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  • 1
    Book
    Book
    Boulder, Colo. : The Geological Society of America
    Keywords: Geology North Pacific Ocean
    Type of Medium: Book
    Pages: XIII, 323 S. , Ill., graph. Darst., Kt
    ISBN: 0813711266
    Series Statement: Memoir / The Geological Society of America 126
    DDC: 551.4654
    Language: English
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  • 2
    Book
    Book
    Boulder, Colo. : The Geological Society of America
    Keywords: Quaternary ; Paleoclimatology ; Paleoceanography
    Type of Medium: Book
    Pages: X, 464 S , graph. Darst., Kt , 1 Kt.-Beil., 3 Mikrofiches
    ISBN: 0813711452
    Series Statement: Memoir / The Geological Society of America 145
    DDC: 551.6
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 246 (1973), S. 18-22 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] We demonstrate quantitatively that the world-wide Mid to Upper Cretaceous transgression and subsequent regression may have been caused by a contemporaneous pulse of rapid spreading at most of the mid-oceanic ridges between −110 to −85 m.y. The rapid spreading caused the ridges to expand ...
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2016-10-06
    Description: https://www.researchgate.net/publication/230891291_The_Orbital_Theory_of_Pleistocene_Climate_Support_frim_a_Revised_Chronology_of_the_Marine_d18O_Record
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
    Format: application/pdf
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  • 5
    Publication Date: 2022-05-26
    Description: Author Posting. © The Author(s), 2013. This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution. The definitive version was published in Nature Communications 5 (2014): 3107, doi:10.1038/ncomms4107.
    Description: Today's Sargasso Sea is nutrient-starved, except for episodic upwelling events caused by wind-driven winter mixing and eddies. Enhanced diatom opal burial in Sargasso Sea sediments indicates that silicic acid, a limiting nutrient today, may have been more available in subsurface waters during Heinrich Stadials, the millennial-scale climate perturbations of the last glacial and deglaciation. Here we use the geochemistry of opalforming organisms from different water depths to demonstrate changes in silicic acid supply and utilisation during the most recent Heinrich Stadial. We suggest that during the early phase (17.5-18 ka), wind-driven upwelling replenished silicic acid to the subsurface, resulting in low Si utilisation. By 17ka, stratification reduced the surface silicic acid supply and increased Si utilization efficiency. This abrupt shift in Si cycling would have contributed to high regional carbon export efficiency during the recent Heinrich Stadial, despite being a period of increasing atmospheric CO2.
    Description: KRH and LFR are funded by US National Science Foundation (USNSF) grant MGG 1029986; KRH is supported by the Climate Change Consortium of Wales (C3W), The Royal Society and a UK NERC New Investigator Grant; LFR is supported by an European Research Council Grant 278705; JFM is funded by US-NSF.
    Description: 2014-07-23
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 6
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    Unknown
    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: A listing of high southern latitude (〉30° S) pre-Pleistocene sediment cores is given for samples obtained by the coring and drilling programs of the Lamont-Doherty Geological Observatory, the Antarctic Program of the Florida State University, the French Museum national d'Histoire naturelle, and the Deep Sea Drilling Program. Information on geologic age, core length, lithology, bathymetry, and geographic location are given for each sediment sample. Ages of cores are given whenever possible to the nearest sub-epoch (middle Miocene, etc), together with (when known) the fossils used to determine the age, and the source of the age determination. Many core ages are from previously unpublished sources. The listing provides information on approximately 500 different cores. A computer-searchable version of the database may be obtained by writing to the senior author. A brief analysis of latitudinal and bathymetric patterns of sedimentation is also given for the Paleogene, Miocene, and Pliocene of the Southern Ocean. Throughout the Neogene, an essentially modern pattern of sedimentation is seen, with carbonate ooze predominating north of the present-day position of the polar front, siliceous ooze between the polar front and approximately 65° S, and clay near the Antarctic continent and in water depths 〉4 km. Paleogene and Cretaceous patterns of sedimentation appear to be different, but are difficult to distinguish due to plate motion and subsidence, and also because of the relatively small number of available pre-Neogene sediment cores.
    Description: Funding was provided by the National Science Foundation under grant Nos. OCE 79-19092 and DPP83-17087.
    Keywords: Marine sediments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 7
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    Unknown
    GSA
    In:  In: Investigation of Late Quaternary Paleoceanography and Paleoclimatology. , ed. by Cline, R. M. and Hays, J. D. Geological Society of America Memoir, 145 . GSA, Boulder, Colo., pp. 247-266.
    Publication Date: 2016-08-02
    Description: Intensification of the North and South Equatorial Current systems and trade winds occurred during glacial periods, according to a comparison of late Holocene (interglacial), 18,000 B.P. (glacial), and late Quaternary (0 to 180,000 B.P.) faunal assemblages and sea-surface temperature estimates from the equatorial Atlantic and Caribbean regions. Faster circulation of the North Equatorial Current system in glacial Northern Hemisphere winters (February) is indicated by increased upwelling of cool (15°C) water off northwest Africa and slightly cooler conditions across the northern tropical Atlantic and Caribbean. Intensification of the South Equatorial Current occurred along the Equator during the Southern Hemisphere winter (August). This interpretation is based on the dominance of a cool-equatorial assemblage, which indicated that waters of 16° to 18°C replaced the tropical assemblage that lives today in 24° to 26°C water in this region. The cool influence of the glacial (August) Benguela-South Equatorial Current decreased rapidly westward along the equatorial belt so that the fauna was dominated by the tropical assemblage in the Caribbean. Sea-surface temperatures increased rapidly from east to west in the equatorial belt, so that at long 35°W, the 16°C water had reached ambient temperatures of 24° to 26°C. Both faunal assemblages and temperature estimates of eight late Quaternary Atlantic and Caribbean sediment cores show that the equatorial region experienced three maximum incursions of cool Benguela Current water during the past 150,000 yr—at approximately 135,000 B.P., 73,000 B.P., and 18,000 B.P. Differences of glacial to interglacial sea-surface temperatures range from 5° to 10°C in the eastern equatorial Atlantic to 2° to 3°C in the western Atlantic and the Caribbean. During this time, only two periods with similar faunas and surface temperatures occurred—today and 125,000 B.P. Seasonal temperature contrast (August to February) is three to four times greater in all cores for glacial conditions than for interglacial conditions. The winter temperatures (February to the north of the thermal equator and August south of it) show the greatest changes, and they control the overall temperature pattern. Identical temperature patterns for cores affected by the North and the South Equatorial Currents suggest that the Northern and Southern Hemispheres are generally in phase and that more severe winters control the glacial temperature pattern.
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 8
    Publication Date: 2023-05-12
    Keywords: AGE; Age, comment; Age, error; DEPTH, sediment/rock; Normalized; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 438 data points
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  • 9
    Publication Date: 2023-06-27
    Keywords: 9-79A; Clay minerals; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Foraminifera; Glomar Challenger; Leg9; Lithology/composition/facies; Manganese; Mica; Nannofossils; North Pacific/VALLEY; Radiolarians; Sample code/label; Sand; Silt; Size fraction 〈 0.002 mm, clay; Smear slide analysis; Stratigraphy
    Type: Dataset
    Format: text/tab-separated-values, 78 data points
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  • 10
    Publication Date: 2023-06-27
    Keywords: 9-83A; Collophane; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Foraminifera; Glauconite; Glomar Challenger; Leg9; Lithology/composition/facies; Manganese; Nannofossils; North Pacific; Sample code/label; Sand; Silt; Size fraction 〈 0.002 mm, clay; Smear slide analysis; Stratigraphy; Volcanic glass
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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