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  • 1
    Call number: SR 90.0001(1884)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 20 S.
    Series Statement: U.S. Geological Survey bulletin 1884
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: SR 90.0001(2030)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 12 S.
    Series Statement: U.S. Geological Survey bulletin 2030
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
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    PANGAEA
    In:  Supplement to: Jones, Richard LI; Whatley, Robin C; Cronin, Thomas M; Dowsett, Harry J (1999): Reconstructing late Quaternary deep-water masses in the eastern Arctic Ocean using benthonic ostracoda. Marine Micropaleontology, 37(3-4), 251-272, https://doi.org/10.1016/S0377-8398(99)00022-5
    Publication Date: 2023-06-27
    Description: The distribution of Ostracoda in three long cores from the deep eastern Arctic Ocean was studied to determine the palaeoceanographical history of the Eurasian Basin during the late Quaternary. The samples for this study were obtained from the Lomonosov Ridge, Morris Jesup Rise and Yermak Plateau during the Arctic 91 expedition. Ostracoda previously studied in coretops at the same sites as the present study have shown that individual species have a strong association with different water masses and bathymetry. Throughout the late Quaternary, cores exhibit ostracod-rich layers separated by barren intervals. On the basis of biostratigraphical, isotopic and palaeomagnetic data the fossiliferous levels are interpreted as representing interglacial stages. The twenty most significant species were selected for subsequent quantitative investigation using Cluster and Factor analyses, in order to determine similarity and variance between the assemblages. An additional statistical method employing Modern Analogues and the Squared Chord Distance dissimilarity coefficient was utilised to compare the present late Quaternary fossil samples with a modern Arctic database. The results reveal a major faunal division within the Arctic Ocean Deep Water (AODW). Highly abundant and diverse assemblages within the cores were found to group and have good analogues with the Recent bathyal depth (1000-2500 m) upper AODW assemblages. Conversely, assemblages with low abundance and diversity correlate well with abyssal depth (〉3000 m) lower AODW assemblages. The palaeoceanographical history is complicated by the influence of adjacent water masses such as Canada Basin Deep Water (CBDW), Greenland Sea Deep Water (GSDW) and most importantly, Arctic Intermediate Water (AIW), which all had an influence on the ostracod assemblages during the late Quaternary. An enhanced flow of warm saline AIW into the Eurasian Basin results in species-rich upper AODW assemblages having good analogues down to 2750 m in the water column. In contrast, lower AODW assemblages influenced by cold well-oxygenated GSDW give analogues at depths as shallow as 1000 m. The faunal changes are the consequence of rapid climatic fluctuations in the eastern Arctic Ocean during the late Quaternary that are intrinsically linked to palaeoceanographical alternations in warm and cold current inflow from adjacent basins.
    Keywords: ARK-VIII/3; KAL; Kasten corer; Lomonosov Ridge, Arctic Ocean; Morris Jesup Rise; Polarstern; PS19/186; PS19/218; PS19/245; PS19 ARCTIC91; PS2185-6; PS2200-5; PS2212-3; Yermak Plateau
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
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    PANGAEA
    In:  Supplement to: Dowsett, Harry J (1988): Diachrony of Late Neogene microfossils in the southwest Pacific Ocean: application of the graphic correlation method. Paleoceanography, 3(2), 209-222, https://doi.org/10.1029/PA003i002p00209
    Publication Date: 2023-06-27
    Description: The assumption of synchrony of first and last occurrences of fossil taxa can be tested using graphic correlation procedures which, by allowing measured stratigraphic sections to be compared on a common depth scale, make it possible to develop a correlation model which integrates information from a number of cores. The strategy of the test presented here is to use a graphic correlation model that is based on data from the Atlantic (Deep Sea Drilling Project (DSDP) sites 502, 516A) and north Pacific (DSDP site 577A) as a basis for determining to what extent fossil datums in the southwest Pacific are synchronous. First and last occurrences of Pliocene calcareous nannofossils and planktonic foraminifers have been compared in five DSDP cores from the southwest Pacific ocean (sites 586, 587, 588, 590A, and 592). All cores were recovered using hydraulic piston coring technology, which assures the best recovery and minimal disturbance. Most of these cores contain abundant, well-preserved foraminifers and nannofossils, as well as a partial record of many of the expected magnetic polarity reversals in this part of the section. To assure taxonomic consistency, all taxonomic identifications were made by the author. Graphic correlation of this data set suggests that several important biostratigraphic markers are highly diachronous. For example, this study confirms that Globorotalia truncatulinoides first occurs at approximately 2.4 Ma between 20° and 35° south latitude in the southwest Pacific, approximately 0.5 m.y. earlier than it is found elsewhere in the Atlantic and Pacific. Other datums, such as the last occurrence of Discoaster brouweri, are essentially synchronous. These findings suggest that biostratigraphic models based on the assumption of synchrony of first and last occurrences of fossil taxa may be incorrect. Biostratigraphic models created with the Graphic Correlation method offer an opportunity to examine the biogeographic dimensions of origination, migration, and extinction of planktonic taxa.
    Keywords: 89-586; 90-587; 90-588; 90-590A; 90-592; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg89; Leg90; South Pacific; South Pacific/Coral Sea/BANK; South Pacific/Tasman Sea/CONT RISE
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Dowsett, Harry J; Loubere, Paul (1992): High resolution late Pliocene sea-surface temperature record from the Northeast Atlantic Ocean. Marine Micropaleontology, 20(2), 91-105, https://doi.org/10.1016/0377-8398(92)90001-Z
    Publication Date: 2023-06-27
    Description: Application of quantitative micropaleontologic methods of sea-surface temperature (SST) estimation to the planktic foraminiferal faunas at Hole 548 in the northeast Atlantic between 3.5 and 2.0 Ma provide a detailed record of Pliocene surface temperature changes during the onset of major Northern Hemisphere glaciation. SST estimates indicate a relatively warm interval of "enhanced interglacials (warm peaks)" between 3.2 and 2.8 Ma followed by steady cooling with a significant step-like change toward colder temperatures occurring about 2.4 Ma. This record compares well with faunal and SST records from other North Atlantic sites.
    Keywords: 80-548; AGE; Communality; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Factor 1; Factor 2; Factor 3; Factor 4; Factor 5; Glomar Challenger; Leg80; North Atlantic/SPUR; Sample code/label; Sea surface temperature, summer; Sea surface temperature, winter; Transfer function GSF18, Dowsett & Poore (1990)
    Type: Dataset
    Format: text/tab-separated-values, 1404 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Dowsett, Harry J; Poore, Richard Z (1990): A new planktic foraminifer transfer function for estimating Pliocene - Holocene Sea Surface temperatures. Marine Micropaleontology, 16(1-2), 1-23, https://doi.org/10.1016/0377-8398(90)90026-I
    Publication Date: 2023-06-27
    Description: A new planktic foraminifer transfer function (GSF18) related 5 North Atlantic assemblages to winter and summer sea surface temperature. GSF18, based on recombined and simplified core top census data, preserves most environmental information and reproduces modern North Atlantic conditions with approximately the same accuracy as previous transfer functions, but can be more readily applied to faunal samples ranging in age from Pliocene to Holocene. Transfer function GSF18 has been applied to faunal data from Deep Sea Drilling Project Hole 552A to produce a 2.5 m.y. sea-surface temperature (SST) time series. Estimates show several periods between 2.3 and 4.6 Ma during which mean SST's were both several degrees warmer and several degrees cooler than modern conditions. Between 2.9 and 4.0 Ma SST was generally warmer than modern except for a 250 k.y. interval centered at 3.3 Ma. Maximum SST, with respect to modern conditions, occurred after the cool interval near 3.1 Ma when SST was approximately 3.6° C warmer than present conditions. Comparison of SST estimates with stable isotope data suggest that after peak warming at 3.1 Ma, there was an overall surface water cooling with concomitant build up of global ice volume, culminating in Northern Hemisphere glaciation. This event is also indicated by the presence of ice rafted detritus in 552A sediments at about 2.45 Ma.
    Keywords: 81-552A; Counting 〉149 µm fraction; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, benthic; Foraminifera, planktic; Foraminifera, planktic, fragments; Foraminifera, planktic, other; Foraminifera, planktic reworked; Globigerina bulloides; Globigerina digitata; Globigerina eamesi; Globigerina falconensis; Globigerina incisa; Globigerina praedigitata; Globigerina pseudobesa; Globigerina sp.; Globigerina woodi; Globigerinella aequilateralis; Globigerinita glutinata; Globigerinoides obliquus; Globigerinoides ruber; Globigerinoides spp.; Globorotalia conomiozea; Globorotalia crassaformis; Globorotalia hirsuta; Globorotalia inflata; Globorotalia margaritae; Globorotalia menardii; Globorotalia scitula; Glomar Challenger; Ice rafted debris; Leg81; Neogloboquadrina acostaensis; Neogloboquadrina atlantica dextral; Neogloboquadrina atlantica sinistral; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; North Atlantic/PLATEAU; Orbulina universa; Sample code/label; Turborotalia quinqueloba
    Type: Dataset
    Format: text/tab-separated-values, 4587 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Poore, Richard Z; Dowsett, Harry J; Verardo, Stacey; Quinn, Terrence Michael (2003): Millennial- to century-scale variability in Gulf of Mexico Holocene climate records. Paleoceanography, 18(2), 1048, https://doi.org/10.1029/2002PA000868
    Publication Date: 2023-06-27
    Description: Proxy records from two piston cores in the Gulf of Mexico (GOM) provide a detailed (50-100 year resolution) record of climate variability over the last 14,000 years. Long-term (millennial-scale) trends and changes are related to the transition from glacial to interglacial conditions and movement of the average position of the Intertropical Convergence Zone (ITCZ) related to orbital forcing. The d18O of the surface-dwelling planktic foraminifer Globigerinoides ruber show negative excursions between 14 and 10.2 ka (radiocarbon years) that reflect influx of meltwater into the western GOM during melting of the Laurentide Ice Sheet. The relative abundance of the planktic foraminifer Globigerinoides sacculifer is related to transport of Caribbean water into the GOM. Maximum transport of Caribbean surface waters and moisture into the GOM associated with a northward migration of the average position of the ITCZ occurs between about 6.5 and 4.5 ka. In addition, abundance variations of G. sacculifer show century-scale variability throughout most of the Holocene. The GOM record is consistent with records from other areas, suggesting that century-scale variability is a pervasive feature of Holocene climate. The frequency of several cycles in the climate records is similar to cycles identified in proxy records of solar variability, indicating that at least some of the century-scale climate variability during the Holocene is due to external (solar) forcing.
    Keywords: Age, 14C AMS; Age, 14C milieu/reservoir corrected (-400 yr); Age, dated; Age, dated standard deviation; Calendar age; DEPTH, sediment/rock; Event label; Gulf of Mexico; GYRE97-6PC-20; PC; Piston corer; RC12; RC12-10; Robert Conrad
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 8
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: 89-586; Ageprofile Datum Description; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg89; South Pacific
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 9
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: 90-587; Ageprofile Datum Description; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg90; South Pacific/Coral Sea/BANK
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 10
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: 90-592; Ageprofile Datum Description; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg90; South Pacific/Tasman Sea/CONT RISE
    Type: Dataset
    Format: text/tab-separated-values, 27 data points
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