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  • Other Sources  (31)
  • Springer  (28)
  • Birkhäuser
  • Geozon Science Media
  • 1985-1989  (31)
  • 1950-1954
  • 1989  (31)
  • 1
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    Birkhäuser
    In:  Basel, Birkhäuser, vol. 18, no. Publ. No. 12, pp. 267, (ISBN 3-534-14102-4)
    Publication Date: 1989
    Keywords: FractureT ; Proceedings of a conference
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  • 2
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    Springer
    In:  Bull., Polar Proj. OP-O3A4, Wavelets: Time-Frequency Methods and Phase, Berlin, Springer, vol. 22, no. 4, pp. 21-37, (ISBN 0080419208)
    Publication Date: 1989
    Keywords: Wavelet processing ; Textbook of geophysics ; Spectrum ; Data analysis / ~ processing ; noksp
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  • 3
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    Birkhäuser
    In:  Basel, 404 pp., Birkhäuser, vol. 10, no. Subvol. b, pp. 220, (ISBN: 0-08-037951-6)
    Publication Date: 1989
    Keywords: Induced seismicity ; GEBIRGSSCHLAG (see also rockburst and Erdstoss) ; Seismology
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  • 4
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    Springer
    In:  Berlin, Springer, vol. 7, no. 1, pp. 443-487, (ISBN 0-89871-560-1)
    Publication Date: 1989
    Keywords: Geodesy ; Muller
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  • 5
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    Springer
    In:  Professional Paper, The German Continental Deep Drilling Program (KTB), Site-Section Studies in the Oberpfalz and Schwarzwald, Berlin, Springer, vol. 120, no. 231, pp. 37-54, (ISBN: 3-540-23712-7)
    Publication Date: 1989
    Keywords: KTB ; Geol. aspects ; Tectonics
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  • 6
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    Springer
    In:  Bull., Open-File Rept., Lecture Notes in Earth Sciences, Berlin, Springer, vol. 89, no. 1, pp. Paper A 25 - A 34, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1989
    Keywords: Seismics (controlled source seismology) ; Textbook of geophysics ; Acoustics
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  • 7
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    Springer
    In:  Berlin, Springer, vol. 138, no. 2, pp. 527-553, (ISBN 0-7923-5034-0)
    Publication Date: 1989
    Keywords: Borehole geophys. ; Tectonics ; Textbook of geophysics ; Geol. aspects ; BO, ; RUB, ; GMG: ; MB ; 4129 ; 3.45.19
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  • 8
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    Springer
    In:  Berlin, Springer, vol. 20, no. 1, pp. 662-664, (ISBN 1-58488-320-0)
    Publication Date: 1989
    Keywords: Handbook of mathematics ; Finite Element Method ; Finite difference method ; DGL
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  • 9
    Publication Date: 1989
    Keywords: Proceedings of a conference ; Geodesy ; Plate tectonics ; Muller
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  • 10
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    Springer
    In:  Berlin, Springer, vol. 15, no. Publ. No. 12, pp. 585, (ISBN 1-85233-708-7)
    Publication Date: 1989
    Keywords: Textbook of informatics ; Textbook of mathematics ; Chaotic behaviour
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  • 11
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    Springer
    In:  Professional Paper, The German Continental Deep Drilling Program (KTB), Site-Selection Studies in the Oberpfalz and Schwarzwald, Berlin, Springer, vol. 9, no. 16, pp. 527-553, (ISBN 1-4020-1729-4)
    Publication Date: 1989
    Keywords: Borehole geophys. ; KTB ; Tectonics ; Review article ; Geol. aspects
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  • 12
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    Springer
    In:  Bull., Open-File Rept., The German Continental Deep Drilling Program (KTB), Site-Section Studies in the Oberpfalz and Schwarzwald, Berlin, Springer, vol. 65, no. 16, pp. 99-150, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1989
    Keywords: KTB ; Deep seismic sounding (espec. cont. crust) ; Tectonics ; Reflection seismics ; Duerbaum ; Durbaum ; Ruehl ; Ruhl ; Meissner
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  • 13
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    Springer
    In:  Polar Biology, 9 (3). pp. 137-145.
    Publication Date: 2020-06-10
    Description: The diets of five breeding seabird species were investigated on Adélie Land in January–February 1982. Stomach contents of Adélie penguins, Pygoscelis adeliae, were sampled by a water off-loading method and of Procellariiformes by spontaneous regurgitation. Diet compositions by mass were: Adélie penguin (79% euphausiid, 18% fish, 3% squid); Cape pigeon, Daption capense, (64% euphausiid, 29% fish, 7% carrion); Antarctic fulmar, Fulmarus glacialoides, (64% euphausiid, 20% carrion, 16% fish); snow petrel, Pagodroma nivea, (95% fish, 2% euphausiid, 1% carrion) and Wilson's stormpetrel, Oceanites oceanicus, (39% fish, 37% euphausiid, 13% carrion, 12% various crustaceans). The present Adélie penguin diet is consistent with those reported in other studies, given our knowledge of geographical variation in food availability. Differences in the diets of fulmarine petrels appear to relate to differences in foraging areas. The snow petrel is a fish-eating bird associated with pack-ice. Cape pigeon and Antarctic fulmar are mainly krill-eaters and we infer segregation along a neritic/oceanic gradient because of the importance of the neritic Euphausia crystallorophias in the former and the oceanic E. superba in the latter.
    Type: Article , PeerReviewed
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  • 14
    Publication Date: 2020-06-10
    Description: The foraging behaviour of fur seals and two species of surface feeding seabirds was observed over swarms of vertically migrating krill along the Antarctic Peninsula in July 1987. Fur Seal haul out patterns were correlated with krill in the upper 30 m of the water column. Krill moved to the surface at night; seals subsequently foraged from 1400-0700 hours before returning to floes. Foraging was continuous through the night. Dive duration decreased as krill moved up to the surface; shorter dives may have been more successful than longer ones. It is possible that very deep dives, which occur early in a foraging bout, represent more of an attempt to assess krill depth and distribution rather than being a genuine foraging effort. Seabirds responded to the presence of a surface krill swarm by circling over it and foraging; krill at depths greater than 30 m elicited directional flight and low frequencies of prey capture attempts. Both Snow Petrels and Antarctic Terns preyed on krill, but each species approached the swarms from different habitats. Snow Petrels primarily overflew areas covered by ice; terns preferred open water. This suggested that prey encounters are essentially opportunistic, although the search for prey is limited to rather specific marine habitats. This feature may be important to our understanding of the factors that determine the pelagic distribution of seabirds.
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  • 15
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    Springer
    In:  Contributions to Mineralogy and Petrology, 102 (1). pp. 93-101.
    Publication Date: 2018-03-02
    Description: Five major alteration zones in the Extrusive Series and the Sheeted Dike Complex of the Troodos Ophiolite are each characterized by (a) distinct elemental changes compared to the original composition and (b) secondary mineralogy. The upper ca. 300 m of the extrusive crust, the highly oxidatedcold seawater alteration zone (CSA), is strongly enriched in K2O and depleted in Na2O. It is followed downwards by alow temperature alteration zone (〈170° C) which is most widespread in the Troodos extrusives and where Na2O and K2O are enriched, the latter less strongly than in the CSA zone. Three types ofhigh temperature alteration zones (〈440° C; HTA I–III) are found in the Sheeted Dike Complex. All are marked by thorough leaching of K2O, while the behavior of Na2O (e.g. unchanged in type III) and CaO (depleted in type I, enriched in types II, III) is variable. Mass budgets of elemental changes are quantified by calibration of whole rock analyses via systematic stable element variations of fresh glasses found throughout the extrusive section. The Troodos extrusive crust and upper Sheeted Dike Complex are a major sink for MgO, K2O, and Na2O, and a source for CaO; the overall scale of fluxes drastically exceeds estimates based on fresh basalt compositions from present ocean crust.
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  • 16
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    Springer
    In:  Paläontologische Zeitschrift, 63 (3). pp. 207-214.
    Publication Date: 2016-02-23
    Description: Growth line analysis of diagenetically altered scleractinians is only possible if carbonate diagenesis has followed the pathway of aragonite leaching and coeval formation of low magnesium calcite. All other possibilities of aragonite transformation into calcite exclude the preservation of this growth line banding. Examples of these diagenetic patterns are found in the Pleistocene of Barbados.
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  • 17
    Publication Date: 2020-07-30
    Description: At ODP Site 661 from the continental margin of Northwest Africa, authigenic clinoptilolites were investigated in detail. Based on chemical data, crystal size and shape and their intergrowth with associated mineral phases, two types of clinoptilolite (type A and B) occur representing different diagenetic conditions under which the formation of zeolites took place. Clinoptilolite type A was found in a sediment section comprises numerous hiatuses and stratigraphically condensed sediments and could have been formed during early diagenesis. In contrast, clinoptilolite type B was precipitated in Campanian sediments during later diagenesis, after the transformation from opal-A to opal-CT had taken place. At Site 661, the silica source for the authigenesis of both clinoptilolite types is biogenic opal. Volcanic ash material occurs, but in low amounts and thus is not a prerequisite for the formation of clinoptilolite at Site 661.
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  • 18
    Publication Date: 2017-06-22
    Description: The Teahitia-Mehetia hot spot region located in the southeastern extension of the Society Islands chain, near 18° S–148° W consists of several active volcanoes. The distribution of recent volcanic activity correlates with seismic epicenters, and covers an area of more than 1000 km2. Intermittent volcanic activity has given rise to large (〉1000 m high) and small (〈500 m high) edifices composed of various types of flows. Several recent volcanic events have produced a suite of alkalic rocks ranging from ankaramites, through alkali basalts to trachy-phonolites. The presence of altered MORB-like tholeiites on one small seamount suggests that a different mantle source material was involved in forming some of the crust in this hot spot region.
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  • 19
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    Springer
    In:  AMBIO, 18 (1). pp. 55-59.
    Publication Date: 2020-09-18
    Description: In the Antarctic there are large unexploited stocks of cephalopods with high potential commercial value and there are two important fisheries for squid in the cool temperate waters of the Southern Ocean, adjacent to the Antarctic, in the Atlantic and Pacific sectors. Squid fisheries can develop very rapidly, and if this were to happen in the Antarctic before adequate management plans could be established, there would be serious consequences for the squid stocks, and also for the vertebrate predator populations which depend on them. It is especially important to increase our knowledge of the Antarctic cephalopod species, their distribution and role in the food chain, and to understand their life cycles
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  • 20
    Publication Date: 2018-03-21
    Description: Phytoplankton production, standing crop, and loss processes (respiration, sedimentation, grazing by zooplankton, and excretion) were measured on a daily basis during the growth, dormancy and decline of a winter-spring diatom bloom in a large-scale (13 m3) marine mesocosm in 1987. Carbonspecific rates of production and biomass change were highly correlated whereas production and loss rates were unrelated over the experimental period when the significant changes in algal biomass characteristic of phytoplankton blooms were occurring. The observed decline in diatom growth rates was caused by nutrient limitation. Daily phytoplankton production rates calculated from the phytoplankton continuity equation were in excellent agreement with rates independently determined using standard 14C techniques. A carbon budget for the winter bloom indicated that 82.4% of the net daytime primary production was accounted for by measured loss processes, 1.3% was present as standing crop at the end of the experiment, and 16.3% was unexplained. Losses via sedimentation (44.8%) and nighttime phytoplankton respiration (24.1%) predominated, while losses due to zooplankton grazing (10.7%) and nighttime phytoplankton excretion (2.8%) were of lesser importance. A model simulating daily phytoplankton biomass was developed to demonstrate the relative importance of the individual loss processes.
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  • 21
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    Springer
    In:  In: Plankton ecology: succession in plankton communities. , ed. by Sommer, U. Springer, Berlin, Germany, pp. 57-106. ISBN 3-540-51373-6
    Publication Date: 2012-03-22
    Type: Book chapter , NonPeerReviewed
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  • 22
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    Springer
    In:  , ed. by Sommer, U. Springer, Berlin, Germany, 369 pp. ISBN 3-540-51373-6
    Publication Date: 2012-02-28
    Type: Book , NonPeerReviewed
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  • 23
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    Springer
    In:  In: Volcanic hazards. , ed. by Latter, J. H. IAVCEI Proceedings in Volcanology, 1 . Springer , Berlin, pp. 210-229.
    Publication Date: 2014-02-10
    Type: Book chapter , NonPeerReviewed
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  • 24
    Publication Date: 2019-02-01
    Description: Manganese nodules from the Kane Gap (a deep sea channel connecting the Sierra Leone and Gambia Basins off West Africa) were investigated chemically and dated by10Be along cross-sections. Comparing the nodule structure with the stratigraphy of the related sediments, the following conclusions are drawn concerning the sedimentation processes during the last 4 to 6×106 years: The growth of the nodules started about 4 to 4.5 Ma before present during or near to the end of a period of erosion on a fossil-free, probably Miocene sediment. During the first phase of only a few hundred thousandyears, the nodules grew very quickly (7 to 〉18 mm/Ma). Fe-rich hydrogenetic material formed the internal sections of the nodules during this time. Slowing down of the bottom currents, resulting in deposition of thin sediment covers for short intervals, caused the character of the nodules to change to a more diagenetic composition. The growth rates were reduced to about 1 to 2 mm/Ma. The time of slowing is roughly 3 to 4 Ma BP. Probable uncertainties of the dating and growth rates resulting from supposed changes of the10Be supply to the nodules due to variations of the near bottom environment are discussed.
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  • 25
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    Springer
    In:  Contributions to Mineralogy and Petrology, 102 (1). pp. 112-126.
    Publication Date: 2019-05-13
    Description: A global compositional dichotomy for N-MORB magma (N1/N2) is recognized on the basis of Na2O, TiO2, CaO, and Al2O3 contents, and their respective ratios. We have characterized the two magma sub-types by means of their trace element patterns, and attempted to explain the differences in major and trace element contents in terms of a partial melting model, using data from DSDP/IPOD Leg 82. Mass balance calculations for N-MORB glass and rock compositions indicate that differences between N1-and N2-MORB are consistent with simple differences (5%–10%) in the degree of partial melting of a plagioclase-(±spinel) lherzolite, at pressures 〈10 kbar, rather than their respective derivation from plagioclase- and spinel-lher-zolite sources. Based on published and calculated partition coefficients, and calculated source magmaphile trace element compositions, the calculations indicate that the overall range of N-MORB compositions may be derived by between approximately 8% and 20% partial melting of a fertile lherzolite source. Fluid dynamic and melt kinematic considerations will probably necessitate refinement of the model, but should also take account of its qualitative precepts.
    Type: Article , PeerReviewed
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  • 26
    Publication Date: 2016-11-25
    Description: Indirect evidence suggests that Stenoteuthis oualaniensis is a multiple spawner, a reproductive strategy not reported previously for squid. After spawning once, S. oualaniensis apparently continues to feed, grow, and mature additional oocytes before spawning again. Squid were caught by jigging at night in waters around the main Hawaiian Islands during four cruises from 1981 to 1987. All females from 200 mm mantle length (ML) to at least 318 mm ML were sexually mature, indicating that considerable growth takes place after reaching sexual maturity. Size-frequency analyses of ovarian oocytes revealed continuous egg production throughout adult life. Mature ova are stored in the oviducts, but oviduct fullness is unrelated to body size, indicating repeat spawning.
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  • 27
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    Springer
    In:  Polar Biology, 9 (6). pp. 385-390.
    Publication Date: 2020-06-10
    Description: The diet of the emperor penguin Aptenodytes forsteri in the eastern Weddell Sea, Antarctica was studied during October and November 1986 by stomach content analysis. Emperor penguins fed mainly on Antarctic krill Euphausia superba, Antarctic silverfish Pleuragramma antarcticum and squid Psychroteuthis glacialis. Benthic prey was not found. The prey composition suggests two different feeding strategies, shallow dives exploring the rugged underside of sea ice where krill is taken, and deep dives when mesopelagic fish and squid are consumed. Chicks were fed on average every 1.44 days.
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  • 28
    Publication Date: 2020-11-06
    Description: The fur seal, Arctocephalus gazella, population at Mossman Peninsula (Laurie Island) was studied from 1985 to 1987. Weekly counts were carried out at a 4 km bachelor haul-out beach from December through June. Maxima of 2 240, 2 787 and 5 196 juvenile and adult males were counted during March of the respective years. Census data indicate an increase in the non-breeding population of 13.5% between 1985–1986 and 46.5% between 1986–1987.
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  • 29
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    Springer
    In:  Marine Biology, 103 (3). pp. 333-338.
    Publication Date: 2020-07-14
    Description: Respiration and nitrogen excretion rates of mature adult Loligo forbesi were investigated at the Roscoff Laboratory (North Brittany, France) during individual short-term incubation experiments in January 1986. The squids were in post-digestive condition and not actively swimming. Both oxygen uptake and nitrogen excretion are continuous processes. The metabolic rates of this active nektonic species (145 ml kg-1 h-1 oxygen uptake, 18.56 μg g-1 h-1 ammonia excretion) are distinctly higher than those of benthic cephalopods. Proteins constitute the main metabolic substrate for energetic needs. Besides ammonia, urea is also continuously released, in amounts ranging from 5 to 16% of ammonia-excretion values.
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  • 30
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    Springer
    In:  In: Plankton ecology - success in plankton communities. , ed. by Sommer, U. Springer, Berlin, Germany, pp. 1-8.
    Publication Date: 2019-08-07
    Type: Book chapter , NonPeerReviewed
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  • 31
    Publication Date: 2020-10-12
    Description: Die quartäre Sedimentfolge der Kärlicher Tongrube ist ein Schlüsselprofil für das Pleistozän Mitteleuropas: (a) Rhein- und Mosel-Terrassenablagerungen belegen die junge tektonische Hebung des paläozoischen Rheinischen Schildes, (b) Löß- und Paläobodenschichten spiegeln spätquartäre Klimaschwankungen wider, (c) Artefakt-Horizonte dokumentieren eine ausgedehnte frühmenschliche Geschichte des Mittelrheinraums, und (d) zahlreiche eingeschaltete Tephralagen — abgelagert während explosiver Vulkaneruptionen im Osteifel-Vulkanfeld — bilden ideale chronostratigraphische Leithorizonte. Die chemische und mineralogische Zusammensetzung zweier phonolithischer Bims-Fallablagerungen, die bisher als „Wehrer Bimse" bezeichnet wurden, unterscheidet sich drastisch von schlotnahen Tephraablagerungen am Wehr-Vulkan selber. Darüber hinaus zeigen (40)Ar/(39)Ar-Laseranalysen von Feldspat-Kristallen, daß die beiden Tephraablagerungen, mit Eruptionsaltern von 452.000 ± 8.000 Jahren vor Heute (KAE-DT2) und 〈 618.000 ± 13.000 Jahren v. h. (KAE-DTl), bis zu doppelt so alt sind, wie bislang angenommen. Schlotnahe, strombolianisch-phreatomagmatische, mafische Tephraschichten (KAE-BT4; lokale Bezeichnung: „Brockentuff"), die einem interglazialen Paläobodenhorizont im Hangenden der jüngeren Bimsablagerung eingeschaltet sind (lokale Bezeichnung: „Kärlicher Interglazial"), stammen von einem heute erodierten, kleinen Eruptionszentrum NW der Tongrube. (40)Ar/(39)Ar-Datierungen von Phlogopit-Ein-sprenglingen nach dem Stufenheizungs- und Laserverfahren ergeben für KAE-BT4 ein Eruptionsalter von 396.000 ± 20.000 Jahren v. h. Unsere Untersuchung zeigt, daß das Kärlicher Profil vor allem terrestrische Pleistozänablagerungen enthält, die zur Zeit der marinen Sauerstoffisotopenstadien 11 bis 19 abgelagert wurden. Jüngere Schichten sind nur unvollständig im Hangenden von KAE-BT4 erhalten. Das „Kärlicher Interglazial locus typicus" repräsentiert eine ca. 400.000 Jahre alte interglaziale Klimaphase und wird hier mit dem marinen Sauerstoffisotopenstadium 11 korreliert. Frühmenschliche Artefakte, die in Schichten unmittelbar im Hangenden der Tephra KAE-BT4 auftreten, könnten demnach ebenfalls bis zu ca. 400.000 Jahre alt sein.
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