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  • 1
    Electronic Resource
    Electronic Resource
    ALLAN V. COX(1926–1987) (1987)
    [s.l.] : Nature Publishing Group
    Nature 326 (1987), S. 134-134 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] ALLAN Cox, Professor of Geophysics at Stanford University in California and principal architect of the magnetic polarity reversal timescale, one of the pillars of plate tectonics, died in an accident on 27 January. Shortly before his death he had announced his intention to return to teaching and ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/326134a0
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    Paper (German National Licenses)
    Fulltext
  • 2
    Electronic Resource
    Electronic Resource
    The ocean floor closely observed: will it subvert marine geology? (1981)
    [s.l.] : Nature Publishing Group
    Nature 289 (1981), S. 9-10 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] IN a recent paper based on work with a deep-diving research submarine, fine-scale observations of the sea floor are ingeniously extrapolated to models of the events occuring at depth*. The paper is a good example of the geologist's method of using detailed observations on rock outcrops to yield ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/289009a0
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    Paper (German National Licenses)
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  • 3
    Electronic Resource
    Electronic Resource
    Greenstones from the Central Valley of the Mid-Atlantic Ridge (1966)
    [s.l.] : Nature Publishing Group
    Nature 209 (1966), S. 604-605 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The collection from the upper slope (Dredge 2, 2,6702,050 m) consists, as noted1, of fragments of greenstone, basalt, and partly metamorphosed basaltic tuff. The fragments exhibit a thin manganiferous coating, usually on all sides. This observation and the angularity of the fragments suggest that ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/209604b0
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    Paper (German National Licenses)
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  • 4
    Electronic Resource
    Electronic Resource
    Oceanography: States of past oceans (1983)
    [s.l.] : Nature Publishing Group
    Nature 305 (1983), S. 178-179 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] No more than a quarter-century ago we knew little about the deposits beneath the ocean floors, and less concerning the history of the two-thirds of the world which they occupy. Since then the new discipline of palaeoceanography has come into being, and has quickly illuminated a remarkable variety ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/305178a0
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    Paper (German National Licenses)
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  • 5
    Electronic Resource
    Electronic Resource
    Consider the incompleteness of the geological record (1981)
    [s.l.] : Nature Publishing Group
    Nature 294 (1981), S. 397-398 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] FOR more than a century geologists have felt comfortable with the notion that geological processes, although very slow, are also steady and so capable of moulding the Earth given enough time. The steady drip hollows the stone. The idea of steadiness came, at least in part, in reaction to the ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/294397a0
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    Paper (German National Licenses)
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  • 6
    Electronic Resource
    Electronic Resource
    Prehistoric shell assemblages from Franchthi Cave and evolution of the adjacent coastal zone (1980)
    [s.l.] : Nature Publishing Group
    Nature 288 (1980), S. 357-359 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] From -9,000 to 8,000 yr BP the inhabitants collected mainly Cyclope neritea2, a small (-15 mm) species which lives in the littoral zone near the mud surface and also flourishes in brackish water. It is gregarious and a carnivore. Although small it is easy to catch because it occurs in large numbers ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/288357a0
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    Paper (German National Licenses)
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  • 7
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    Unknown
    Depositional History of the South Atlantic Ocean during the Last 125 Million Years (1977)
    The University of Chicago Press
    In:  The Journal of Geology, 85 (6). pp. 651-698.
    Details
    Publication Date: 2018-02-07
    Description: This study is based on a reconstruction of the paleogeographic and paleobathymetric history of the South Atlantic and on a standardized set of sediment and biostratigraphic data from all Deep Sea Drilling Project sites. Standard data sets used are the lithologic description, biostratigraphic age, CaCO3 content, carbonate and carbonate-free sedimentation rates corrected for compaction, and hiatus distribution. For each site the subsidence history has been determined. Paleoceanographic variables used are the spatial and temporal lithofacies distribution, history of calcite compensation depth, surface fertility and lyocline, erosional events, and special lithologies (black shales). During its early history the South Atlantic consisted of a narrow rift divided by the Rio Grande Rise- Walvis Ridge barrier into a restricted northern and an open (to the southern ocean) southern basin. In the northern basin, evaporites are the earliest known marine sediments (Aptian) while more normal pelagic deposits formed in the southern basin. Free circulation of surface water between the southern ocean and the North Atlantic became possible late in the Mesozoic or in the early Cenozoic, and deep circulation (below 3 km depth) paths were open from north to south by the early Cenozoic. During the early and middle Mesozoic the South Atlantic had its own oceanographic character with dominantly terrigenous sedimentation and two anoxic black mudstone phases (Albian and Santonian) probably resulting from a strong oxygen minimum in mid-water caused by either excess surface fertility or old, slow moving bottom water. In the late Cretaceous the South Atlantic became part of the world ocean system and global events have overshadowed local ones since that time. After the early phase of rapid sedimentation of terrigenous material, the depositional history has been in- fluenced mainly by the increasing width and water depth of the basin and by fluctuations of the level and intensity of carbonate dissolution. At the Eocene/Oligocene boundary, the onset of a deep water circulation dominated by a cold circum-polar source of surface water is clearly marked by erosional events, a sharp drop of the calcite compensation depth and the arrival of biogenic siliceous oozes in the Argentine Basin.
    Type: Article , PeerReviewed
    Format: text
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 8
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    Unknown
    Radiolaria abundance of Hole 16-161A (2005)
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Keywords: 16-161A; Abundance estimate; Artophormis barbadensis; Artophormis gracilis; Calocycletta parva; Cannartus prismaticus; Centrobotrys gravida; Cycladophora hispida; Cycladophora turris; Cyclampterium milowi; Cyclampterium pegetrum; Deep Sea Drilling Project; DEPTH, sediment/rock; Dorcadospyris ateuchus; Dorcadospyris circulus; Dorcadospyris papilio; Dorcadospyris praeforcipata; Dorcadospyris pseudopapilio; Dorcadospyris quadripes; Dorcadospyris riedeli; Dorcadospyris spinosa; Dorcadospyris triceros; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Eusyringium fistuligerum; Eusyringium lagena; Glomar Challenger; Leg16; Lithapium mitra; Lithochytris vespertilio; Lithocyclia angusta; Lithocyclia aristotelis; Lithocyclia crux; Lithocyclia ocellus group; Lophocyrtis jacchia; North Pacific/CONT RISE; Podocyrtis ampla; Podocyrtis chalara; Podocyrtis goetheana; Podocyrtis mitra; Podocyrtis papalis; Podocyrtis sinuosa; Podocyrtis trachodes; Preservation; Sample code/label; Sethochytris babylonis; Sethochytris babylonis group; Sethochytris triconiscus; Stratigraphy; Theocampe mongolfieri; Theocorys anapographa; Theocotyle ficus; Theocyrtis annosa; Theocyrtis tuberosa; Thyrsocyrtis bromia; Thyrsocyrtis rhizodon; Thyrsocyrtis tetracantha; Thyrsocyrtis triacantha
    Type: Dataset
    Format: text/tab-separated-values, 812 data points
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    DATA PANGAEA
  • 9
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    Planktic foraminifera abundance of Hole 16-155 (2005)
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Keywords: 16-155; Abundance estimate; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Globigerina nepenthes; Globigerinoides bollii; Globigerinoides obliquus; Globoquadrina altispira; Globoquadrina dehiscens; Globoquadrina venezuelana; Globorotalia acostaensis; Globorotalia bononiensis; Globorotalia fohsi fohsi; Globorotalia fohsi lobata; Globorotalia fohsi robusta; Globorotalia gigantea; Globorotalia lenguaensis; Globorotalia mayeri; Globorotalia menardii; Globorotalia peripheroronda; Globorotalia praemenardii; Globorotalia scitula; Globorotalia siakensis; Globorotaloides hexagonus; Globorotaloides variabilis; Glomar Challenger; Leg16; North Pacific/RIDGE; Sample code/label; Sphaeroidinella seminulina; Sphaeroidinella subdehiscens; Stratigraphy
    Type: Dataset
    Format: text/tab-separated-values, 210 data points
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    DATA PANGAEA
  • 10
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    Unknown
    Planktic foraminifera abundance of Hole 16-158 (2005)
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Keywords: 16-158; Abundance estimate; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Globigerina calida; Globigerina fistulosa; Globigerina hystricosus; Globigerina nepenthes; Globigerinoides bollii; Globigerinoides conglobatus; Globigerinoides extremus; Globigerinoides gomitulus; Globigerinoides obliquus; Globigerinoides ruber; Globigerinoides subquadratus; Globoquadrina altispira; Globoquadrina dehiscens; Globoquadrina pseudofoliata; Globoquadrina venezuelana; Globoquadrina venezuelana conglomerata; Globorotalia acostaensis; Globorotalia crassaformis; Globorotalia crassula; Globorotalia fohsi robusta; Globorotalia gigantea; Globorotalia humerosa; Globorotalia intermedia; Globorotalia lenguaensis; Globorotalia limbata; Globorotalia margaritae; Globorotalia mayeri; Globorotalia menardii; Globorotalia multicamerata; Globorotalia multiloba; Globorotalia plesiotumida; Globorotalia praemenardii; Globorotalia pseudopima; Globorotalia scitula; Globorotalia siakensis; Globorotalia tumida; Globorotaloides hexagonus; Globorotaloides variabilis; Glomar Challenger; Leg16; Neogloboquadrina dutertrei; North Pacific/RIDGE; Pulleniatina obliquiloculata; Pulleniatina primalis; Pulleniatina sp.; Pulleniatina spectabilis; Sample code/label; Sphaeroidinella dehiscens; Sphaeroidinella kochi; Sphaeroidinella paenedehiscens; Sphaeroidinella seminulina; Sphaeroidinella subdehiscens; Sphaeroidinellopsis kochi; Sphaeroidinellopsis paenedehiscens; Stratigraphy
    Type: Dataset
    Format: text/tab-separated-values, 902 data points
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    DATA PANGAEA
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