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  1. Book ; Conference proceedings ; Online: Glacial sedimentation in ODP Leg 119 samples, supplementary data to: Barron, John A; Larsen, Birger; Baldauf, Jack G (1991): Evidence for late Eocene to early Oligocene Antarctic glaciation and observations on late Neogene glacial history of Antarctica: results from Leg 119. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 869-891

    Barron, John A / Baldauf, Jack G / Larsen, Birger

    1991  

    Abstract: Although scientific evidence prior to that from ODP Leg 119 indicates the presence of an ice sheet on East Antarctica by at least the earliest Oligocene, the question as to the size and stability of that initial ice sheet is still contested. Current ... ...

    Abstract Although scientific evidence prior to that from ODP Leg 119 indicates the presence of an ice sheet on East Antarctica by at least the earliest Oligocene, the question as to the size and stability of that initial ice sheet is still contested. Current hypotheses include (1) the presence of a small ice sheet in the earliest Oligocene with stepwise growth during the Neogene, (2) the presence of a continental-sized ice sheet in the late middle Eocene with no major evidence of subsequent deglaciation, and (3) the presence of glacial ice in the earliest Oligocene with a major ice sheet during the mid-Oligocene, followed by growth and decay of several ice sheets with characteristics similar to the temperate ice sheets of the Pleistocene of North America but with changes over a longer time scale (millions of years vs. 100,000 yr).
    Principal results from Leg 119 suggest the presence of significant late middle and late Eocene glaciation in East Antarctica and the presence of a continental-size ice sheet in East Antarctica during the earliest Oligocene. Although the Leg 119 results provide only glimpses of the Neogene glacial history of East Antarctica, they do provide evidence of fluctuations in the extent of the ice sheet and the waxing and waning of glaciers across the Prydz Bay shelf during the later part of the late Miocene and Pliocene.
    Language English
    Dates of publication 1991-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Conference proceedings ; Online
    Note This dataset is supplement to doi:10.2973/odp.proc.sr.119.194.1991
    DOI 10.1594/PANGAEA.758078
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  2. Book ; Conference proceedings ; Online: Diatom biostratigraphy of the Kerguelen Plateau and Prydz Bay, Southern Ocean, supplementary data to: Baldauf, Jack G; Barron, John A (1991): Diatom biostratigraphy: Kerguelen Plateau and Prydz Bay regions of the Southern Ocean. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 547-598

    Baldauf, Jack G / Barron, John A

    1991  

    Abstract: Samples were examined for diatoms from 22 holes at 11 sites cored by ODP Leg 119 on the Kerguelen Plateau and in Prydz Bay, East Antarctica. Diatoms were observed in Oligocene through Holocene sediments recovered from the Kerguelen Plateau. The diatom ... ...

    Abstract Samples were examined for diatoms from 22 holes at 11 sites cored by ODP Leg 119 on the Kerguelen Plateau and in Prydz Bay, East Antarctica. Diatoms were observed in Oligocene through Holocene sediments recovered from the Kerguelen Plateau. The diatom flora from the Kerguelen Plateau is characterized by species such as Azpeitia oligocenica, Rocella gelida, Rocella vigilans, and Synedra jouseana in the Oligocene and Crucidenticula nicobarica, Denticulopsis hustedtii, Nitzschia miocenica, and Thalassiosira miocenica in the Miocene. This somewhat cosmopolitan assemblage gives way to a Pliocene and Holocene assemblage characterized by species such as Nitzschia kerguelensis, Thalassiosira inura, and Thalassiosira torokina, which are endemic to the Southern Ocean region. Samples examined from Prydz Bay are generally devoid of diatoms. The exception is Site 739, where diatoms occur sporadically in lower Oligocene and upper Miocene through Quaternary sediments.
    The Leg 119 diatom biostratigraphic results allow the development of a stratigraphic framework for the Indian sector of the Southern Ocean. This diatom zonation integrates diatom zonations developed previously for other sectors of the Southern Ocean. The zonation proposed here is based on biostratigraphic events of both geographically widespread and endemic species calibrated to the paleomagnetic stratigraphy. As such, this zonation has application throughout the Southern Ocean and allows correlation from the southern high latitudes to the low latitudes.
    Language English
    Dates of publication 1991-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Conference proceedings ; Online
    Note This dataset is supplement to doi:10.2973/odp.proc.sr.119.135.1991
    DOI 10.1594/PANGAEA.728491
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  3. Book ; Conference proceedings ; Online: Oligocene diatom biostratigraphy for the Labrador Sea, supplementary data to: Baldauf, Jack G; Monjanel, Anne-Lise (1989): An Oligocene diatom biostratigraphy for the Labrador Sea: DSDP Site 112 and ODP Hole 647A. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 323-347

    Baldauf, Jack G / Monjanel, Anne-Lise

    1989  

    Abstract: The Oligocene diatom assemblage observed in samples from Hole 647A consists of a mixture of species characteristic of the low latitudes, the high southern latitudes, and the Norwegian-Greenland Sea. This diverse and well-preserved diatom assemblage ... ...

    Abstract The Oligocene diatom assemblage observed in samples from Hole 647A consists of a mixture of species characteristic of the low latitudes, the high southern latitudes, and the Norwegian-Greenland Sea. This diverse and well-preserved diatom assemblage allows a diatom stratigraphy to be established for the Labrador Sea and to be correlated with previously established diatom zonations. Changes in the composition of the diatom assemblage from warm-temperate to temperate species suggest a change in oceanographic conditions in the Labrador Sea during the early Oligocene.
    Language English
    Dates of publication 1989-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Conference proceedings ; Online
    Note This dataset is supplement to doi:10.2973/odp.proc.sr.105.129.1989
    DOI 10.1594/PANGAEA.745250
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  4. Book ; Conference proceedings ; Online: Miocene to Holocene diatom biostratigraphy of ODP Leg 105 sites, supplementary data to: Monjanel, Anne-Lise; Baldauf, Jack G (1989): Miocene to Holocene diatom biostratigraphy from Baffin Bay and Labrador Sea, Ocean Drilling Program Sites 645 and 646. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 305-322

    Monjanel, Anne-Lise / Baldauf, Jack G

    1989  

    Abstract: Diatoms occur sporadically in lower Miocene to Holocene sediments recovered at ODP Site 645 and in upper Pliocene to Holocene sediments at ODP Site 646. The diatom assemblage at Site 645 contains rare stratigraphic indicators. Fragmentation of frustules ... ...

    Abstract Diatoms occur sporadically in lower Miocene to Holocene sediments recovered at ODP Site 645 and in upper Pliocene to Holocene sediments at ODP Site 646. The diatom assemblage at Site 645 contains rare stratigraphic indicators. Fragmentation of frustules and the occurrence of species characteristic of high-latitude shelf, upper-slope environments suggest current transportation from the shelf. The diatom abundance and preservation at Site 646 probably reflect climatic changes and are also affected by dissolution, but it is not possible to detect the dominant factor. Therefore, the stratigraphic ranges of the primary and secondary biostratigraphic indicators are often unreliable.
    Language English
    Dates of publication 1989-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Conference proceedings ; Online
    Note This dataset is supplement to doi:10.2973/odp.proc.sr.105.127.1989
    DOI 10.1594/PANGAEA.745236
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  5. Book: Oligocene marine diatoms recovered in dredge samples from the Navarin Basin Province, Bering Sea

    Baldauf, Jack G / Barron, John A

    (U.S. Geological Survey bulletin ; 1765)

    1987  

    Author's details by Jack G. Baldauf and John A. Barron
    Series title U.S. Geological Survey bulletin ; 1765
    Keywords Diatoms, Fossil. ; Paleobotany
    Language English
    Size iii, 17 p., 14 leaves of plates :, ill. ;, 28 cm.
    Publisher U.S. G.P.O ; For sale by the Books and Open-File Reports Section, U.S. Geological Survey
    Publishing place Washington, D.C. ; Denver, CO
    Document type Book
    Note Includes index.
    Database NAL-Catalogue (AGRICOLA)

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  6. Book: Oligocene marine diatoms recovered in dredge samples from the Navarin Basin Province, Bering Sea

    Baldauf, Jack G / Barron, John A

    (US Geological Survey bulletin ; 1765)

    1987  

    Institution United States Geological Survey
    Author's details by Jack G. Baldauf and John A. Barron
    Series title US Geological Survey bulletin ; 1765
    Language English
    Size III, 17 S., 14 pl., Ill., Kt.
    Publisher U.S. Gov. Print. Off
    Publishing place Washington, D.C
    Document type Book
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  7. Book ; Conference proceedings ; Online: Stable and strontium isotope ratios and age determination of ODP Site 130-803, supplementary data to: Barrera, Enriqueta C; Baldauf, Jack G; Lohmann, Kyger C (1993): Strontium isotope and benthic foraminifer stable isotope results from Oligocene sediments at Site 803. In: Berger, WH; Kroenke, LW; Mayer, LA; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 130, 269-279

    Barrera, Enriqueta C / Baldauf, Jack G / Lohmann, Kyger C

    1993  

    Abstract: Stratigraphic information from strontium, oxygen, and carbon isotopic ratios has been integrated with diatom and planktonic foraminifer datums to refine the Oligocene to early Miocene chemostratigraphy of Site 803. The Sr isotope results are based on ... ...

    Abstract Stratigraphic information from strontium, oxygen, and carbon isotopic ratios has been integrated with diatom and planktonic foraminifer datums to refine the Oligocene to early Miocene chemostratigraphy of Site 803. The Sr isotope results are based on analyses of mixed species of planktonic foraminifer and bulk carbonate samples. 87Sr/86Sr ratios of bulk carbonate samples are, in most cases, less radiogenic than contemporaneous seawater. Estimated sediment ages based on planktonic foraminifer 87Sr/86Sr ratios, using the Sr-isotope-age relation determined by Hess and others in 1989, are in moderately good agreement with the biostratigraphic ages. Chronological resolution is significantly enhanced with the correlation of oxygen and carbon isotope records to those of the standard Oligocene section tied to the Geomagnetic Polarity Time Scale at Site 522. Ages revised by this method and other published ages of planktonic foraminifer datums are used to revise the Oligocene stratigraphy of Site 77 to correlate the stable isotope records of Sites 77 and 803.
    Comparison of the Cibicidoides stable isotope records of Sites 77 and 574 with paleodepths below 2500 m in the central equatorial Pacific, and Site 803 at about 2000-m paleodepth in the Ontong Java Plateau reveals inversions in the vertical d18O gradient at several times during the Oligocene and in the early Miocene. The shallower water site had significantly-higher d18O values than the deeper water sites after the earliest Oligocene 18O enrichment and before 34.5 Ma, in the late Oligocene from 27.5 to at least 25 Ma, and in the early Miocene from 22.5 to 20.5 Ma. It is not possible to ascertain if the d18O inversion persisted
    during the Oligocene/Miocene transition because the deeper sites have hiatuses spanning this interval. We interpret this pattern to reflect that waters at about 2000 m depth were cold and may have formed from mixing with colder waters originating in northern or southern high-latitude regions. The deeper water appear to have been warmer and may have been a mixture with warm saline waters from mid- or low-latitude regions. No apparent vertical d13C gradient is present during the Oligocene, suggesting that the age difference of these water masses was small.
    Language English
    Dates of publication 1993-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Conference proceedings ; Online
    Note This dataset is supplement to doi:10.2973/odp.proc.sr.130.022.1993
    DOI 10.1594/PANGAEA.779979
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  8. Book ; Conference proceedings ; Online: Age determination of Paleogene sediments from the Prysz Bay, supplementary data to: Thierstein, Hans R; MacDougall, J Douglas; Martin, Ellen E; Larsen, Birger; Barron, John A; Baldauf, Jack G (1991): Age determinations of Paleogene Diamictites from Prydz Bay (Site 739), Antarctica, using sr isotopes of mollusks and biostratigraphy of microfossils (diatoms and coccoliths). In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 739-745

    Thierstein, Hans R / Baldauf, Jack G / Barron, John A / Larsen, Birger / MacDougall, J Douglas / Martin, Ellen E

    1991  

    Abstract: Age dating of Paleogene diamictites from ODP Site 739 in Prydz Bay with marine microfossils (diatoms and calcareous nannofossils) suggests the build-up of a major East Antarctic ice shield in latest Eocene to earliest Oligocene time, about 35-38 m.y. ago. ...

    Abstract Age dating of Paleogene diamictites from ODP Site 739 in Prydz Bay with marine microfossils (diatoms and calcareous nannofossils) suggests the build-up of a major East Antarctic ice shield in latest Eocene to earliest Oligocene time, about 35-38 m.y. ago. Strontium isotopic analyses of small mollusk remains found within these diamictites, however, yield younger ages ranging from 29 to 23 Ma (i.e., latest early Oligocene to earliest Miocene). These age discrepancies could be caused by repeated glacial reworking of microfossils, macrofossils, and sediment clasts through the late Oligocene or, alternatively, by ion exchange in the still aragonitic mollusk shells.
    Language English
    Dates of publication 1991-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Conference proceedings ; Online
    Note This dataset is supplement to doi:10.2973/odp.proc.sr.119.178.1991
    DOI 10.1594/PANGAEA.758206
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  9. Book ; Conference proceedings ; Online: Biostratigraphy of ODP Leg 108 sites, supplementary data to: Weaver, Philip PE; Backman, Jan; Baldauf, Jack G; Bloemendal, Jan; Manivit, Helene; Miller, Kenneth G; Pokras, Edward M; Raymo, Maureen E; Tauxe, Lisa; Valet, Jean-Pierre; Chepstow-Lusty, Alex J; Olafsson, Gunnar (1989): Biostratigraphic synthesis, Leg 108, eastern equatorial Atlantic. In: Ruddiman, W; Sarnthein, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 108, 455-462

    Weaver, Philip PE / Backman, Jan / Baldauf, Jack G / Bloemendal, Jan / Manivit, Helene / Miller, Kenneth G / Pokras, Edward M / Raymo, Maureen E / Tauxe, Lisa / al., et

    1989  

    Abstract: Leg 108 cored 12 sites in the eastern equatorial Atlantic and along the northwest African continental margin to investigate the late Neogene and Quaternary oceanographic and climatic history of these regions. Sediments recovered during Leg 108 provide in ...

    Abstract Leg 108 cored 12 sites in the eastern equatorial Atlantic and along the northwest African continental margin to investigate the late Neogene and Quaternary oceanographic and climatic history of these regions. Sediments recovered during Leg 108 provide in part a high-resolution stratigraphic record for the upper Pliocene through Holocene interval. The bio- and magnetostratigraphy are intercalibrated where possible and provide a useful chronostratigraphy for paleoceanographic studies.
    Language English
    Dates of publication 1989-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Conference proceedings ; Online
    Note This dataset is supplement to doi:10.2973/odp.proc.sr.108.171.1989
    DOI 10.1594/PANGAEA.746642
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  10. Book ; Online: Age, biostratigraphic and paleomagnetic events at DSDP Leg 94, supplementary data to: Baldauf, Jack G; Thomas, Ellen; Clement, Bradford M; Takayama, Toshiaki; Weaver, Philip PE; Backman, Jan; Jenkins, G; Mudie, Peta J; Westberg-Smith, MJ (1987): Magnetostratigraphic and biostratigraphic synthesis, Deep Sea Drilling Project Leg 94. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 94, 1159-1205

    Baldauf, Jack G / Backman, Jan / Clement, Bradford M / Jenkins, G / Mudie, Peta J / Takayama, Toshiaki / Thomas, Ellen / Weaver, Philip PE / Westberg-Smith, MJ

    1987  

    Abstract: During DSDP Leg 94 sediment was recovered from 22 holes at six sites situated between 37° and 53°N in the North Atlantic. Paleomagnetic, calcareous nannofossil, foraminiferal, diatom, radiolarian, and dinocyst stratigraphic studies were completed. The ... ...

    Abstract During DSDP Leg 94 sediment was recovered from 22 holes at six sites situated between 37° and 53°N in the North Atlantic. Paleomagnetic, calcareous nannofossil, foraminiferal, diatom, radiolarian, and dinocyst stratigraphic studies were completed. The excellent magnetostratigraphic results, the near-complete recovery, and the abundant fossil content of the sediment allowed refinement of these stratigraphies, especially for the upper Pliocene-Holocene. Because the Leg 94 sites span middle and high North Atlantic latitudes, it is possible to use them to evaluate the synchrony of late Pliocene to Holocene datums.
    Language English
    Dates of publication 1987-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Online
    Note This dataset is supplement to doi:10.2973/dsdp.proc.94.146.1987
    DOI 10.1594/PANGAEA.788798
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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