamys ercolanianus; Chlamys lilli; Chlamys radians; Chlamys spinulosus duwelzi; Chlamys tigerinus; Chrysallida pygmaea; Cingula proxima; Circulus hennei; Circulus praecedens; Circulus striatus; Clavatula boreointerrupta; Clavatula boreoromana; Clavatula hemmoorensis; Clavatula obliquiplicatula; Clavatula olgae; Clavus bicingulatus; Clavus borealis; Clavus diensti; Clavus hannoveranus; Clavus obtusangulus; Clavus selenkae; Clavus terebra intermedia; Conus dujardini; Corbula basteroti; Corbula gibba; Corbulamya donaciformis; Crepidula cvepidula; Cuspidaria costellata; Cuspidaria cuspidata; Cylichna cylindracea; Cymatium tarbellianum; Daphnella anceps; Daphnella grippi; Daphnella rappardi; Daphnella scabra; Daphnella zetes; Dentalium dollfussi; Dentalium entale; Dentalium michelotti; Dentalium novemcostatum mutabile; Dentalium vitreum; Distorsio tortuosum; Donax intermedius; Dorsanum boreobaccatum; Dosinia basteroti; Ensis ensis; Ervilia pusilla; Erycina degrangii; Eulimella acicula; Eulimella hoernesi; Eulimella neumayri; Exilia contigua; Genota ramosa elisae; Genota ramosa parvicarinata; Globularia compressa; Glycimeris pilosa; Gouldia minima; Haedropleura maitreja; Hydrobia antwerpiensis; Isocardia lunulata; Isocardia punctata; Laevicardium cyprium; Lathyrus rothi; Leda emarginata; Leda pygmaea; Leda westendorpi; Lepton transversarium; Lienardia boehmi; Lienardia elatior; Lienardia luisae; Lienardia textilis; Lima subauriculata; Limopsis aradasi; Limopsis aurita; Limopsis lamellata; Liomesus pompeckyi; Lucina fragilis; Lutetia nitida; Mangilia g¸richi; Mangilia miorugulosa; Mangilia roemeri; Mangilia tenella; Martesia rugosa; Melanella lactea; Melanella polita; Mitra bellardii; Mitra grateloupi; Mitra planicosta; Modiolus phaseolinus; Momtacuta truncata; Montacuta coarctata; Murex delbosianus scalariformis; Murex inornatus; Murex nysti; Murex spinicosta; Musculus sp.; Mytilus fuscus; Nassa cavata; Nassa cymbrica; Nassa facki; Nassa holsatica; Nassa polsensis; Nassa prismatica; Nassa schroederi; Nassa scklotheimi; Nassa serraticosta; Nassa tenuistriata; Nassa tumida crassispiralis; Nassa turbinella; Natica beyrichi; Natica hayiseata; Niso terebellum acarinatoconica; Nucula haesendoncki; Nucula jeffreysi; Nucula laevigata; Nucula nucleus; Odostomia conoidea; Oliva dufresnei procera; Opalia pertusa; Opalia straeleni; Opalia torulosa perconica; Ostrea cochlear; Ostrea digitalina; Pandora inaequivalvis; Panopaea menardi; Pecten brummeIi; Pecten subbenedictus; Peratotoma hosiusi; Phacoides borealis; Phacoides dentatus laevigatas; Phacoides droueti; Phalium bicoronatum; Phalium miolaevigatum; Philbertia reticulata; Phos decussatus; Pinna pectinata; Pirula condita; Pirula simplex; Pitar chionoides; Pitar cimbrica; Pitar incrassata nysti; Pitar rudis; Polynices catena helicina; Polynices catena johannae; Polynices miopusilla; Polynices olla; Polynices submamillaris dertomamilla; Polynices varians protractus; Potamides tricinctus; Pteria phalaenacea; Pyramidella plicosa; Pyrene corrugata; Pyrene nassoides; Pyrgulina cimbrica; Raphitoma plicatella; Retusa elongata; Retusa truncatula; Ringicula auriculata buccinea; Ringicula auriculata ventricosa; Ringicula costata; Sabatia utricula; Sample comment; Sandbergeria wolffi; Saxicava arctica; Scacchia cimbrica; Scala amoena subreticula; Scala crassicostata; Scala crebricostellata; Scala frondicula; Scala procomitalis; Scala sallomacensis nordica; Scala weyersi; Scaphander grateloupi; Scaphella bolli; Schleswig-Holstein, Germany; Scurria compressiuscula; Seila trilineata; S-H; Sigaretus aquensis deshayesi; Sipho grippi; Solariella miosuturalis; Solariella straeleni; Solariella tournoueri; Solenocurtus basteroti; Spiratella atlanta; Spisula subtruncata triangula; Streptochetus sexcostatus; Strombiformis taurinensis; Taras trigonulus; Teinostoma hanseata; Terebra acuminata; Terebra basteroti; Terebra hoernesi; Terebra neglecta; Thapsiella costulata; Thracia ventricosa; Thyasira flexuosa; Tornus dollfussi; Triphora fritschi; Trophon vaginatus semperi; Turbonilla amoena; Turbonilla densecostata; Turbonilla elegantissima gastaldi; Turbonilla miomutinensis; Turbonilla miostriatula edegemensis; Turbonilla pseudoauricula; Turbonilla pseudoterebralis; Turricula steinvorthi; Turris boreoturricula; Turris coronata; Turris denticula borealis; Turris duchasteli flexiplicata; Turris inermis; Turris stoffelsi; Turris zimmermanni; Turritella eryna; Turritella geinitzi; Turritella subangulata; Typhis fistulosus; Vaginella depressa; Venus multilamella; Venus ovata; Vermetus intortus woodi; Vexillum aciculum; Vexillum cimbricum; Volvula acuminata; Xenophora deshayesi; Yoldia glaberrima
    Type: Dataset
    Format: text/tab-separated-values, 294 data points
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  • 2
    Publication Date: 2023-07-09
    Keywords: Acamptogenotia straeleni; Admete subangulosa; Anadara diluvii; Aporrhais alata; Aquilofusus semiglaber; Arca pectunculoides; Astarte fusca; Astarte reimersi; Astarte waeli; Asthenotoma festiva; Bathytoma cataphracta; Bathytoma mioturbida; Cancellaria rothi; Cardita orbicularis; Cardium papillosum; Chlamys radians; Clavus obeliscus; Clavus obtusangulus; Clavus staringi; Conus antediluvianus; Corbula gadus; Corbula gibba; Counting; Cylichna cylindracea; Drillia modiola; Gauss-Krueger Hochwert; Gauss-Krueger Rechtswert; Gauss-Krueger Streifen; Isocardia forchhammeri; Leda pygmaea; Mangelia sp.; Murex spinicosta; Nassa prismatica; Nassa syltensis; Natica koeneni; Nucula jeffreysi; Nucula laevigata; Phalium miolaevigatum; Philbertia reticulata; Pyramidella plicosa; Pyrene nassoides; Ringicula auriculata; Sabatia utricula; Sample ID; Scala frondicula; Schleswig-Holstein, Germany; Sipho distinctus; Spisula subtruncata triangula; Streptochetus sexcostatus; Terebra forchhammeri; Trophon vaginatus semperi; Turbonilla densecostata; Turris annae; Turris aquensis; Turris badensis; Turris helena; Turritella tricarinata; Turritella triplicata; Typhis fistulosus; Uetersen; Venus multilamella; Xenophora testigera; Yoldia glaberrima
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 3
    Publication Date: 2023-07-09
    Keywords: Abra antwerpiensis; Acamptpgenotia escheri; Acera bellardii; Acirsa lanceolata; Aclaeon inflatus; Actaeonidea terebelloides; Actaeon semistriatus; Admete fusiformis; Alvania antwerpiensis; Alvania belgica; Amusium woodi; Anadara diluvii; Anadara suessi; Ancilla obsoleta; Ancistrosyrinx cometi; Angulus fallax; Angulus posterus; Anomia epphippium; Aphinotoma debilis; Aporrhais alata; Aporrhais speciosa margerini; Aquilofusus beyrichi; Aquilofusus oppenheimi; Aquilofusus virgineus; Arca pectunculoides; Architectonica carocollatum; Architectonica simplex; Astarle triangularis; Astarte goldfussi; Astarte gracilis; Astarte pygmaea; Astarte radiata; Astenotoma pannus; Asthenotoma basteroti; Asthenotoma colus; Asthenotoma festiva; Asthenotoma pannoides; Aturia aturi; Bathytoma cataphracta; Bathytoma mioturbida; Behrendorf; Bittium spina; Borsonia uniplicata; Cadulus gadus; Calliostoma laureatum; Calliostoma muelleri; Calyptraea chinensis; Cancellaria aperta; Cancellaria behmi; Cancellaria beyrichi; Cancellaria calais; Cancellaria cancellata praecedens; Cancellaria contorta; Cancellaria mitraeformis parvula; Cancellaria umbilicaris pluricostata; Cancellaria varicosa; Capulus striatulus; Capulus ungaricus; Cardita chamaeformis; Cardita squamulosa; Cardium danubianum; Cardium hanseatum; Cardium papillosum; Cardium straeleni; Cerithella genei; Cerithiopsis subsoluta; Chama gryphaeoides; Chlamys angelonii; Chlamys edegemensis; Chlamys ercolanianus; Chlamys lilli; Chlamys radians; Chlamys spinulosus duwelzi; Chlamys tigerinus; Chrysallida pygmaea; Cingula proxima; Circulus hennei; Circulus praecedens; Circulus striatus; Clavatula boreointerrupta; Clavatula boreoromana; Clavatula hemmoorensis; Clavatula obliquiplicatula; Clavatula olgae; Clavus bicingulatus; Clavus borealis; Clavus diensti; Clavus hannoveranus; Clavus obtusangulus; Clavus selenkae; Clavus terebra intermedia; Conus dujardini; Corbula basteroti; Corbula gibba; Corbulamya donaciformis; Crepidula cvepidula; Cuspidaria costellata; Cuspidaria cuspidata; Cylichna cylindracea; Cymatium tarbellianum; Daphnella anceps; Daphnella grippi; Daphnella rappardi; Daphnella scabra; Daphnella zetes; Dentalium dollfussi; Dentalium entale; Dentalium michelotti; Dentalium novemcostatum mutabile; Dentalium vitreum; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Distorsio tortuosum; Donax intermedius; Dorsanum boreobaccatum; Dosinia basteroti; Ensis ensis; Ervilia pusilla; Erycina degrangii; Eulimella acicula; Eulimella hoernesi; Eulimella neumayri; Event label; Exilia contigua; Gauss-Krueger Hochwert; Gauss-Krueger Rechtswert; Gauss-Krueger Streifen; Genota ramosa elisae; Genota ramosa parvicarinata; Globularia compressa; Glycimeris pilosa; Gouldia minima; Großenwiehe; Haedropleura maitreja; Hydrobia antwerpiensis; Isocardia lunulata; Isocardia punctata; Laevicardium cyprium; Lathyrus rothi; Leda emarginata; Leda pygmaea; Leda westendorpi; Lepton transversarium; Lienardia boehmi; Lienardia elatior; Lienardia luisae; Lienardia textilis; Lima subauriculata; Limopsis aradasi; Limopsis aurita; Limopsis lamellata; Liomesus pompeckyi; Lucina fragilis; Lutetia nitida; Mangilia g¸richi; Mangilia miorugulosa; Mangilia roemeri; Mangilia tenella; Martesia rugosa; Melanella lactea; Melanella polita; Mitra bellardii; Mitra grateloupi; Mitra planicosta; Modiolus phaseolinus; Momtacuta truncata; Montacuta coarctata; Murex delbosianus scalariformis; Murex inornatus; Murex nysti; Murex spinicosta; Musculus sp.; Mytilus fuscus; Nassa cavata; Nassa cymbrica; Nassa facki; Nassa holsatica; Nassa polsensis; Nassa prismatica; Nassa schroederi; Nassa scklotheimi; Nassa serraticosta; Nassa tenuistriata; Nassa tumida crassispiralis; Nassa turbinella; Natica beyrichi; Natica hayiseata; Niso terebellum acarinatoconica; Nucula haesendoncki; Nucula jeffreysi; Nucula laevigata; Nucula nucleus; Odderade; Odostomia conoidea; Oliva dufresnei procera; Opalia pertusa; Opalia straeleni; Opalia torulosa perconica; Ostrea cochlear; Ostrea digitalina; Oxlund; Pandora inaequivalvis; Panopaea menardi; Pecten brummeIi; Pecten subbenedictus; Peratotoma hosiusi; Phacoides borealis; Phacoides dentatus laevigatas; Phacoides droueti; Phalium bicoronatum; Phalium miolaevigatum; Philbertia reticulata; Phos decussatus; Pinna pectinata; Pirula condita; Pirula simplex; Pitar chionoides; Pitar cimbrica; Pitar incrassata nysti; Pitar rudis; Polynices catena helicina; Polynices catena johannae; Polynices miopusilla; Polynices olla; Polynices submamillaris dertomamilla; Polynices varians protractus; Potamides tricinctus; Pteria phalaenacea; Pyramidella plicosa; Pyrene corrugata; Pyrene nassoides; Pyrgulina cimbrica; Raphitoma plicatella; Retusa elongata; Retusa truncatula; Ringicula auriculata buccinea; Ringicula auriculata ventricosa; Ringicula costata; Sabatia utricula; Sample ID; Sandbergeria wolffi; Saxicava arctica; Scacchia cimbrica; Scala amoena subreticula; Scala crassicostata; Scala crebricostellata; Scala frondicula; Scala procomitalis; Scala sallomacensis nordica; Scala weyersi; Scaphander grateloupi; Scaphella bolli; Schleswig-Holstein, Germany; Scurria compressiuscula; Seila trilineata; Sigaretus aquensis deshayesi; Sipho grippi; Solariella miosuturalis; Solariella straeleni; Solariella tournoueri; Solenocurtus basteroti; Spiratella atlanta; Spisula subtruncata triangula; Streptochetus sexcostatus; Strombiformis taurinensis; Suederhastedt; Taras trigonulus; Teinostoma hanseata; Terebra acuminata; Terebra basteroti; Terebra hoernesi; Terebra neglecta; Thapsiella costulata; Thracia ventricosa; Thyasira flexuosa; Tornus dollfussi; Triphora fritschi; Trophon vaginatus semperi; Turbonilla amoena; Turbonilla densecostata; Turbonilla elegantissima gastaldi; Turbonilla miomutinensis; Turbonilla miostriatula edegemensis; Turbonilla pseudoauricula; Turbonilla pseudoterebralis; Turricula steinvorthi; Turris boreoturricula; Turris coronata; Turris denticula borealis; Turris duchasteli flexiplicata; Turris inermis; Turris stoffelsi; Turris zimmermanni; Turritella eryna; Turritella geinitzi; Turritella subangulata; Typhis fistulosus; Vaginella depressa; Venus multilamella; Venus ovata; Vermetus intortus woodi; Vexillum aciculum; Vexillum cimbricum; Vioel; Volvula acuminata; Xenophora deshayesi; Yoldia glaberrima
    Type: Dataset
    Format: text/tab-separated-values, 3574 data points
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Niino, Hiroshi (1955): On a manganese nodule and Perotrochus beyrichii dredged from the banks near the Izu Islands. Records of Oceanographic works in Japan, 2(2), 120-126, hdl:10013/epic.47489.d001
    Publication Date: 2023-08-28
    Description: Manganese nodules have been found by the author in the shallow waters of the Hyotan-se bank west of Shikime-jima, an island of the Izu archipelago in the Sea of Japan. The slopes around the bank are steep and rocks are exposed; gravels and coarse material cover the broad and flat plain on its top; andesite and basalt, which are very common in the bedrock, are found mingled with liparite gravels together with a number of manganese concretions from the bank.
    Keywords: Dredge; DRG; Hakuho-Maru; HAM_1968-1976; JAPAN_B; Japan Sea; Niino_9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Goldberg, Edward D; Arrhenius, Gustaf (1958): Chemistry of Pacific pelagic sediments. Geochimica et Cosmochimica Acta, 13(2-3), 153-212, https://doi.org/10.1016/0016-7037(58)90046-2
    Publication Date: 2023-08-28
    Description: The chemical and mineralogical composition of pelagic sediments from the East Pacific Ocean has been determined with the aim of defining the ultimate sources and the mechanisms of formation of the solid phases. The distribution of elements between sea-water, the pore solution and the various solid components of the sediments permits interpretations of the variations in time and space of the gross chemical composition of pelagic clays. For example, manganese, present in sea-water in a divalent form, is apparently oxidized at the sediment-water interface to tetravalent species which subsequently become a part of the group of ferromanganese oxide minerals which are found in the marine environment. It is suggested the rate of manganese accumulation in sediments is some function of the length of time the sediment surface is in contact with sea-water. The contribution of chemical species from the different geospheres is considered. The quantitative importance of pelagic clays in the major sedimentary cycle is studied on the basis of the distribution of the weathered igneous rock products between continental and pelagic deposits and sea-water. These analyses of a wide variety of pelagic clays allow a reformulation of the geochemical balance and it is concluded that pelagic clays account for approximately 13 per cent of the total mass of sediments produced over geologic time.
    Keywords: 08995002-SC11; Barium; Boron; Calcium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; File name; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; San Clemente Basin, Pacific ocean; Strontium; Tin; Titanium; Uniform resource locator/link to image; Vanadium; X-ray microanalyzer analysis (XMA); Ytterbium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1958): Drift Station Alpha - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2023-08-28
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) on the Drift Station Alpha in the Arctic Ocean from August 1957 until June 1958. A total of 16 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Arctic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DSA-10; DSA-12; DSA-5; DSA-9; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to metadata file
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 7
    Publication Date: 2023-08-28
    Description: Deposits of manganese ore have been found in five of the six provinces of Cuba and have been reported from the sixth. Only Oriente and Pinar del Rio provinces have more than a few known deposits and only the deposits of Oriente have yielded any appreciable amount of ore. In this area the Cobre formation, of late Cretaceous(?) to middle Eocene age, overlies the Vinent formation but their stratigraphie relations are unknown. The Cobre overlies unconformably the Habana(?) formation. The Cobre formation consists of andesitic, basaltic, and dacitic tuff, agglomerate, and lavas with minor amounts of marine clastic and limestone deposits, and a prominent limestone bed, the Charco Redondo limestone member, at the top of the formation. All productive manganese deposits of Oriente are in the Cobre formation, usually within a few tens of meters above or below the base of the Charco Redondo limestone member.
    Keywords: Charco_Redondo_S; Comment; Cuba; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Guanaba_S; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Ponupo_S; Position; Quantity of deposit; Quinto_S; Sample ID; Sediment type; Size; Substrate type; Taratana_S
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 8
    Publication Date: 2023-08-28
    Description: Saipan, situated about 15° N. and 146° E., is one of the larger and more southerly of the Mariana Islands. The 15 small islands of this chain are strung along an eastwardly convex ridge for more than 400 miles north to south, midway between Honshu and New Guinea and about 1,200 miles east of the Philippines. Paralleling this ridge 60 to 100 miles further east is a deep submarine trench, beyond which lies the Pacific Basin proper. To the west is the Philippine Sea, generally deeper than 2,000 fathoms. The trench coincides with a zone of negative gravity anomalies, earthquake foci occur at increasing depths westward from it, and silica- and alumina-rich volcanic rocks characterize the emergent island chain itself. The contrast between these features and those of the Pacific Basin proper to the east is held to favor the conclusion that the Mariana island arc and trench define the structural and petrographic front of Asia.
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; Mariana Islands; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Papago_C; Position; Quantity of deposit; Sample ID; Sediment type; Size
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: Jones, L H P; Milne, Angela A (1956): Birnessite, a new manganese oxide mineral from Aberdeenshire, Scotland. Mineralogical Magazine, 31(235), 283-288, https://doi.org/10.1180/minmag.1956.031.235.01
    Publication Date: 2023-08-28
    Description: A manganese pan near Birness contains grains of an optically uniaxial negative mineral near (Na0.7Ca0.3)Mn7O14·2·8H2O, giving an X-ray powder pattern similar to that of synthetic materials described as 'manganous manganite' and delta-MnO2. Material giving a similar pattern has been described from a natural occurrence in Canada, but no mineral name was assigned; the name birnessite is now proposed. The mineral is probably formed by air-oxidation of manganous oxides under alkaline conditions.
    Keywords: Aluminium oxide; Birness_J; Calcium oxide; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese dioxide; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Scotland; Sediment type; Silicon dioxide; Sodium oxide; Titanium dioxide; Water in rock
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Dietz, Robert S (1955): Manganese deposits on the northeast Pacific sea floor. California Journal of Mines and Geology, 51(3), 209-220, https://archive.org/details/californiajourna53cali
    Publication Date: 2023-08-28
    Description: Sea floor dredging by the H.M.S. Challenger, the U.S.S. Albatross, the U.S.S. EPC(R) 857, and vessels of the Scripps Institution of Oceanography shows that extensive deposits of manganese nodules are on the deep sea floor and that crusts of manganese dioxide cover many seamounts. Sea floor photography reveals that in some places these crusts are quite continuous and the nodules are closely packed. These crusts and nodules are fully oxidized and hydrated mixtures of man¬ganese and iron plus earthy impurities. Also, relatively high concen¬trations of the trace elements nickel, copper, and cobalt are present.
    Keywords: DICH-SS; Dredge; Dredge, rock; DRG; DRG_R; Erben Seamount, Pacific Ocen; GOLDHW1; Horizon; MDPC02HO-MP-025F-2; MDPC02HO-MP-026A-3; MDPC02HO-MP-037A; MIDPAC; MPC-25F-2; MPC-26A-3; MPC-37A; NEL-667; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D1; NTHL-D7; Pacific Ocean; Sylvania Seamount, Pacific Ocean; Wired profile sonde; WP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 11
    Publication Date: 2023-08-28
    Description: The Kara scientific expedition of 1945, using the fishing trawler M. Gorkiy and survey vessel Osetr, took sediment samples in the Kara Sea in addition to other oceanographic work. The investigations of sediments composition was compared with biological and hydrological data obtained in the same areas. The sediments sampled were subjected to mechanical, mineralogical, chemical and faunistic analyses. During this survey iron-manganese concretions were recovered.
    Keywords: Deposit type; DEPTH, sediment/rock; Description; EG; Ekman grab; Elevation of event; Event label; GORK45-10; GORK45-11; GORK45-14; GORK45-16; GORK45-17; GORK45-18; GORK45-19; GORK45-20; GORK45-21; GORK45-30; GORK45-32; GORK45-37; GORK45-39; GORK45-4; GORK45-7; GORK45-8; Gorkiy1945; Identification; Kara Sea; Latitude of event; Longitude of event; Maxim Gorkiy; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Peterson grab; PETG; Position; Quantity of deposit; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
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  • 12
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    In:  Supplement to: Hurley, RJ (1956): Expedition CHINOOK I, Lowering log, June-August 1956. University of California, Scripps Institution of Oceanography, Unpublished, hdl:10013/epic.46558.d001
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken during the CHINOOK Expedition in July to August 1956 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 20 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: CHIN02BD; CHIN02BD-013GA; CHIN02BD-016G; CHIN0ABD-001G; CHIN0ABD-002G; CHIN0ABD-004G; CHIN0ABD-006G; CHIN0ABD-007G; CHINOOK; CHNK-13G; CHNK-16G; CHNK-18G; CHNK-1G; CHNK-2G; CHNK-4G; CHNK-6G; CHNK-7G; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Size; Spencer F. Baird; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 13
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    In:  Supplement to: Bruun, Anton F (1959): General introduction to the reports and list of deep-sea stations. in: Galathea Report - Scientific Results of the Danish Deep Sea Expedition Round the World. 1950-1952, Danish Science Press, Copenhagen, Denmark, 7-48
    Publication Date: 2023-08-28
    Description: The Danish Expedition of the "Galathea II" around the world brought important results concerning the marine organisms in the deep sea. The "Galathea II" showed not only different organisms of the Abyssal but for the first time of the deepest trenches of the western Pacific. Anton Bruun coined the term Hadal for the region below the Abyssal under 6000 m. Although the "Galathea II" aimed to investigate new deep sea regions beside the routes of former expeditions and to widen the horizon of knowledge relating marine organisms the technical equipment and the methodological approach had partly been developed earlier. The expedition of the "Galathea II" is part of a long tradition of cruises such as that of the British "Challenger", the German "Valdivia" and the Swedish "Albatross" and especially the Danish cruises of the "Dana I" and "Dana II" which happened some years before.
    Keywords: Banda Sea; Comment; Core; CORE; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GAL_1950-1952_Denmark; Galathea; GALT-179; GALT-182; GALT-435; GALT-469; GALT-494; GALT-574; GALT-658; GALT-724; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Philippine Sea; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Tasman Sea
    Type: Dataset
    Format: text/tab-separated-values, 73 data points
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  • 14
    Publication Date: 2023-08-28
    Description: The cores described in this list were taken on the THETA-1 (TH1) Expedition in June to September 1956 from the R/V Theta. A total of 19 cores and dredges were recovered and are archived at Scripps for sampling and study.
    Keywords: Atlantic Ocean; C-58; C-60; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; TH1; TH1-57SCC; TH1-59SCC; TH1-TR4; TH1-TR6; TH1-TR7; Theta; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 15
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1959): FANFARE Expedition 1959, List of cores and dredge samples copied from shipboard logs (R/V H. M. Smith and R/V Spencer F. Baird). Scripps Institution of Oceanography, UC San Diego, unpublished, 6 pp, https://www.ngdc.noaa.gov/mgg/geology/data/1599/15995003/15995003.pdf
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken on the FANFARE Expedition in July 1959 by Scripps Institution of Oceanography from the R/V H. M. Smith and the R/V Spencer F. Baird. A total of 49 cores and dredges were recovered and are available at Scripps for sampling and study. The coring sites, all in the eastern tropical central Pacific.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge, chain bag; DRG_C; Elevation of event; Event label; FANB01BD; FANB01BD-024G; FANBD-20D; FANBD-24G; FANBD-25D; FANFARE-B; FANFARE-S; FANS01HMS; FANS01HMS-016G; FANS-16G; GC; Gravity corer; H.M. Smith; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Size; Spencer F. Baird; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 16
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    In:  Supplement to: Bramlette, M; Faughn, James L; Hurley, RJ (1959): Anomalous sediment deposition on the flank of Eniwetok Atoll. Geological Society of America Bulletin, 70(12), 1549-1552, https://doi.org/10.1130/0016-7606(1959)70%5B1549:ASDOTF%5D2.0.CO;2
    Publication Date: 2023-08-28
    Description: Some short cores from the shelf at about 800-1000 fathoms on the southwest flank of Eniwetok Atoll penetrated Pliocene deposits with little to no later sediment cover. The Quaternary deposits include much coarse reef debris, particularly the fragments of algae such as Halimeda and other shallow-water material up to several millimeters in grain size, mixed with varying amounts of pelagic Foraminifera. The Pliocene sediments (one may be upper Miocene) are pure pelagic deposits of much finer grain size, consisting of coccoliths and pelagic Foraminifera with no admixture of reef material. Bottom photographs show areas of well-developed ripple marks in coarse sediment (C. J. Shipek, manuscript) apparently formed only in the areas with the veneer of post-Tertiary coarse sediments. A brown impregnation at the top and extending down as mottling for a few centimeters is also usual in the Tertiary sediment of the cores. This seems to consist of iron and manganese oxides and adds somewhat to the induration.
    Keywords: 10-J1268; 10-J1269; 10-J1270; 10-J1271; 10-J1272; 10-J1273; 10-J1274; 10-J1275; 11-J1276; 3-J1225; 3-J1226; 3-J1227; 3-J1228; 4-J1230; 4-J1231; 4-J1232; 4-J1233; 4-J1234; 4-J1235; 6-J1237; 6-J1238; 6-J1239; 6-J1240; 6-J1241; 6-J1242; 6-J1243; 6-J1244; 8-J1260; 8-J1261; 8-J1262; 8-J1263; 8-J1264; 8-J1265; 8-J1266; Comment; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; ENIW10PH-1268; ENIW10PH-1269; ENIW10PH-1270; ENIW10PH-1271; ENIW10PH-1272; ENIW10PH-1273; ENIW10PH-1274; ENIW10PH-1275; ENIW11PH-1276; ENIW20C; ENIW27C; ENIW3PH-1225; ENIW3PH-1226; ENIW3PH-1227; ENIW3PH-1228; ENIW4C; ENIW4PH-1230; ENIW4PH-1231; ENIW4PH-1232; ENIW4PH-1233; ENIW4PH-1234; ENIW4PH-1235; ENIW6PH-1237; ENIW6PH-1238; ENIW6PH-1239; ENIW6PH-1240; ENIW6PH-1241; ENIW6PH-1242; ENIW6PH-1243; ENIW6PH-1244; ENIW8PH-1260; ENIW8PH-1261; ENIW8PH-1262; ENIW8PH-1263; ENIW8PH-1264; ENIW8PH-1265; ENIW8PH-1266; ENIWETOK_Operation; Eniwetok Atoll, Central Pacific; Event label; H.M. Smith; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 341 data points
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  • 17
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1959): Expedition VEMA 15. Lamont Geological Observatory, Columbia University, New York, unpublished, 26 pp, https://www.ngdc.noaa.gov/mgg/curator/data/vema/vm15/vm15_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 15 Expedition from October 1958 until July 1959 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 410 cores and dredges were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; 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; Sample ID; Sediment type; Size; Substrate type; TRAWL; Trawl net; V15; V15-003PD; V15-101; V15-119SBT; V15-120SBT; V15-122SBT; V15-125SBT; V15-129; V15-130; V15-131; V15-135; V15-135SBT; V15-136; V15-138; V15-144; V15-151SBT; V15-160; V15-187; V15-188; V15-197; V15-202; V15-30; V15-40; V15-44A; V15-45; V15-47; V15-48; V15-61SBT; V15-66; V15-77SBT; V15-78SBT; V15-79SBT; V15-8; V15-80SBT; V15-81SBT; V15-82SBT; V15-95SBT; Vema
    Type: Dataset
    Format: text/tab-separated-values, 698 data points
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  • 18
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    In:  Supplement to: Ericson, D; Baker, RN; Goldstein, RF (1955): Vema Cruise 07 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 8 pp, https://www.ngdc.noaa.gov/mgg/geology/data/vema/vm07/vm07_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 7 Expedition from May until September 1955 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 78 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; V07; V07-25; V07-61; V07-71; V07-8; Vema
    Type: Dataset
    Format: text/tab-separated-values, 50 data points
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  • 19
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    In:  Supplement to: Hekinian, Roger; Starkes, J; Ericson, D (1956): Vema Cruise 09 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, 40 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 9 Expedition from February until April 1958 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 34 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; TC; Trigger corer; V09; V09-13TW; V09-15; V09-16; V09-18; V09-2; V09-21; V09-26; V09-28; V09-33; V09-9; Vema
    Type: Dataset
    Format: text/tab-separated-values, 138 data points
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  • 20
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    In:  Supplement to: Ericson, D; Morgenstein, M; Grinnell, R (1956): Vema Cruise 10 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 145 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 10 Expedition from June until September 1956 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 95 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; V10; V10-1; V10-11; V10-19; V10-20; V10-21; V10-32; V10-42; V10-50; V10-6; V10-65; V10-72; V10-77; V10-78; V10-80; V10-82; V10-83; V10-88; V10-95; V10-97; V10-99; Vema
    Type: Dataset
    Format: text/tab-separated-values, 254 data points
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  • 21
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1957): Vema Cruise 12 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 87 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 12 Expedition from December 1956 until August 1957 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 119 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; V12; V12-1; V12-101; V12-103; V12-104; V12-107; V12-108; V12-109; V12-111; V12-114; V12-115; V12-116; V12-117; V12-120; V12-121; V12-127; V12-128; V12-14; V12-19; V12-20; V12-22; V12-52; V12-54; V12-56; V12-65; V12-72; V12-73; V12-80; V12-85; V12-93; V12-96; V12-97; V12-98; V12-99; Vema
    Type: Dataset
    Format: text/tab-separated-values, 377 data points
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  • 22
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    In:  Supplement to: Kuno, Hisashi; Fisher, Robert L; Nasu, Noriyuki (1956): Rock fragments and pebbles dredged near Jimmu Seamount, northwestern Pacific. Deep Sea Research, 3(2), 126-133, https://doi.org/10.1016/0146-6313(56)90090-9
    Publication Date: 2023-08-28
    Description: Fifty-five rock fragments and pebbles were dredged at 2,550-2,800 fathoms (4,650-5,100 metres) near Jimmu Seamount, 700 miles southeast of Kamchatka. Tuffaceous shale, andesitic and dacitic tuff, pyroxene-hornblende dacite-pumice, and augite-hypersthene andesite are the most abundant rock types. Minor constituents in the haul include augite-pigeonite basalt, augite-olivine basalt, olivine dolerite, quartz syenite porphyry, metabasalt, sandstone, and chert. Petrographic and chemical analyses indicate closer affinities with Kuril Islands and Kamchatka volcanic rocks than with Cenozoic Japanese or Pacific Basin types. Probably these rocks were dropped by Pleistocene icebergs carried south and east by ocean currents.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Spencer F. Baird; Substrate type; TRAN_JG; TRANSPAC; Trans-Pacific; Uniform resource locator/link to image; Western Pacific
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
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  • 23
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    In:  Supplement to: Ljunggren, P (1955): Geochemistry and radioactivity of some Mn and Fe bog ores. Geologiska Föreningens i Stockholm förhandlingar: GFF (The transactions of the Geological Society of Sweden, 77(1), 33-44, https://doi.org/10.1080/11035895509455349
    Publication Date: 2023-08-28
    Description: The trace element content of different bog ores has been measured and it appeared that most of these elements are enriched in the manganiferous bog ores as compared with the ferriferous ones. The manganiferous bog ores have also proved to have a higher radioactivity than the ferriferous ones.
    Keywords: Barium; Beryllium; Boron; Caesium; Chromium; Cobalt; DEPTH, sediment/rock; Description; Detector raw counts; Event label; Geiger counter; Identification; Iron oxide, Fe2O3; Lake Tisjoen, Sweden; Lead; Lika_L; Manganese dioxide; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium; River Lika, Sweden; Rubidium; Strontium; Tisjoen_L; Vanadium; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 181 data points
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  • 24
    Publication Date: 2023-08-28
    Keywords: Cerium oxide; CHA-276; Challenger1872; DEPTH, sediment/rock; Description; Grab; GRAB; H.M.S. Challenger (1872); Mercury oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample code/label; Thorium oxide
    Type: Dataset
    Format: text/tab-separated-values, 5 data points
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  • 25
    Publication Date: 2023-08-28
    Keywords: 248; CHA-248; CHA-252; CHA-276; Challenger1872; DEPTH, sediment/rock; Description; Event label; Grab; GRAB; H.M.S. Challenger (1872); Insoluble material; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Sample code/label; Soluble residue; TRAWL; Trawl net
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 26
    Publication Date: 2023-08-28
    Keywords: 248; CHA-248; CHA-252; CHA-276; Challenger1872; Deposit type; DEPTH, sediment/rock; Description; Event label; Feature; Grab; GRAB; H.M.S. Challenger (1872); NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Station label; Substrate type; TRAWL; Trawl net; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 27
    Publication Date: 2023-08-28
    Keywords: ALB-13; Albatross (1882-1921); Albatross1899-1900; ALBTR-13; Colorimetry; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Fluorescence radiometry; Iron; Manganese dioxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Radium; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 28
    Publication Date: 2023-08-28
    Keywords: Albatross (1882-1921); Albatross1904-1905; ALBTR-4658; Colorimetry; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Fluorescence radiometry; Iron; Manganese dioxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Radium; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 29
    Publication Date: 2023-07-10
    Keywords: Batrachium; Betula; Betula nana; Betula pendula; Betula pubescens; Beug_pollen-archive; Calliergon giganteum; Calliergon sarmentosum; Calliergon stramineum; Carex rostrata; Carex sect. Eucarex; Carex sect. Vignea; Cicuta virosa; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Drepanocladus exannulatus; Drepanocladus fluitans; Eleocharis palustris; Fiberg57makro; Fichtelgebirge, Northern Germany; Helodium blandowii; Hippuris vulgaris; Juniperus; Meesea triquetra; Menyanthes trifoliata; Montia rivularis; Myriophyllum alterniflorum; Nitella; Paludella squarrosa; Pinus sp.; Pinus sylvestris; Polytrichum commune; Polytricum strictum; Potamogeton obtusifolius; Potamogeton pusillus; Potamogeton rutilus; Potentilla palustris; PROFILE; Profile sampling; Rhynchospora; Salix; Sampling on land; Sphagnum sect. Cuspidata; Sphagnum teres; Stellaria palustris
    Type: Dataset
    Format: text/tab-separated-values, 675 data points
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  • 30
    Publication Date: 2023-11-01
    Keywords: Abies; Alnus; Apiaceae; Artemisia; Athyrium filix-femina; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Bupleurum; Calluna; Campanulaceae; Carpinus; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Circaea; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Fabaceae; Fagus; Fichtelgebirge, Northern Germany; Filicinae; Filipendula; Fraxinus; Gentianaceae; Geranium; Hedera; Helianthemum alpestre; Hippophae; Juniperus; Knautia; Lamiaceae; Lycopodium annotinum; Lysimachia; Melampyrum; Onobrychis; Onosma; Picea; Pinus; Plantago lanceolata; Plantago major/media-type; Poaceae; Polygonum bistorta-type; Polypodium vulgare; Populus; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; Ranunculus; Ranunculus subgen. Batrachium; Rhamnus frangula; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Saxifraga oppositifolia-type; Scrophulariaceae; SEELOH92; Seelohe; Sparganium-type; Sphagnum; Succisa; Thalictrum; Tilia cordata-type; Typha latifolia; Ulmus; Vaccinium-type; Valeriana dioica; Valeriana sambucifolia; Viburnum
    Type: Dataset
    Format: text/tab-separated-values, 1748 data points
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  • 31
    Publication Date: 2023-11-01
    Keywords: Alnus; Apiaceae; Artemisia; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Calluna; Campanulaceae; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Fabaceae; Filicinae; Filipendula; Fraxinus; Gentianaceae; Gypsophila; Hedera; Helianthemum; Hippophae; Juniperus; Kleines Rotes Moor/Rhön; Knautia; Lycopodium alpinum-type; Lysimachia; Melampyrum; Menyanthes; Montia; Onobrychis; Picea; Pinus; Plantago major/media-type; Poaceae; Polemonium; Polygonum bistorta-type; Polypodium vulgare; Populus; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; Ranunculus; Ranunculus subgen. Batrachium; Rhamnus frangula; Rhinanthus; RotesMoor1; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Saxifraga oppositifolia-type; Scabiosa; Scrophulariaceae; Selaginella selaginoides; Sparganium-type; Sphagnum; Thalictrum; Tilia cordata-type; Trifolium; Ulmus; Vaccinium-type; Valeriana dioica; Valeriana sambucifolia
    Type: Dataset
    Format: text/tab-separated-values, 2130 data points
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  • 32
    Publication Date: 2023-11-01
    Keywords: Apiaceae; Armeria; Artemisia; Athyrium filix-femina; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Calluna; Campanulaceae; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Empetrum; Ephedra distachya-type; Epilobium; Equisetum; Filicinae; Filipendula; Geranium; Harz, Germany; Helianthemum; Hippophae; Indeterminata; Juniperus; Lamiaceae; Lycopodium alpinum-type; Melampyrum; Menyanthes; Montia; Onobrychis; Pinus; Poaceae; Polygonum bistorta-type; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; RadauerBorn56; Ranunculus; Ranunculus subgen. Batrachium; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Selaginella selaginoides; Sparganium-type; Sphagnum; Thalictrum; Ulmus; Vaccinium-type; Valeriana sambucifolia; Varia
    Type: Dataset
    Format: text/tab-separated-values, 550 data points
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  • 33
    Publication Date: 2023-11-01
    Keywords: Alnus; Apiaceae; Artemisia; Athyrium filix-femina; Betula; Beug_pollen-archive; Botrychium; Brassicaceae; Bupleurum; Calluna; Campanulaceae; Caryophyllaceae; Centaurea scabiosa-type; Chenopodiaceae; Circaea; Compositae Liguliflorae; Compositae Tubuliflorae; Corylus; Counting, palynology; Cuscuta; Cyperaceae; DEPTH, sediment/rock; Drosera rotundifolia; Dryopteris filix-mas; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Fabaceae; Fiberg57; Fichtelgebirge, Northern Germany; Filicinae; Filipendula; Fraxinus; Gentianaceae; Geranium; Hedera; Helianthemum alpestre; Helianthemum nummularium-type; Hippophae; Juniperus; Knautia; Lamiaceae; Lycopodium alpinum-type; Lycopodium inundatum; Lysimachia; Melampyrum; Menyanthes; Montia; Myriophyllum; Myriophyllum spicatum-type; Onobrychis; Picea; Pinus; Plantago lanceolata; Plantago major/media-type; Pleurospermum; Poaceae; Polemonium; Polygonum bistorta-type; Populus; Potamogeton eupotamogeton-type; Potentilla-type; PROFILE; Profile sampling; Quercus; Ranunculus; Ranunculus subgen. Batrachium; Rhamnus; Rubiaceae; Rumex acetosa-type; Salix; Sampling on land; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Saxifraga oppositifolia-type; Scrophulariaceae; Selaginella selaginoides; Sorbus-type; Sparganium-type; Sphagnum; Thalictrum; Thelypteris; Tilia cordata-type; Trifolium; Typha latifolia; Ulmus; Urtica; Vaccinium-type; Valeriana dioica; Valeriana sambucifolia
    Type: Dataset
    Format: text/tab-separated-values, 6028 data points
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  • 34
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    In:  Supplement to: Riley, J P; Sinhaseni, P (1958): Chemical composition of three manganese nodules from the Pacific Ocean. Journal of Marine Research, 17, 466-482, hdl:10013/epic.46183.d001
    Publication Date: 2023-08-28
    Description: Three manganese nodules from the Pacific Ocean have been analysed for 35 elements by using mainly spectrophotometric and spectrographic methods. Cu, Co, Ni, Zn, and Pb were found in amounts approaching 1 %, which far exceeds their average concentrations in igneous rocks. On the other hand, elements having readily hydrolysable ions, such as Ga, Sc, Zr, Y, La and Ti, are present only in amounts comparable with their concentrations in igneous rocks. Sb, Bit Be, and Cr were not detected. The hydrochloric acid-insoluble fraction of nodules is practically free of the heavy metals that are characteristic of the acid-soluble fraction; it consists principally of clay minerals, together with lesser amounts of quartz, apatite, biotite and sodium and potassium felspars.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 35
    Publication Date: 2023-08-28
    Keywords: 248; Aluminium oxide; Barium oxide; Boron oxide; Cadmium oxide; Calcium oxide; Carbon dioxide; CHA-248; CHA-252; CHA-276; Challenger1872; Chromium(III) oxide; Cobalt oxide; Copper(II) oxide; DEPTH, sediment/rock; Description; Event label; Gallium oxide; Germanium oxide; Grab; GRAB; H.M.S. Challenger (1872); Iron oxide, Fe2O3; Lanthanum oxide; Lead oxide; Magnesium oxide; Manganese oxide; Molybdenum trioxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Oxygen, gas; Phosphorus pentoxide; Potassium oxide; Sample code/label; Scandium oxide; Silver oxide; Sodium oxide; Spectrophotometric; Strontium oxide; Thallium(I) oxide; Tin dioxide; Titanium dioxide; TRAWL; Trawl net; Tungsten trioxide; Vanadium oxide; Water in rock; Yttrium oxide; Zinc oxide; Zirconium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 104 data points
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  • 36
    Publication Date: 2023-08-28
    Keywords: ALB-173; Albatross (1882-1921); Albatross1899-1900; ALBTR-173; Colorimetry; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Fluorescence radiometry; Iron; Manganese dioxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Radium; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 43 data points
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  • 37
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    In:  Supplement to: Pettersson, Hans (1955): Manganese nodules and oceanic radium. Deep Sea Research - Supplement to Volume 3: Papers in Marine Biology and Oceanography, Pergamon Press, London & New York, 335-345, https://archive.org/details/papersinmarinebi00lond
    Publication Date: 2023-08-28
    Description: Thanks to the courtesy of the British Museum of Natural History the author obtained from their Challenger collections two small nodules, and through a similar courtesy of the Mineralogical Department of the Riksmuseum in Stockholm one half of a much larger nodule, also from the Challenger Expedition. Results from his initial measurements of the radium contents of these samples convinced the author that the radium in the nodules is accumulated from the surrounding sediment. In the present paper the author conducted a much more thorough investigation on nodules obtained during the U.S. Albatross cruises of Dr. Agassiz. Detailed measurements of radium were conducted on individual layers and spots inside each nodule.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 38
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1958): Expedition VEMA 14. Lamont Geological Observatory, Columbia University, New York, unpublished, 24 pp, https://www.ngdc.noaa.gov/mgg/geology/data/vema/vm14/vm14_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 14 Expedition from November 1957 until August 1958 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 151 cores and dredges were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Indian Ocean; Latitude of event; LGO-BT-57 or VM14 SBT57 (SIO); Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; V14; V14-106; V14-114; V14-132; V14-133; V14-136; V14-144; V14-16BT; V14-2; V14-28; V14-28BT; V14-46; V14-51RD; V14-57RD; V14-65; V14-69C; V14-6RD; V14-78; V14-8; V14-84A; V14-85; V14-86; V14-9; V14-91; V14-93; V14-99; Vema; VM14 51-CP (SIO); VM14 9TW (SIO)
    Type: Dataset
    Format: text/tab-separated-values, 325 data points
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  • 39
    Publication Date: 2023-08-28
    Keywords: 248; Aluminium oxide; Barium; Calcium oxide; CHA-248; CHA-252; CHA-276; Challenger1872; Cobalt; Copper; DEPTH, sediment/rock; Description; Event label; Gallium; Grab; GRAB; H.M.S. Challenger (1872); Iron oxide, Fe2O3; Lead; Magnesium oxide; Manganese oxide; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwest Pacific Ocean; Phosphorus pentoxide; Potassium oxide; Sample code/label; Silicon dioxide; Sodium oxide; Spectrophotometric; Strontium; Tin; Titanium dioxide; TRAWL; Trawl net; Vanadium; Water in rock; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 59 data points
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  • 40
    Publication Date: 2023-08-28
    Keywords: Area/locality; Cobalt; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Erben Seamount, Pacific Ocen; Event label; Horizon; Identification; Iron; Manganese; MDPC02HO-MP-026A-3; MIDPAC; MPC-26A-3; NEL-667; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D7; Pacific Ocean; Wet chemistry; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 41
    Publication Date: 2023-08-28
    Keywords: Area/locality; Cobalt; Deposit type; DEPTH, sediment/rock; DICH-SS; Dredge; Dredge, rock; DRG; DRG_R; Event label; GOLDHW1; Horizon; Identification; Iron; Manganese; MDPC02HO-MP-037A; MIDPAC; MPC-37A; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D1; NTHL-D7; Pacific Ocean; Sylvania Seamount, Pacific Ocean; Wet chemistry; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 42
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Area/locality; Calcium oxide; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; DRG; Horizon; Identification; Insoluble residue; Iron; Loss on ignition; Magnesium oxide; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL-D1; Phosphorus pentoxide; Silicon dioxide; Sulfur, total; Titanium dioxide; Vanadium oxide; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
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  • 43
    Publication Date: 2023-08-28
    Keywords: Description; DICH-SS; Dredge, rock; DRG_R; Event label; File name; Horizon; MDPC02HO-MP-025F-2; MIDPAC; MPC-25F-2; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Page(s); Sylvania Seamount, Pacific Ocean; Uniform resource locator/link to image; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 44
    Publication Date: 2023-08-28
    Keywords: Aluminium; Calcium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Hakuho-Maru; HAM_1968-1976; Identification; Iron; JAPAN_B; Japan Sea; Lead; Manganese; Molybdenum; Nickel; Niino_9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Silicon; Wet chemistry; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 45
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Hakuho-Maru; HAM_1968-1976; Identification; JAPAN_B; Japan Sea; Niino_9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 46
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    PANGAEA
    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2023-09-25
    Keywords: Acapulco Trench, Pacific ocean; CHUB01BD; CHUB01BD-001G; CHUB01BD-002G; CHUB01BD-003G; CHUB01BD-009G; CHUB01BD-017G; CHUB01BD-019G; CHUB01BD-033G; CHUB01BD-034G; CHUB01BD-039G; CHUB02BD-010G; CHUB-1; CHUB-17; CHUB-19; CHUB-2; CHUB-3; CHUB-33; CHUB-34; CHUB-39; CHUB5; CHUB-9; CHUBASCO; CHUB-X; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Feature; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 116 data points
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  • 47
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    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2023-09-25
    Keywords: CAP-13HG; CAP-22HG; CAP-24HG; CAP-26HG; CAP-28HG; CAP-30BG; CAP-31BG; CAP-32HG; CAP-33BG; CAP-34BG; CAP-36HG; CAP-39BG-1; CAP-41BG-1; CAP-44HG; CAP-50BG-1; CAPB01BD-030BG; CAPB01BD-031BG; CAPB01BD-033BG; CAPB01BD-034BG; CAPB01BD-039BG-01; CAPB01BD-041BG-01; CAPB01BD-050BG-01; CAPH0AHO-013G; CAPH0BHO-022G; CAPH0BHO-024G; CAPH0BHO-026G; CAPH0BHO-028G; CAPH0CHO-036G; CAPH0CHO-044G; CAPRICORN-B; CAPRICORN-H; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Event label; Feature; GC; Gravity corer; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 48
    Publication Date: 2023-11-03
    Description: Die biologischen Arbeiten der Deutschen Antarktischen Expedition 1938/39 wurden in übereinstimmung mit dem Institut für Walforschung der damaligen Reichsanstalt für Fischerei in Hamburg durchgeführt. ... Hier sollen nur die Beobachtungen über die Wale, Robben und Vögel betrachtet werden. Verbunden damit ist ein Überblick über die hydrographischen Verhältnisse sowie die Zusammenstellung der Volumina der quantitativen Oberflächenplanktonproben.
    Keywords: Abundance estimate; Amphipoda; Appendicularia; Auricularia; BNET; Brutnetz; Chaetognatha; Chaetopoda; Comment of event; Copepoda; Counting; Counting, Stereo Microscope; Crustacea indeterminata; Ctenophora; DAE3_1; DAE3_10; DAE3_11; DAE3_12; DAE3_13a; DAE3_13b; DAE3_14; DAE3_15; DAE3_16; DAE3_17; DAE3_18; DAE3_19; DAE3_1938/39; DAE3_2; DAE3_20; DAE3_21; DAE3_22; DAE3_23; DAE3_24; DAE3_25; DAE3_26; DAE3_27; DAE3_28; DAE3_29; DAE3_3; DAE3_30; DAE3_31; DAE3_32; DAE3_33; DAE3_34; DAE3_35; DAE3_36; DAE3_37; DAE3_38; DAE3_39; DAE3_4; DAE3_40; DAE3_41; DAE3_42; DAE3_43; DAE3_44; DAE3_45; DAE3_46; DAE3_47; DAE3_48; DAE3_49; DAE3_5; DAE3_50; DAE3_51; DAE3_52; DAE3_53; DAE3_54; DAE3_55; DAE3_56; DAE3_57; DAE3_58; DAE3_59; DAE3_6; DAE3_60; DAE3_61; DAE3_62; DAE3_63; DAE3_64; DAE3_65; DAE3_66; DAE3_67; DAE3_68; DAE3_69; DAE3_7; DAE3_70; DAE3_71; DAE3_72; DAE3_73; DAE3_74; DAE3_75; DAE3_76; DAE3_77; DAE3_78; DAE3_79; DAE3_8; DAE3_80; DAE3_81; DAE3_82; DAE3_83; DAE3_84; DAE3_9; Date/Time of event; Decapoda larvae; Depth, bottom/max; Depth, top/min; DEPTH, water; Deutsche Antarktische Expedition 1938/39; Directory of research expeditions of Germany; Estimated; Event label; EXP_GER; Fish indeterminata; KN; Krill net; Large volume water sampler; Latitude of event; Longitude of event; LVS; Medusa; Method/Device of event; Mollusca; Ostracoda; PLA; Plankton net; Radiolarians indeterminata; Rubber boat, Zodiac; Schizopoda; Schwabenland; Sediment sample; SES; Siphonophora sp.; Smear slide analysis; Southern Ocean; Thaliacea; Trawling; ZODIAC
    Type: Dataset
    Format: text/tab-separated-values, 653 data points
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  • 49
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    In:  Supplement to: Menard, H William; Shipek, CJ (1958): Surface concentrations of manganese nodules. Nature, 182(4643), 1156-1158, https://doi.org/10.1038/1821156b0
    Publication Date: 2024-07-01
    Description: Manganese nodules were investigated during the Downwind Expedition, a part of the International Geophysical Year programme of the Scripps Institution of Oceanography of the University of California. Attempts were made to collect bottom photographs, cores and dredge hauls in the same areas, to measure the distribution at the surface and in depth, and to obtain large samples for physical and chemical analysis.
    Keywords: Comment; Coverage; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0BBD; DOWNWIND-B1; DOWNWIND-B2; DWBP10; DWBP11; DWBP2; DWBP5; DWBP8; DWBP9; East Pacific, Austral Basin; Elevation of event; Event label; French Polynesia; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Nodules, mass abundance; North-East Pacific Ocean; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Southwest Pacific Ocean; Spencer F. Baird; Station 10-K1253; Station 11-K1252; Station 2-K1243; Station 5-K1250; Station 8-K1248; Station 9-K1244; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 50
    Publication Date: 2024-07-01
    Description: The cores described in this report were taken on the DOWNWIND Expedition in October 1957 to February 1958 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird and the R/V Horizon. A total of 201 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DNWB0ABD; DNWB0ABD-002G; DNWB0ABD-003G; DNWB0ABD-007G; DNWB0ABD-015G; DNWB0ABD-016G; DNWB0ABD-017G; DNWB0ABD-018G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-030GA; DNWB0BBD-030GB; DNWB0BBD-031G; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-044G; DNWB0BBD-045G; DNWB0BBD-046G; DNWB0BBD-047G; DNWB0BBD-048G; DNWB0BBD-052G; DNWB0BBD-054G; DNWB0BBD-055G; DNWB0BBD-056G; DNWB0BBD-057GA; DNWB0BBD-057GB; DNWB0CBD; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-0014H; DNWH0AHO-004H; DNWH0AHO-007H; DNWH0AHO-008TB; DNWH0BHO-031G; DNWH0BHO-034G; DNWH0DHO-092H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B3; DOWNWIND-B4; DOWNWIND-H; Dredge; DRG; DWBD1; DWBD2; DWBD4; DWBD5; DWBD7; DWBD8; DWBG122A-C; DWBG147B; DWBG15; DWBG16; DWBG17; DWBG18; DWBG19; DWBG2; DWBG3; DWBG30A; DWBG30B; DWBG31; DWBG37; DWBG40; DWBG43; DWBG44; DWBG45; DWBG46; DWBG47; DWBG48; DWBG52; DWBG54; DWBG55; DWBG56; DWBG57A; DWBG57B; DWBG-58; DWBG-59; DWBG7; DWH48; DWHD15; DWHD16; DWHD25; DWHD42; DWHD47; DWHD55; DWHD72; DWHG31; DWHG34; DWHH14; DWHH27; DWHH32; DWHH4; DWHH7; DWHH92; DWHT8B; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; Horizon; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 669 data points
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  • 51
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    In:  Supplement to: Tatsumoto, M; Goldberg, Edward D (1959): Some aspects of the marine geochemistry of uranium. Geochimica et Cosmochimica Acta, 17(3-4), 201-208, https://doi.org/10.1016/0016-7037(59)90094-8
    Publication Date: 2024-07-01
    Description: The uranium concentrations in marine calcareous material of a biological origin varied between 0.0X and 0.X p.p.m. with the exception of corals which had concentrations of several p.p.m. The aragonitic oolites and aragonite precipitated from sea-water had values similar to those of the corals. A geochronology based on the growth of ionium (thorium-230) from uranium is applicable not only to corals, as previous investigators have pointed out, but also to oolites. Several examples of "oolite ages" are given. The uranium content of ferromanganese minerals from pelagic deposits is of the order of from 4 to 5 p.p.m.
    Keywords: Atlantic Ocean; DEPTH, sediment/rock; DNWB0BBD; DNWB0BBD-047G; DNWB0BBD-052G; DOWNWIND-B2; DOWNWIND-H; Dredge; DRG; DWBG47; DWBG52; DWHD55; Event label; GC; Gravity corer; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Spencer F. Baird; TH1; TH1-TR4; Theta; Uranium; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 52
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    PANGAEA
    In:  Supplement to: SCRIPPS Institution of Oceanography (1957): MUKLUK Expedition, July-August, 1957: Cores and Dredge Samples. SIO Reference Series, 57-53, 6 pp
    Publication Date: 2024-07-01
    Description: The cores and dredges described are taken during the MUKLUK expedition of the R/V Spencer Baird in July-August 1957 by the Scripps Institute of Oceanography. A total of 31 cores and dredges were recovered and are available at Scripps Institute of Oceanography for sampling and study.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Latitude of event; Longitude of event; MKLK02BD; MKLK03BD-029D; MKLK03BD-030D; MUKLUK-B; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Spencer F. Baird; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 21 data points
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  • 53
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    PANGAEA
    In:  EPIC3Veröffentlichungen des Geobotanischen Institutes Rübel in Zürich, Bremerhaven, PANGAEA, 34, pp. 150-158
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 54
    Publication Date: 2016-02-18
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 55
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 56
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2015-10-28
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 57
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2016-01-27
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 58
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2016-04-07
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 59
    Publication Date: 2022-04-11
    Description: Natural sites in urban spaces can have a key role in citizen well-being, providing fundamental ecosystem services to the population and assuring a multitude of benefits. Therefore, cities should guarantee a number of green areas and their conservation in time as an essential part of urban architecture. In this framework, cooperation between scientists, decision makers and citizens is critical to ensure the enhancement of green public spaces. Social and scientific communities are called to work in a tuned way to combine scientific knowledge and methods to local socio-economic contexts, driven by the values of geoethics. The Bullicante Lake case study, discussed in this work, represents an example of application of geoethical values, such as inclusiveness, sharing, sustainability and conservation of bio- and geodiversity. This urban lake in Rome appeared following illegal excavation works in 1992 and remained closed until 2016 favouring re-naturalization processes. Over time, this site was often threatened by pending actions for building. The aim of this study was to highlight how fruitful cooperation between science and citizens is able to transform a degraded urban area into a place of knowledge, recreation, enjoyment and eco-systemic preservation. Moreover, on the basis of this experience, the authors proposed a generalised approach/strategy to be developed and applied in other contexts. The active involvement of citizens and the cooperation among scientists, artists and institutions were able to redress opportunistic behaviours well by preventing site degradation and its improper use, favouring environmental safeguarding and making possible the site’s recognition as a natural monument. The results of these actions led to the improved quality of citizen life, showing an excellent example of virtuous cooperation between science and society.
    Description: Published
    Description: 4429
    Description: 1TM. Formazione
    Description: 2TM. Divulgazione Scientifica
    Description: JCR Journal
    Keywords: geoethics ; conservation ; education ; citizen participation ; ecosystems ; urban lake ; green areas ; Rome ; 05.09. Miscellaneous ; 05.03. Educational, History of Science, Public Issues
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 60
    Publication Date: 2022-04-04
    Description: The Adventure Plateau, located in the NW sector of the Sicilian Channel, experienced several episodes of exposure/erosion and subsequent drowning, with the most recent occurring after the Last Glacial Maximum (LGM). Unlike other parts of the Sicilian Channel, the Adventure Plateau is relatively tectonically stable and is therefore best suitable for reconstructing its coastal configuration before the post-LGM marine transgression. Here, we use high-resolution seismic data to identify and map the palaeo-coastline at the LGM on the basis of the internal architecture of the prograding wedges (i.e., the location of the subaqueous clinoform rollover point) and the erosional markers such as the subaerial unconformities and the wave ravinement surfaces. These data, which show an extreme variability in the palaeo-morphology of the coastal margins of the Adventure Plateau, have been complemented with vintage seismic profiles in order to entirely cover its perimeter. The mapped LGM coastline has then been compared to predictions from glacial isostatic adjustment (GIA) modeling, which considers the horizontal migration of the shorelines in response to sea level rise and to Earth’s rotational and deformational effects associated with deglaciation. The two shorelines (i.e., the coastline derived from the marine data interpretation and the one derived from the GIA model) are in good agreement at 21 kyears BP, although some discrepancies occur in the southern part of the plateau, where the seabed slope is extremely gentle, which makes the clinoform rollover points and the buried erosional unconformities difficult to detect. After 20 kyears BP, an acceleration in the rate of the sea level rise occurred. The results of this study indicate the importance of comparing experimental data with model predictions in order to refine and calibrate boundary parameters and to gain a better picture of the evolution of sea level rise over various time scales. View Full-Text
    Description: Published
    Description: 125
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 61
    Publication Date: 2022-03-31
    Description: The pressure-gradient current is among the weaker ionospheric current systems arising from plasma pressure variations. It is also called diamagnetic current because it produces a magnetic field which is oriented oppositely to the ambient magnetic field, causing its reduction. The magnetic reduction can be revealed in measurements made by low-Earth orbiting satellites flying close to ionospheric plasma regions where rapid changes in density occur. Using geomagnetic field, plasma density and electron temperature measurements recorded on board ESA Swarm A satellite from April 2014 to March 2018, we reconstruct the flow patterns of the pressure-gradient current at high-latitude ionosphere in both hemispheres, and investigate their dependence on magnetic local time, geomagnetic activity, season and solar forcing drivers. Although being small in amplitude these currents appear to be a ubiquitous phenomenon at ionospheric high latitudes characterized by well defined flow patterns, which can cause artifacts in the main field models. Our findings can be used to correct magnetic field measurements for diamagnetic current effect, to improve modern magnetic field models, as well as to understand the impact of ionospheric irregularities on ionospheric dynamics at small-scale sizes of a few tens of kilometers.
    Description: Published
    Description: 1428
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: JCR Journal
    Keywords: High-latitude ionosphere ; Pressure-gradient current ; Diamagnetic current ; Swarm constellation ; 01.02. Ionosphere ; 04.05. Geomagnetism
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 62
    Publication Date: 2022-03-07
    Description: The study concerns the analysis of 220Rn (thoron) recorded in the surface soil in two sites of the Campi Flegrei caldera (Naples, Southern Italy) characterized by phases of volcanic unrest in the seven-year period 1 July 2011–31 December 2017. Thoron comes only from the most surface layer, so the characteristics of its time series are strictly connected to the shallow phenomena, which can also act at a distance from the measuring point in these particular areas. Since we measured 220Rn in parallel with 222Rn (radon), we found that by using the same analysis applied to radon, we obtained interesting information. While knowing the limits of this radioisotope well, we highlight only the particular characteristics of the emissions of thoron in the surface soil. Here, we show that it also shows some clear features found in the radon signal, such as anomalies and signal trends. Consequently, we provide good evidence that, in spite of the very short life of 220Rn compared to 222Rn, both are related to the carrier effect of CO2, which has significantly increased in the last few years within the caldera. The hydrothermal alterations, induced by the increase in temperature and pressure of the caldera system, occur in the surface soils and significantly influence thoron’s power of exhalation from the surface layer. The effects on the surface thoron are reflected in both sites, but with less intensity, the same behavior of 222Rn following the increasing movements and fluctuations of the geophysical and geochemical parameters (CO2 flux, fumarolic tremor, background seismicity, soil deformation). An overall linear correlation was found between the 222−220Rn signals, indicating the effect of the CO2 vector. The overall results represent a significant step forward in the use and interpretation of the thoron signal.
    Description: Published
    Description: 5809
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: 220Rn ; volcanic unrest ; hydrothermal alteration ; CO2 ; anomaly and trend ; Campi Flegrei
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 63
    Publication Date: 2022-03-07
    Description: Here, we describe the dataset of seismic envelopes used to study the S-wave Q-coda attenuation quality factor Qc of the Gargano Promontory (Southern Italy). With this dataset, we investigated the crustal seismic attenuation by the Qc parameter. We collected this dataset starting from two different earthquake catalogues: the first regarding the period from April 2013 to July 2014; the second regarding the period from July 2015 to August 2018. Visual inspection of the envelopes was carried out on recordings filtered with a Butterworth two-poles filter with central frequency fc = 6 Hz. The obtained seismic envelopes of coda decay can be linearly fitted in a bilogarithmic diagram in order to obtain a series of single source-receiver measures of Qc for each seismogram component at different frequency fc. The analysis of the trend Qc(fc) gives important insights into the heterogeneity and the anelasticity of the sampled Earth medium.
    Description: Published
    Description: 98
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
    Keywords: Seismicity Seismic Envelopes ; Seismological data
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 64
    Publication Date: 2022-03-07
    Description: As a result of changes in approach from traditional to virtual banking system, security in data exchange has become more important; thus, it seems essentially necessary to present a pattern based on smart models in order to reduce fraud in this field. A new algorithm has been provided in this article to improve security and to specify the limits of giving special services to Internet banking users in order to pave appropriate ground for virtual banking. In addition to identifying behavioral models of customers, this algorithm compares the behaviors of any customer with this model and finally computes the rate of trust in customer’s behavior. The hybrid data-mining and knowledge based structure has been adapted in this algorithm according to fuzzy systems. In this research, qualitative data was gathered from interviews with banking experts, analyzed by Expert Choice to identify the most important variables of customer behavior analysis, and to analyze customer behavior and customer bank Internet transaction data for a period of one year by MATLAB and Clementine. The results of this survey indicate that the potential of the given structure to recognize the rate of trust in Internet bank user’s behavior might be at reasonable level for experts in this area.
    Description: Published
    Description: 916
    Description: 3IT. Calcolo scientifico
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 65
    Publication Date: 2022-03-07
    Description: The investigation of submerged speleothems for sea level studies has made significant contributions to the understanding of the global and regional sea level variations during the Middle and Late Quaternary. This has especially been the case for the Mediterranean Sea, where more than 300 submerged speleothems sampled in 32 caves have been analysed so far. Here, we present a comprehensive review of the results obtained from the study of submerged speleothems since 1978. The studied speleothems cover the last 1.4 Myr and are mainly focused on Marine Isotope Stages (MIS) 1, 2, 3, 5.1, 5.3, 5.5, 7.1, 7.2, 7.3, and 7.5. The results reveal that submerged speleothems represent extraordinary archives providing accurate information on former sea level changes. New results from a stalagmite collected at Palinuro (Campania, Italy) and characterized by marine overgrowth are also reported. The measured elevations of speleothems are affected by the local response to glacial and hydro-isostatic adjustment (GIA), and thus might significantly deviate from the global eustatic signal. A comparison of the ages and altitude values of the Mediterranean speleothems and flowstone from the Bahamas with local GIA provides a new scenario for MIS 5 and 7 sea level reconstructions
    Description: Published
    Description: 77
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Keywords: Mediterranean Sea; submerged speleothems; phreatic speleothems; sea level change; coastal caves; GIA ; sea level
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 66
    Publication Date: 2022-03-07
    Description: Areas of the Mediterranean Sea are dynamic habitats in which human activities have been conducted for centuries and which feature micro-tidal environments with about 0.40 m of range. For this reason, human settlements are still concentrated along a narrow coastline strip, where any change in the sea level and coastal dynamics may impact anthropic activities. We analyzed light detection and ranging (LiDAR) and Copernicus Earth observation data. The aim of this research is to provide estimates and detailed maps (in three coastal plain of Sardinia (Italy) and in the Pontina Plain (southern Latium, Italy) of: (i) the past marine transgression occurred during MIS 5.5 highstand 119 kyrss BP; (ii) the coastline regression occurred during the last glacial maximum MIS 2 (21.5 krs cal BP); and (iii) the potential marine submersion for 2100 and 2300. The objective of this multidisciplinary study is to provide maps of sea level rise future scenarios using the IPCC RCP 8.5 2019 projections and glacio-hydro-isostatic movements for the above selected coastal zones (considered tectonically stable), which are the locations of touristic resorts, railways and heritage sites. We estimated a potential loss of land for the above areas of between about 146 km2 (IPCC 2019-RCP8.5 scenario) and 637 km2 along a coastline length of about 268 km.
    Description: Published
    Description: 2597
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Keywords: central Mediterranean coastal plains; past (MIS 5.5) and future sea level at 2100 and 2300; Sardinia; Pontina Plain ; sea level
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 67
    Publication Date: 2022-03-14
    Description: The size and shape of snow grains directly impacts the reflection by a snowpack. In this article, different approaches to retrieve the optical-equivalent snow grain size (ropt) or, alternatively, the specific surface area (SSA) using satellite, airborne, and ground-based observations are compared and used to evaluate ICON-ART (ICOsahedral Nonhydrostatic—Aerosols and Reactive Trace gases) simulations. The retrieval methods are based on optical measurements and rely on the ropt-dependent absorption of solar radiation in snow. The measurement data were taken during a three-week campaign that was conducted in the North of Greenland in March/April 2018, such that the retrieval methods and radiation measurements are affected by enhanced uncertainties under these low-Sun conditions. An adjusted airborne retrieval method is applied which uses the albedo at 1700 nm wavelength and combines an atmospheric and snow radiative transfer model to account for the direct-to-global fraction of the solar radiation incident on the snow. From this approach, we achieved a significantly improved uncertainty (〈25%) and a reduced effect of atmospheric masking compared to the previous method. Ground-based in situ measurements indicated an increase of ropt of 15 μm within a five-day period after a snowfall event which is small compared to previous observations under similar temperature regimes. ICON-ART captured the observed change of ropt during snowfall events, but systematically overestimated the subsequent snow grain growth by about 100%. Adjusting the growth rate factor to 0.012 μm2 s�1 minimized the difference between model and observations. Satellite-based and airborne retrieval methods showed higher ropt over sea ice (〈300 μm) than over land surfaces (〈100 μm) which was reduced by data filtering of surface roughness features. Moderate- Resolution Imaging Spectroradiometer (MODIS) retrievals revealed a large spread within a series of subsequent individual overpasses, indicating their limitations in observing the snow grain size evolution in early spring conditions with low Sun.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 68
    Publication Date: 2022-03-09
    Description: The eruptions of Campi Flegrei (Southern Italy), one of the most studied and dangerous active volcanic areas of the world, are fed by mildly potassic alkaline magmas, from shoshonite to trachyte and phonotrachyte. Petrological investigations carried out in past decades on Campi Flegrei rocks provide crucial information for understanding differentiation processes in its magmatic system. However, the compositional features of rocks are a palimpsest of many processes acting over timescales of 100–104 years, including crystal entrapment from multiple reservoirs with different magmatic histories. In this work, olivine, clinopyroxene and feldspar crystals from volcanic rocks related to the entire period of Campi Flegrei’s volcanic activity are checked for equilibrium with combined and possibly more rigorous tests than those commonly used in previous works (e.g., Fe–Mg exchange between either olivine or clinopyroxene and melt), with the aim of obtaining more robust geothermobarometric estimations for the magmas these products represent. We applied several combinations of equilibrium tests and geothermometric and geobarometric methods to a suite of rocks and related minerals spanning the period from ~59 ka to 1538 A.D. and compared the obtained results with the inferred magma storage conditions estimated in previous works through different methods. This mineral-chemistry investigation suggests that two prevalent sets of T–P (temperature–pressure) conditions, here referred to as “magmatic environments”, characterized the magma storage over the entire period of Campi Flegrei activity investigated here. These magmatic environments are ascribable to either mafic or differentiated magmas, stationing in deep and shallow reservoirs, respectively, which interacted frequently, mostly during the last 12 ka of activity. In fact, open-system magmatic processes (mixing/mingling, crustal contamination, CO2 flushing) hypothesized to have occurred before several Campi Flegrei eruptions could have removed earlier-grown crystals from their equilibrium melts. Moreover, our new results indicate that, in the case of complex systems such as Campi Flegrei’s, in which different pre-eruptive processes can modify the equilibrium composition of the crystals, one single geothermobarometric method offers little chance to constrain the magma storage conditions. Conversely, combined methods yield more robust results in agreement with estimates obtained in previous independent studies based on both petrological and geophysical methods
    Description: Published
    Description: 308
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 69
    Publication Date: 2022-03-14
    Description: On Vulcano Island (Italy), many geochemical crises have occurred during the last 130 years of solfataric activity. The main crises occurred in 1978–1980, 1988–1991, 1996, 2004–2007, 2009–2010 and the ongoing 2021 anomalous degassing activity. These crises have been characterized by early signals of resuming degassing activity, measurable by the increase of volatiles and energy output emitted from the summit areas of the active cone, and particularly by increases of gas/water ratios in the fumarolic area at the summit. In any case, a direct rather than linear correspondence has been observed among the observed increase in the fluid output, seismic release and ground deformation, and is still a subject of study. We present here the results obtained by the long-term monitoring (over 13 years of observations) of three extensive parameters: the SO2 flux monitored in the volcanic plume, the soil CO2 flux and the local heat flux, monitored in the mild thermal anomaly located to the east of the high-temperature fumarole. The time variations of these parameters showed cyclicity in the volcanic degassing and a general increase in the trend in the last period. In particular, we focused on the changes in the mass and energy output registered in the period of June–December 2021, to offer in near-real-time the first evaluation of the level and duration of the actual exhalative crisis affecting Vulcano Island. In this last event, a clear change in degassing style was recorded for the volatiles emitted by the magma. For example, the flux of diffused CO2 from the soils reached the maximum never-before-recorded value of 34,000 g m−2 d −1 and the flux of SO2 of the plume emitted by the fumarolic field on the summit crater area reached values higher than 200 t d−1 . The interpretation of the behavior of this volcanic system, resulting from the detailed analyses of these continuous monitoring data, will complete the framework of observations and help in defining and possibly forecasting the next evolution of the actual exhaling crisis.
    Description: This research was funded by the INGV-DPCN (Italian National Institute of Geophysics and Volcanology—Italian National Department for Civil Protection) volcanic surveillance program of Vulcano island, ObFu 0304.010. Moreover, this investigation was partially funded by the TORS project in the framework of institutional INGV projects “Ricerca Libera” ObFu 9999.549; and Pianeta Dinamico Task V2, ObFu 1020.010.
    Description: Published
    Description: 1283
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: : SO2 flux; CO2 flux; heat flux; Vulcano Island; geochemical crisis; extensive parameters
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 70
    Publication Date: 2022-04-22
    Description: An accurate understanding of dissimilarities in geomagnetic variability between quiet and disturbed periods has the potential to vastly improve space weather diagnosis. In this work, we exploit some recently developed methods of dynamical system theory to provide new insights and conceptual ideas in space weather science. In particular, we study the co-variation and recurrence statistics of two geomagnetic indices, SYM-H and AL, that measure the intensity of the globally symmetric component of the equatorial electrojet and that of the westward auroral electrojet, respectively. We find that the number of active degrees of freedom, required to describe the phase space dynamics of both indices, depends on the geomagnetic activity level. When the magnetospheric substorm activity, as monitored by the AL index, increases, the active number of degrees of freedom increases at high latitudes above the dimension obtained through classical time delay embedding methods. Conversely, a reduced number of degrees of freedom is observed during geomagnetic storms at low latitude by analysing the SYM-H index. By investigating time-dependent relations between both indices we find that a significant amount of information is shared between high and low latitude current systems originating from coupling mechanisms within the magnetosphere–ionosphere system as the result of a complex interplay between processes and phenomena of internal origin activated by the triggering of external source processes. Our observations support the idea that the near-Earth electromagnetic environment is a complex system far from an equilibrium
    Description: Published
    Description: 226
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: JCR Journal
    Keywords: Space weather ; geomagnetic storms ; magnetospheric substorms ; geomagnetic indices ; 04.05. Geomagnetism
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 71
    Publication Date: 2022-04-21
    Description: The dynamics of magma is often studied through 2D numerical simulations because 3D simulations are usually complex and computationally expensive. However, magmatic systems and physical processes are 3D and approximating them in 2D requires an evaluation of the information which is lost under different conditions. This work presents a physical and numerical model for 3D magma convection dynamics. The model is applied to study the dynamics of magma convection and mixing between andesitic and dacitic magmas. The 3D simulation results are compared with corresponding 2D simulations. We also provide details on the numerical scheme and its parallel implementation in C++ for high-performance computing. The performance of the numerical code is evaluated through strong scaling exercises involving up to 〉 12,000 cores.
    Description: Published
    Description: 760773
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 72
    Publication Date: 2022-04-22
    Description: The recent Chinese Seismo-Electromagnetic Satellite (CSES-01) provides a good opportunity to investigate some features of plasma properties and its motion in the topside ionosphere. Using simultaneous measurements from the electric field detector and the magnetometers onboard CSES-01, we investigate some properties of the plasma ExB drift velocity for a case study during a crossing of the Southern auroral region in the topside ionosphere. In detail, we analyze the spectral and scaling features of the plasma drift velocity and provide evidence of the turbulent character of the ExB drift. Our results provide an evidence of the occurrence of 2D ExB intermittent convective turbulence for the plasma motion in the topside ionospheric F2 auroral region at scales from tens of meters to tens of kilometers. The intermittent character of the observed turbulence suggests that the macro-scale intermittent structure is isomorphic with a quasi-1D fractal structure, as happens, for example, in the case of a filamentary or thin-tube-like structure. Furthermore, in the analyzed range of scales we found that both magnetohydrodynamic and kinetic processes may affect the plasma dynamics at spatial scales below 2 km. The results are discussed and compared with previous results reported in the literature.
    Description: Published
    Description: 1936
    Description: 2A. Fisica dell'alta atmosfera
    Description: JCR Journal
    Keywords: Turbulence ; Auroral ionosphere ; ExB plasma motion ; 01.02. Ionosphere
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 73
    Publication Date: 2022-04-26
    Description: Constraining the magmatic 3He/4He signature of fluids degassed from a magmatic system is crucial for making inferences on its mantle source. This is especially important in arc volcanism, where variations in the composition of the wedge potentially induced by slab sediment fluids must be distinguished from the effects of magma differentiation, degassing, and crustal contamination. The study of fluid inclusions (FIs) trapped in minerals of volcanic rocks is becoming an increasingly used methodology in geochemical studies that integrates the classical study of volcanic and geothermal fluids. Here, we report on the first noble gas (He, Ne, Ar) concentrations and isotopic ratios of FI in olivine (Ol) and pyroxene (Px) crystals separated from eruptive products of the Telica and Baru volcanoes, belonging to the Nicaraguan and Panamanian arc-segments of Central America Volcanic arc (CAVA). FIs from Telica yield air corrected 3He/4He (Rc/Ra) of 7.2–7.4 Ra in Ol and 6.1–7.3 in Px, while those from Baru give 7.1–8.0 Ra in Ol and 4.2–5.8 Ra in Px. After a data quality check and a comparison with previous 3He/4He measurements carried out on the same volcanoes and along CAVA, we constrained a magmatic Rc/Ra signature of 7.5 Ra for Telica and of 8.0 Ra for Baru, both within the MORB range (8 1 Ra). These 3He/4He differences also reflect variations in the respective arc-segments, which cannot be explained by radiogenic 4He addition due to variable crust thickness, as the mantle beneath Nicaragua and Panama is at about 35 and 30 km, respectively. We instead highlight that the lowest 3He/4He signature observed in the Nicaraguan arc segment reflects a contamination of the underlying wedge by slab sediment fluids. Rc/Ra values up to 9.0 Ra are found at Pacaya volcano in Guatemala, where the crust is 45 km thick, while a 3He/4He signature of about 8.0 Ra was measured at Turrialba volcano in Costa Rica, which is similar to that of Baru, and reflects possible influence of slab melting, triggered by a change in subduction conditions and the contemporary subduction of the Galapagos hot-spot track below southern Costa Rica and western Panama.
    Description: Published
    Description: 2076-3417
    Description: 1V. Storia eruttiva
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: JCR Journal
    Keywords: Telica volcano ; Baru volcano ; 3He/4He ; fluid inclusions ; CAVA ; slab fluids ; Isotope Geochemistry ; Noble gases ; 04.08. Volcanology ; 04.01. Earth Interior
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 74
    Publication Date: 2022-04-28
    Description: Geogenic and anthropogenic sources of atmospheric particulate and CO2 can lead to threats to human health in volcanic areas. Although the volcanic CO2 hazard is a topic frequently debated in the related scientific literature, space and time distribution of PM2.5 are poorly known. The results of combined CO2/PM2.5 surveys, carried out at Salina, Stromboli, and Vulcano islands (Aeolian archipelago, Italy) in the years 2020-2021, and integrated with investigations on bioaccumulation of metallic particulate matter by the mean of data on the magnetic properties of oleander leaves, are presented in this work. The retrieved results indicate that no significant anthropogenic sources for both CO2 and PM2.5 are active in these islands, at the net of a minor contribution due to vehicular traffic. Conversely, increments in volcanic activity, as the unrest experienced by Vulcano island since the second half of 2021, pose serious threats to human health, due to the near-ground accumulation of CO2, and the presence of suspended micro-droplets of condensed hydrothermal vapor, fostering the diffusion of atmophile viruses, such as the COVID-19. Gas hazard conditions can be generated, not only by volcanic vents or fumarolic fields, but also by unconventional sources, such as the outgassing from shallow hydrothermal aquifers through drilled or hand-carved wells.
    Description: Published
    Description: 4833
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Keywords: Aeolian Islands; gas hazard; magnetic properties; plant leaves; volcanic ash; volcanic unrest
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 75
    Publication Date: 2022-04-29
    Description: We identify the source of the Mw = 6.4 earthquake that rocked north-central Albania on November 26, 2019 02:54 UTC. We use synthetic aperture radar interferograms tied to the time series of coordinates of two permanent Global Navigation Satellite System (GNSS) stations (DUR2 and TIR2). We model the source by inverting the displacement data. Assuming in our model a half-space elastic medium and uniform slip along a rectangular fault surface, we invert the 104 picked measurements on a couple of ascending and descending interferograms to calculate the parameters of the fault. All inversions made with di erent input parameters converge towards a stable and robust solution with root mean square (r.m.s.) residual of 5.4 mm, thus ~1/5 of a fringe. They reveal that the earthquake occurred deep in the crust on a low-angle fault (23 ) dipping towards east with a centroid at 16.5 km depth. The best-fitting length and width of the fault are 22 and 13 km, and the reverse slip, 0.55 m. The seismic moment deduced from our model agrees with those of the published seismic moment tensors. This geometry is compatible with a blind thrust fault that may root on the main basal thrust, i.e., along the thrust front that separates Adria–Apulia from Eurasia. It is notable that there is a 123 ns yr-1 active shortening of the crust between the GNSS stations DUR2-TIR2 (equivalent to a shortening rate of 3.6 mm yr-1), and roughly in the east–west direction. Given this amount of strain the recurrence time of M6+ earthquakes along this fault should be of the order of 150 years.
    Description: Published
    Description: 210
    Description: 3T. Sorgente sismica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 76
    Publication Date: 2022-05-03
    Description: Rocky reefs provide complex structures in the otherwise largely sand-dominated coastal North Sea. Therefore, these reefs are highly important natural habitats for the functioning of coastal ecosystems, as they provide shelter, refuge and nursery grounds for various mobile and sessile species. In the North Sea, the spatial distribution of these habitats has been intensively investigated over recent years. However, these studies generally provide static accounts of the current state of these reef systems, but limited data exist on the temporal variations in sediment dynamics at and around natural rocky reefs. In this study, we provide observations from a multiannual time series of hydroacoustic seafloor surveys conducted at an isolated rocky reef in the North Sea. We use multibeam bathymetry and side-scan sonar backscatter data in combination with video observations, sediment sampling, and sub-bottom profiler data to assess the long-term variations of the rocky reef system. The reef is located in water depths between 11 and 17 m with an areal extent of ~0.5 km2 and is surrounded by mobile sands. The topography of the rocky reef appears to create a distinct hydrodynamic system that permits mobile sands to settle or move into bathymetrical deeper parts of the reef. Our results suggest a very dynamic system surrounding the reef with large scale scouring, sediment reworking and transport, while the shallower central part of the reef remains stable over time. We demonstrate the importance of hydrodynamics and current scouring around reefs for the local variability in seafloor properties over time. These small-scale dynamics are likewise reflected in the spatial distribution of sessile species, which are less abundant in proximity to mobile sands. The hydroacoustic mapping and monitoring of seafloor dynamics at higher spatial and temporal resolutions presents an important future direction in the study of valuable coastal habitats.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 77
    Publication Date: 2022-05-25
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Sadai, S., Condron, A., DeConto, R., & Pollard, D. Future climate response to Antarctic Ice Sheet melt caused by anthropogenic warming. Science Advances, 6(39), (2020): eaaz1169, doi:10.1126/sciadv.aaz1169.
    Description: Meltwater and ice discharge from a retreating Antarctic Ice Sheet could have important impacts on future global climate. Here, we report on multi-century (present–2250) climate simulations performed using a coupled numerical model integrated under future greenhouse-gas emission scenarios IPCC RCP4.5 and RCP8.5, with meltwater and ice discharge provided by a dynamic-thermodynamic ice sheet model. Accounting for Antarctic discharge raises subsurface ocean temperatures by 〉1°C at the ice margin relative to simulations ignoring discharge. In contrast, expanded sea ice and 2° to 10°C cooler surface air and surface ocean temperatures in the Southern Ocean delay the increase of projected global mean anthropogenic warming through 2250. In addition, the projected loss of Arctic winter sea ice and weakening of the Atlantic Meridional Overturning Circulation are delayed by several decades. Our results demonstrate a need to accurately account for meltwater input from ice sheets in order to make confident climate predictions.
    Description: This research was supported by the NSF Office of Polar Programs through NSF grant 1443347, the Biological and Environmental Research (BER) division of the U.S. Department of Energy through grant DE-SC0019263, the NSF through ICER 1664013, and by a grant to the NASA Sea Level Science Team 80NSSC17K0698.
    Repository Name: Woods Hole Open Access Server
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  • 78
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    American Association for the Advancement of Science
    Publication Date: 2022-05-25
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Foukal, N. P., Gelderloos, R., & Pickart, R. S. A continuous pathway for fresh water along the East Greenland shelf. Science Advances, 6(43), (2020): eabc4254, doi:10.1126/sciadv.abc4254.
    Description: Export from the Arctic and meltwater from the Greenland Ice Sheet together form a southward-flowing coastal current along the East Greenland shelf. This current transports enough fresh water to substantially alter the large-scale circulation of the North Atlantic, yet the coastal current’s origin and fate are poorly known due to our lack of knowledge concerning its north-south connectivity. Here, we demonstrate how the current negotiates the complex topography of Denmark Strait using in situ data and output from an ocean circulation model. We determine that the coastal current north of the strait supplies half of the transport to the coastal current south of the strait, while the other half is sourced from offshore via the shelfbreak jet, with little input from the Greenland Ice Sheet. These results indicate that there is a continuous pathway for Arctic-sourced fresh water along the entire East Greenland shelf from Fram Strait to Cape Farewell.
    Description: Funding for this work comes from the NSF under grant numbers OCE-1756361 and OCE-1558742 (N.P.F. and R.S.P.) and grant numbers OCE-1756863 and OAC-1835640 (R.G.).
    Repository Name: Woods Hole Open Access Server
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  • 79
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 80
    Publication Date: 2022-03-16
    Description: Based on the review of the available stratigraphic, tectonic, morphological, geodetic, and seismological data, along with new structural observations, we present a reappraisal of the potential seismogenic faults and fault systems in the inner northwest Apennines, Italy, which was the site, one century ago, of the devastating Mw ~6.5, 1920 Fivizzano earthquake. Our updated fault catalog provides the fault locations, as well as the description of their architecture, large-scale segmentation, cumulative displacements, evidence for recent to present activity, and long-term slip rates. Our work documents that a dense network of active faults, and thus potential earthquake fault sources, exists in the region. We discuss the seismogenic potential of these faults, and propose a general tectonic scenario that might account for their development.
    Description: Published
    Description: 139
    Description: 2T. Deformazione crostale attiva
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
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  • 81
    Publication Date: 2022-03-11
    Description: In this paper, we present two novel experimental setups specifically designed to perform in situ long-term monitoring of the aging behaviour of commercial plastic granules (HDPE, PP, PLA and PBAT). The results of the first six months of a three year monitoring campaign are presented. The two experimental setups consist of: (i) special cages positioned close to the sea floor at a depth of about 10 m, and (ii) a box containing sand exposed to atmospheric agents to simulate the surface of a beach. Starting from March 2020, plastic granules were put into the cages and plunged in sea water in two different locations in the sand boxes. Chemical spectroscopic and thermal analyses (GPC, SEM, FTIR-ATR, DSC, TGA) were performed on the granules before and after exposure to natural elements for six months, in order to identify the physical-chemical modifications occurring in marine environmental conditions (both in seawater and in sandy coastal conditions). Changes in colour, surface morphology, chemical composition, thermal properties and molecular weight, and the polydispersity of the materials, showed the different influences of the environmental conditions. Photooxidative reaction pathways were prevalent in the sandbox. Abrasive phenomena acted specially in the sea environment. PLA and PBAT did not show significant degradation after six months, making the possible reduction of marine pollution due to this process negligible
    Description: Published
    Description: 1111
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Keywords: multi-parametric platform ; bioplastics ; polymer degradation ; marine environment ; microplastics ; spectroscopy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 82
    Publication Date: 2022-03-18
    Description: Wetlands are hotspots of CH4 emissions to the atmosphere, mainly sustained by microbial decomposition of organic matter in anoxic sediments. Several knowledge gaps exist on how environmental drivers shape CH4 emissions from these ecosystems, posing challenges in upscaling efforts to estimate global emissions from waterbodies. In this work, CH4 and CO2 diffusive fluxes, along with chemical and isotopic composition of dissolved ionic and gaseous species, were determined from two wetlands of Tuscany (Italy): (i) Porta Lake, a small wetland largely invaded by Phragmites australis reeds experiencing reed die‐back syndrome, and (ii) Massaciuccoli Lake, a wide marsh area including open‐water basins and channels affected by seawater intrusion and eutrophication. Both wetlands were recognized as net sources of CH4 to the atmosphere. Our data show that the magnitude of CH4 diffusive emission was controlled by CH4 production and consumption rates, being mostly governed by (i) water temperature and availability of labile carbon substrates and (ii) water column depth, wind exposure and dissolved O2 contents, respectively. This evidence suggests that the highest CH4 diffusive fluxes were sustained by reed beds, providing a large availability of organic matter supporting acetoclastic methanogenesis, with relevant implications for global carbon budget and future climate models.
    Description: Published
    Description: 12156
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 83
    Publication Date: 2022-03-23
    Description: Mediterranean wetlands are severely affected by habitat degradation and related loss of biodiversity. In this scenario, the wide number of artificial farm ponds can play a significant role in the biodiversity conservation of aquatic flora. In the present contribution we show the preliminary results of a study on Mediterranean farm ponds of north-western Sicily (Italy), aimed to investigating the environmental factors linked to the occurrence of submerged macrophytes (vascular plants and charophytes). We studied the aquatic flora of 30 ponds and determined the chemical and isotopic composition of their water bodies on a subset of the most representative 10 sites. Results show that (1) farm ponds host few but interesting species, such as Potamogeton pusillus considered threatened at regional level; (2) Chara vulgaris, C. globularis and P. pusillus behave as disturbance-tolerant species, occurring both in nitrates-poor and nitrates-rich waters, whereas Stuckenia pectinata and Zannichellia palustris occur only in nitrates-poor waters. Although farm ponds are artificial and relatively poor habitats, these environments seem to be important for the aquatic flora and for the conservation of the local biodiversity, and can give useful information for the use of macrophytes as bioindicators in the Mediterranean area.
    Description: Published
    Description: 1292
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Keywords: Mediterranean flora; aquatic flora; bioindicators; carbon isotopes; conservation; hydrophytes; inland waters; water geochemistry
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 84
    Publication Date: 2022-03-23
    Description: The Campi Flegrei geothermal system sets in one of the most famous and hazardous volcanic caldera in the world. The geothermal dynamics is suspected to have a crucial role in the monitored unrest phases and in the eruption triggering as well. Numerical models in the literature do not properly consider the geochemical effects of fluid-rock interaction into the hydrothermal circulation and this gap limits the wholly understanding of the dynamics. This paper focuses on fluid-rock interaction effects at the Campi Flegrei and presents relevant information requested for reactive transport simulations. In particular, we provide: (1) an extensive review of available data and new petrographic analyses of the San Vito cores rearranged in a conceptual model useful to define representative geochemical and petrophysical parameters of rock formations suitable for numerical simulations and (2) the implemented thermodynamic and kinetic data set calibrated for the San Vito 1 well area, central in the geothermal reservoir. A preliminary 0D-geochemical model, performed with a different contribution of CO2 at high (165 ◦C) and low (85 ◦C) temperatures, firstly allows reproducing the hydrothermal reactions over time of the Campanian Ignimbrite formation, the most important deposits in the case study area.
    Description: Published
    Description: 810
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: 1TR. Georisorse
    Description: 4IT. Banche dati
    Description: JCR Journal
    Keywords: geothermal system ; hydrothermal alteration ; Campi Flegrei ; San Vito 1 well ; reactive model
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 85
    Publication Date: 2022-03-24
    Description: The ionospheric plasma density irregularities are known to play a role in the propagation of electromagnetic signals and to be one of the most important sources of disturbance for the Global Navigation Satellite System, being responsible for degradation and, sometimes, interruptions of the signals received by the system. In the equatorial ionospheric F region, these plasma density irregularities, known as plasma bubbles, find the suitable conditions for their development during post-sunset hours. In recent years, important features of plasma bubbles such as their dependence on latitude, longitude, and solar and geomagnetic activities have been inferred indirectly using their magnetic signatures. Here, we study the scaling properties of both the electron density and the magnetic field inside the plasma bubbles using measurements on board the Swarm A satellite from 1 April 2014 to 31 January 2016. We show that the spectral features of plasma irregularities cannot be directly inferred from their magnetic signatures. A relation more complex than the linear one is necessary to properly describe the role played by the evolution of plasma bubbles with local time and by the development of turbulent phenomena.
    Description: Published
    Description: 918
    Description: 2A. Fisica dell'alta atmosfera
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 86
    Publication Date: 2022-03-22
    Description: A systematic multiparametric and multiplatform approach to detect and study geo-space perturbations attributed to preparation processes related to natural hazards is fundamental in order to obtain useful insights on a series of complex dynamic phenomena of the Earth system, namely, earthquakes, volcanic and Saharan dust events, as well as geomagnetic disturbances. In particular, integrated analysis and interpretation of data from ground-based and spaceborne observations of the lower and upper atmospheres are of paramount importance for understanding the associated physical processes. In this Special Issue, we include pertinent studies on this field of research, presenting recent results and highlighting future directions for advances in the topic.
    Description: Published
    Description: 496
    Description: 7T. Variazioni delle caratteristiche crostali e "precursori"
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 87
    Publication Date: 2022-03-22
    Description: Low Earth orbit satellites collect and study information on changes in the ionosphere, which contributes to the identification of earthquake precursors. Swarm, the European Space Agency three-satellite mission, has been launched to monitor the Earth geomagnetic field, and has successfully shown that in some cases it is able to observe many several ionospheric perturbations that occurred as a result of large earthquake activity. This paper proposes the SafeNet deep learning framework for detecting pre-earthquake ionospheric perturbations. We trained the proposed model using 9017 recent (2014–2020) independent earthquakes of magnitude 4.8 or greater, as well as the corresponding 7-year plasma and magnetic field data from the Swarm A satellite, and excellent performance has been achieved. In addition, the influence of different model inputs and spatial window sizes, earthquake magnitudes, and daytime or nighttime was explored. The results showed that for electromagnetic pre-earthquake data collected within a circular region of the epicenter and with a Dobrovolsky-defined radius and input window size of 70 consecutive data points, nighttime data provided the highest performance in discriminating pre-earthquake perturbations, yielding an F1 score of 0.846 and a Matthews correlation coefficient of 0.717. Moreover, SafeNet performed well in identifying pre-seismic ionospheric anomalies with increasing earthquake magnitude and unbalanced datasets. Hypotheses on the physical causes of earthquake-induced ionospheric perturbations are also provided. Our results suggest that the performance of pre-earthquake ionospheric perturbation identification can be significantly improved by utilizing SafeNet, which is capable of detecting precursor effects within electromagnetic satellite data.
    Description: Published
    Description: 5033
    Description: 7T. Variazioni delle caratteristiche crostali e "precursori"
    Description: JCR Journal
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  • 88
    Publication Date: 2022-02-28
    Description: The polyphase structural evolution of a sector of the internal Central Apennines, where the significance of pelagic deposits atop neritic carbonate platform and active margin sediments has been long debated, is here documented. The results of a new geological survey in the Volsci Range, supported by new stratigraphic constraints from the syn-orogenic deposits, are integrated with the analysis of 2D seismic reflection lines and available wells in the adjacent Latin Valley. Late Cretaceous syn-sedimentary faults are documented and interpreted as steps linking a carbonate platform to the adjacent pelagic basin, located to the west. During Tortonian time, the pelagic deposits were squeezed off and juxtaposed as mélange units on top of the carbonate platform. Subsurface data highlighted stacked thrust sheets that were first involved into an initial in-sequence propagation with top-to-the-ENE, synchronous to late Tortonian foredeep to wedge-top sedimentation. We distinguish up to four groups of thrust faults that occurred during in-sequence shortening (thrusts 1–3; about 55–60 km) and backthrusting (thrust 4). During Pliocene to recent times, the area has been uplifted and subsequently extended by normal faults cross-cutting the accretionary wedge. Beside regional interest, our findings bear implications on the kinematic evolution of an orogenic wedge affected by far-traveled units.
    Description: Published
    Description: 160
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 89
    Publication Date: 2022-02-28
    Description: A crystal chemical investigation of a natural specimen of whitlockite, ideally Ca9Mg(PO4)6[PO3(OH)], from Palermo Mine (USA), was achieved by means of a combination of electron microprobe analysis (EMPA) in WDS mode, single‐crystal neutron diffraction probe (NDP) and single‐crystal X‐ray diffraction (XRD), and Fourier transform infrared (FTIR) spectroscopy. The crystal‐chemical characterization resulted in the empirical formula (Ca8.682Na0.274Sr0.045)Σ9.000(Ca0.034□0.996)Σ1.000(Mg0.533Fe2+0.342Mn2+0.062Al0.046)Σ0.983(P1.006O4)6[PO3(OH0.968F0.032)Σ1.000]. Crystal‐structure refinement, in the space group R3c, converged to R1 = 7.12% using 3273 unique reflections from NDP data and to R1 = 2.43% using 2687 unique reflections from XRD data. Unit cell parameters from NDP are a = 10.357(3) Å, c = 37.095(15) Å and V = 3446(2) Å3, and from XRD, the parameters are a = 10.3685(4) Å, c = 37.1444(13) Å and V = 3458.2(3) Å3. NDP results allowed a deeper definition of the hydrogen‐bond system and its relation with the structural unit [PO3(OH)]. The FTIR spectrum is very similar to that of synthetic tricalcium phosphate Ca3(PO4)2 and displays minor band shifts due to slightly different P‐O bond lengths and to the presence of additional elements in the structure. A comparison between whitlockite, isotypic phases from the largest merrillite group, and its synthetic counterpart Ca3(PO4)2 is provided, based on the XRD/NDP and FTIR results.
    Description: Published
    Description: 225
    Description: 1TR. Georisorse
    Description: JCR Journal
    Keywords: whitlockite ; calcium phosphates ; Mineralogy ; crystal chemistry ; spectroscopy
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  • 90
    Publication Date: 2022-02-28
    Description: Seismic prediction was considered impossible, however, there are no reasons in theoretical physics that explicitly prevent this possibility. Therefore, it is quite likely that prediction is made stubbornly complicated by practical difficulties such as the quality of catalogs and data analysis. Earthquakes are sometimes forewarned by precursors, and other times they come unexpectedly; moreover, since no unique mechanism for nucleation was proven to exist, it is unlikely that single classical precursors (e.g., increasing seismicity, geochemical anomalies, geoelectric potentials) may ever be effective in predicting impending earthquakes. For this reason, understanding the physics driving the evolution of fault systems is a crucial task to fine-tune seismic prediction methods and for the mitigation of seismic risk. In this work, an innovative idea is inspected to establish the proximity to the critical breaking point. It is based on the mechanical response of faults to tidal perturbations, which is observed to change during the “seismic cycle”. This technique allows to identify different seismic patterns marking the fingerprints of progressive crustal weakening. Destabilization seems to arise from two different possible mechanisms compatible with the so called preslip patch, cascade models and with seismic quiescence. The first is featured by a decreasing susceptibility to stress perturbation, anomalous geodetic deformation, and seismic activity, while on the other hand, the second shows seismic quiescence and increasing responsiveness. The novelty of this article consists in highlighting not only the variations in responsiveness of faults to stress while reaching the critical point, but also how seismic occurrence changes over time as a function of instability. Temporal swings of correlation between tides and nucleated seismic energy reveal a complex mechanism for modulation of energy dissipation driven by stress variations, above all in the upper brittle crust. Some case studies taken from recent Greek seismicity are investigated.
    Description: Published
    Description: 9596
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
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  • 91
    Publication Date: 2021-12-22
    Description: Volcanic emissions are a well-known hazard that can have serious impacts on local populations and aviation operations. Whereas several remote sensing observations detect high-intensity explosive eruptions, few studies focus on low intensity and long-lasting volcanic emissions. In this work, we have managed to fully characterize those events by analyzing the volcanic plume produced on the last day of the 2018 Christmas eruption at Mt. Etna, in Italy. We combined data from a visible calibrated camera, a multi-wavelength elastic/Raman Lidar system, from SEVIRI (EUMETSAT-MSG) and MODIS (NASA-Terra/Aqua) satellites and, for the first time, data from an automatic sun-photometer of the aerosol robotic network (AERONET). Results show that the volcanic plume height, ranging between 4.5 and 6 km at the source, decreased by about 0.5 km after 25 km. Moreover, the volcanic plume was detectable by the satellites up to a distance of about 400 km and contained very fine particles with a mean e ective radius of about 7 m. In some time intervals, volcanic ash mass concentration values were around the aviation safety thresholds of 2 10􀀀3 g m􀀀3. Of note, Lidar observations show two main stratifications of about 0.25 km, which were not observed at the volcanic source. The presence of the double stratification could have important implications on satellite retrievals, which usually consider only one plume layer. This work gives new details on the main features of volcanic plumes produced during low intensity and long-lasting volcanic plume emissions.
    Description: Published
    Description: 3866
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: JCR Journal
    Keywords: 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 92
    Publication Date: 2021-11-08
    Description: Over the last few years, several authors have presented contrasting models to describe the response of boulders to extreme waves, but the absence of direct observation of movements has hindered the evaluation of these models. The recent development of online video-sharing platforms in coastal settings has provided the opportunity to monitor the evolution of rocky coastlines during storm events. In September 2018, a surveillance camera of the Marine Protected Area of Plemmirio recorded the movement of several boulders along the coast of Maddalena Peninsula (Siracusa, Southeastern Sicily) during the landfall of the Mediterranean tropical-like cyclone (Medicane) Zorbas. Unmanned autonomous vehicle (UAV) photogrammetric and terrestrial laser scanner (TLS) surveys were performed to reconstruct immersive virtual scenarios to geometrically analyze the boulder displacements recorded in the video. Analyses highlighted that the displacements occurred when the boulders were submerged as a result of the impact of multiple small waves rather than due to a single large wave. Comparison between flow velocities obtained by videos and calculated through relationships showed a strong overestimation of the models, suggesting that values of flow density and lift coefficient used in literature are underestimated.
    Description: Published
    Description: 1497
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
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  • 93
    Publication Date: 2021-11-08
    Description: The dynamics of the sandy coast between Castellaneta and Taranto (Southern Italy) has been influenced by many natural and anthropogenic factors, resulting in significant changes in the coastal system over the last century. The interactions between vertical components of sea-level changes and horizontal components of the sedimentary budget, in combination with anthropogenic impact, have resulted in different erosion and accretion phases in the past years. Local isostatic, eustatic, and vertical tectonic movements, together with sedimentary budget changes, must be considered in order to predict the shoreline evolution and future marine submersion. In this study, all morpho-topographic data available for the Gulf of Taranto, in combination with Vertical Land Movements and sea-level rise trends, were considered by assessing the local evolution of the coastal trend as well as the future marine submersion. Based on the predicted spatial and temporal coastal changes, a new predictive model of submersion was developed to support coastal management in sea-level rise conditions over the next decades. After that, a multi-temporal mathematical model of coastal submersion was implemented in a Matlab environment. Finally, the effects of the relative sea-level rise on the coastal surface prone to submersion, according to the Intergovernmental Panel on Climate Change Assessment Reports (AR) 5 Representative Concentration Pathways (RCP) 2.6 and RCP 8.5 scenarios, were evaluated up to 2100.
    Description: Published
    Description: 1414
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
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  • 94
    Publication Date: 2021-11-25
    Description: This article describes research aimed at developing a system able to support local authorities and port communities in optimizing port navigation, avoiding or managing critical situations induced by sea-level variations in harbours and minimizing environmental damages and economic losses. In the Mediterranean basin, sea-level changes are mostly due to astronomical tides, related to the gravitational attraction between Earth, Moon and Sun. Nevertheless, sea-level variations are also influenced by meteorological tides, which are geodetic adjustments of sea surface due to atmospheric pressure variations above a water basin. So, starting from monitoring or forecasting environmental parameters in harbours, the system updates port bathymetric maps based on sea-level variations (acquired in the past, measured in real-time, or expected in the future) and detects hazardous areas for a certain ship moving inside a port at a given moment, by means of the implementation of “virtual traffic lights”. The system was tested on some real situations, including the analysis of maritime accidents (stranding of ships), providing satisfactory results by correctly signalling potentially dangerous areas variable over time. The architecture of the system and results achieved using it in the ports of Livorno and Bari, in Italy, are herewith described.
    Description: Published
    Description: 10265
    Description: 4A. Oceanografia e clima
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 95
    Publication Date: 2021-11-29
    Description: Sources of groundwater contaminants in inhabited areas, located in complex geo-tectonic contexts, are often deeply interlocked, thus, making the discrimination between anthropic and natural origins difficult. In this study, we investigate the Peloritani Mountain aquifers (Sicily, Italy), using the combination of probability plots with concentration contour maps to retrieve an overall view of the groundwater geo-chemistry with a special focus on the flux of heavy metals. In particular, we present a methodology for integrating spatial data with very different levels of precision, acquired before and during the “geomatic era”. Our results depict a complex geochemical layout driven by a geo-puzzle of rocks with very different lithological natures, hydraulically connected by a dense tectonic network that is also responsible for the mixing of deep hydrothermal fluids with the meteoric recharge. Moreover, a double source, geogenic or anthropogenic, was individuated for many chemicals delivered to groundwater bodies. The concentration contour maps, based on the different data groups identified by the probability plots, fit the coherency and congruency criteria with the distribution of both rock matrices and anthropogenic sources for chemicals, indicating the success of our geostatistical approach.
    Description: Published
    Description: 3269
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 96
    Publication Date: 2022-02-18
    Description: The purpose of the present paper is to investigate the effects of variable eruption source parameters on volcanic plume transport in the Mediterranean basin after the paroxysm of Mount Etna on 23 November 2013. This paroxysm was characterized by a north-east transport of ash and gas, caused by a low-pressure system in northern Italy. It is evaluated here in a joint approach considering the WRF-Chem model configured with eruption source parameters (ESPs) obtained elaborating the raw data from the VOLDORAD-2B (V2B) Doppler radar system. This allows the inclusion of the transient and fluctuating nature of the volcanic emissions to accurately model the atmospheric dispersion of ash and gas. Two model configurations were considered: the first with the climax values for the ESP and the second with the time-varying ESP according to the time profiles of the mass eruption rate recorded by the V2B radar. It is demonstrated that the second configuration produces a considerably better comparison with satellite retrievals from different sensors platforms (Ozone Mapping and Profiler Suite, Meteosat Second-Generation Spinning Enhanced Visible and Infrared Imager, and Visible Infrared Imaging Radiometer Suite). In the context of volcanic ash transport dispersion modeling, our results indicate the need for (i) the use of time-varying ESP, and (ii) a joint approach between an online coupled chemical transport model like WRF-Chem and direct near-source measurements, such as those carried out by the V2B Doppler radar system.
    Description: Published
    Description: 4037
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: 7A. Geofisica per il monitoraggio ambientale
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: 1IT. Reti di monitoraggio e sorveglianza
    Description: 3IT. Calcolo scientifico
    Description: 6IT. Osservatori non satellitari
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 97
    Publication Date: 2022-02-18
    Description: The Mediterranean Basin is characterized by a significant variability in tectonic behaviour, ranging from subsidence to uplifting. However, those coastal areas considered to be tectonically stable show coastal landforms at elevations consistent with eustatic and isostatic sea level change models. In particular, geomorphological indicators—such as tidal notches or shore platforms—are often used to define the tectonic stability of the Mediterranean coasts. We present the results of swim surveys in nine rocky coastal sectors in the central Mediterranean Sea using the Geoswim approach. The entire route was covered in 22 days for a total distance of 158.5 km. All surveyed sites are considered to have been tectonically stable since the last interglacial (Marine Isotope Stage 5.5 [MIS 5.5]), because related sea level markers fit well with sea level rise models. The analysis of visual observations and punctual measurements highlighted that, with respect to the total length of surveyed coast, the occurrence of tidal notches, shore platforms, and other indicators accounts for 85% of the modern coastline, and only 1% of the MIS 5.5 equivalent. Therefore, only 1% of the surveyed coast showed the presence of fossil markers of paleo sea levels above the datum. This significant difference is mainly attributable to erosion processes that did not allow the preservation of the geomorphic evidence of past sea level stands. In the end, our research method showed that the feasibility of applying such markers to define long-term tectonic behaviour is much higher in areas where pre-modern indicators have not been erased, such as at sites with hard bedrock previously covered by post-MIS 5.5 continental deposits, e.g., Sardinia, the Egadi Islands, Ansedonia, Gaeta, and Circeo. In general, the chances of finding such preserved indicators are very low.
    Description: Published
    Description: 2127
    Description: 4A. Oceanografia e clima
    Description: 7A. Geofisica per il monitoraggio ambientale
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 98
    Publication Date: 2022-02-18
    Description: We applied a new version of physics-based earthquake simulator upon a seismogenic model of the Italian seismicity derived from the latest version of the Database of Individual Seismogenic Sources (DISS). We elaborated appropriately for their use within the simulator all fault systems identified in the study area. We obtained synthetic catalogs spanning hundreds of thousands of years. The resulting synthetic seismic catalogs exhibit typical magnitude, space and time features that are comparable to those obtained by real observations. A typical aspect of the observed seismicity is the occurrence of earthquake sequences characterized by multiple main shocks of similar magnitude. Special attention was devoted to verifying whether the simulated catalogs include this notable aspect, by the use of an especially developed computer code. We found that the phenomenon of Coulomb stress transfer from causative to receiving source patches during an earthquake rupture has a critical role in the behavior of seismicity patterns in the simulated catalogs. We applied the simulator to the seismicity of the northern and central Apennines and compared the resulting synthetic catalog with the observed seismicity for the period 1650–2020. The result of this comparison supports the hypothesis that the occurrence of sequences containing multiple mainshocks is not just a casual circumstance.
    Description: Published
    Description: 2062
    Description: 2T. Deformazione crostale attiva
    Description: 3T. Fisica dei terremoti e Sorgente Sismica
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
    Keywords: numerical modeling ; earthquake simulator ; statistical methods ; earthquake clustering ; 04.06. Seismology ; 04.07. Tectonophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 99
    Publication Date: 2022-02-17
    Description: The interaction between fluids and tectonic structures such as fault systems is a muchdiscussed issue. Many scientific works are aimed at understanding what the role of fault systems in the displacement of deep fluids is, by investigating the interaction between the upper mantle, the lower crustal portion and the upraising of gasses carried by liquids. Many other scientific works try to explore the interaction between the recharge processes, i.e., precipitation, and the fault zones, aiming to recognize the function of the abovementioned structures and their capability to direct groundwater flow towards preferential drainage areas. Understanding the role of faults in the recharge processes of punctual and linear springs, meant as gaining streams, is a key point in hydrogeology, as it is known that faults can act either as flow barriers or as preferential flow paths. In this work an investigation of a fault system located in the Nera River catchment (Italy), based on geo-structural investigations, tracer tests, geochemical and isotopic recharge modelling, allows to identify the role of the normal fault system before and after the 2016–2017 central Italy seismic sequence (Mmax = 6.5). The outcome was achieved by an integrated approach consisting of a structural geology field work, combined with GIS-based analysis, and of a hydrogeological investigation based on artificial tracer tests and geochemical and isotopic analyses.
    Description: Published
    Description: 1499
    Description: 2IT. Laboratori analitici e sperimentali
    Description: JCR Journal
    Keywords: tracer tests; isotope hydrology; faults; carbonate aquifers; earthquakes; Mts. Sibillini; central Italy ; 03.02. Hydrology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 100
    Publication Date: 2022-02-23
    Description: In the Tethyan realm, leucocratic rocks were recognized as dikes and layers outcropping in the ophiolitic rocks of the Western Alps, in Corsica, and in the Northern Apennines. Several authors have suggested that the origin of leucocratic rocks is associated with partial melting of cumulate gabbro. Major and trace elements composition and paragenesis provided information about the leucocratic rocks genetic processes. This research aims at disclosing, for the first time, the petrographical and geochemical features of Timpa delle Murge leucocratic rocks, Pollino Massif (southern Italy), in order to discuss their origin and geodynamic significance through a comparison with other Tethyan leucocratic rocks. These rocks are characterized by high amounts of silica with moderate alumina and iron-magnesium contents showing higher potassium contents than plagiogranites, due to plagioclase alteration to sericite. Plagioclase fractionation reflects negative Eu anomalies indicating its derivation from gabbroic crystal mushes. The chondrite normalized REEs patterns suggest the participation of partial melts derived from a metasomatized mantle in a subduction environment. The results reveal some similarities in composition with other Tethyan leucocratic rocks, especially those concerning Corsica and the Northern Alps. These new data provide further clues on the origin of these leucocratic rocks and the Tethyan area geodynamic evolution.
    Description: Published
    Description: 1264
    Description: 2TR. Ricostruzione e modellazione della struttura crostale
    Description: JCR Journal
    Keywords: leucocratic rocks; geochemistry; fractional crystallization; ophiolite; geodynamic evolution; Pollino Massif; Southern Italy ; Petrography and Geochemistry of the Leucocratic Rocks in the Ophiolites from the Pollino Massif (Southern Italy)
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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