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  1. Article ; Online: A quaternary question. Response.

    Berggren, William A

    Science (New York, N.Y.)

    2008  Volume 320, Issue 5873, Page(s) 177–178

    Language English
    Publishing date 2008-04-11
    Publishing country United States
    Document type Comment ; Letter
    ZDB-ID 128410-1
    ISSN 1095-9203 ; 0036-8075
    ISSN (online) 1095-9203
    ISSN 0036-8075
    Database MEDical Literature Analysis and Retrieval System OnLINE

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    In stock of ZB MED Cologne/Königswinter

    Zs.A 27: Show issues Location:
    Je nach Verfügbarkeit (siehe Angabe bei Bestand)
    bis Jg. 1994: Bestellungen von Artikeln über das Online-Bestellformular
    Jg. 1995 - 2021: Lesesall (1.OG)
    ab Jg. 2022: Lesesaal (EG)
    Zs.MG 77: Show issues

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  2. Book ; Conference proceedings: Geochronology, time scales and global stratigraphic correlation

    Berggren, William A

    [Research Symposium in New Orleans (27 April 1993) entitled Geochronology, Time Scales and Stratigraphic Correlation]

    (Special publication / SEPM (Society for Sedimentary Geology) ; 54)

    1995  

    Institution Society for Sedimentary Geology
    Event/congress Research Symposium "Geochronology, Time Scales and Stratigraphic Correlation" (1993.04.27-28, NewOrleans)
    Author's details ed. by William A. Berggren
    Series title Special publication / SEPM (Society for Sedimentary Geology) ; 54
    Keywords Chronostratigraphie ; Stratigraphie ; Geologische Korrelation ; Geochronologie
    Language English
    Size VI, 386 S., Ill., graph. Darst., Kt
    Publisher SEPM (Society for Sedimentary Geology)
    Publishing place Tulsa, Okla
    Document type Book ; Conference proceedings
    Note Literaturangaben
    Accompanying material graph. Darst
    ISBN 1565760247 ; 9781565760240
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  3. Article: Review and revision of Cenozoic tropical planktonic foraminiferal biostratigraphy and calibration to the geomagnetic polarity and astronomical time scale

    Wade, Bridget S / Pearson, Paul N / Berggren, William A / Pälike, Heiko

    Earth-science reviews. 2011 Jan., v. 104, no. 1-3

    2011  

    Abstract: Planktonic foraminifera are widely utilized for the biostratigraphy of Cretaceous and Cenozoic marine sediments and are a fundamental component of Cenozoic chronostratigraphy. The recent enhancements in deep sea drilling recovery, multiple coring and ... ...

    Abstract Planktonic foraminifera are widely utilized for the biostratigraphy of Cretaceous and Cenozoic marine sediments and are a fundamental component of Cenozoic chronostratigraphy. The recent enhancements in deep sea drilling recovery, multiple coring and high resolution sampling both offshore and onshore, has improved the planktonic foraminiferal calibrations to magnetostratigraphy and/or modified species ranges. This accumulated new information has allowed many of the planktonic foraminiferal bioevents of the Cenozoic to be revised and the planktonic foraminiferal calibrations to be reassessed. We incorporate these developments and amendments into the existing biostratigraphic zonal scheme. In this paper we present an amended low-latitude (tropical and subtropical) Cenozoic planktonic foraminiferal zonation. We compile 187 revised calibrations of planktonic foraminiferal bioevents from multiple sources for the Cenozoic and have incorporated these recalibrations into a revised Cenozoic planktonic foraminiferal biochronology. We review and synthesize these calibrations to both the geomagnetic polarity time scale (GPTS) of the Cenozoic and astronomical time scale (ATS) of the Neogene and late Paleogene. On the whole, these recalibrations are consistent with the previous work; however, in some cases, they have led to major adjustments to the duration of biochrons. Recalibrations of the early–middle Eocene first appearance datums of Globigerinatheka kugleri, Hantkenina singanoae, Guembelitrioides nuttalli and Turborotalia frontosa have resulted in large changes in the durations of Biochrons E7, E8 and E9. We have introduced (upper Oligocene) Zone O7 utilizing the biostratigraphic utility of ‘Paragloborotalia’ pseudokugleri. For the Neogene Period, major revisions are applied to the fohsellid lineage of the middle Miocene and we have modified the criteria for recognition of Zones M7, M8 and M9, with additional adjustments regarding the Globigerinatella lineage to Zones M2 and M3. The revised and recalibrated datums provide a major advance in biochronologic resolution and a template for future progress of the Cenozoic time scale.
    Keywords drilling ; latitude ; marine sediments
    Language English
    Dates of publication 2011-01
    Size p. 111-142.
    Publishing place Elsevier B.V.
    Document type Article
    ZDB-ID 1792-9
    ISSN 0012-8252
    ISSN 0012-8252
    DOI 10.1016/j.earscirev.2010.09.003
    Database NAL-Catalogue (AGRICOLA)

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    In stock of ZB MED Bonn / Germany

    Z 69/92: Show issues

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  4. Book ; Online: Introduction to marine micropaleontology

    Berggren, William A / Haq, Bilal U

    1998  

    Abstract: This beautifully illustrated text book, with state-of-the-art illustrations, is useful not only for an introduction to the subject, but also for the application of marine microfossils in paleoceanographic, paleoenvironmental and biostratigraphic analyses. ...

    Author's details ed. by Bilal U. Haq
    Abstract This beautifully illustrated text book, with state-of-the-art illustrations, is useful not only for an introduction to the subject, but also for the application of marine microfossils in paleoceanographic, paleoenvironmental and biostratigraphic analyses. The recent revival of interest in marine micropaleontology worldwide in the wake of the development of sequence stratigraphic models has led to the decision to reissue the volume in its original, but paperback, form. The ideas expressed in various chapters of this second edition remain as valid today as they were when the book was first issued. The text, however, includes an updated Phanerozoic geologic time which has been considerably modified since the 1980s
    Keywords Fossil ; Mikrofossil ; Carbonate ; Biogenes Sediment ; Meeressediment ; Phosphate ; Silicate
    Language English
    Size Online-Ressource (VIII, 376 S)
    Edition [Nachdr.]
    Publisher Elsevier
    Publishing place Amsterdam u.a.
    Document type Book ; Online
    Note First ed. published 1978 ; Includes bibliographical references and index
    ISBN 0444826726 ; 9780444826725
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  5. Book ; Conference proceedings ; Online: Neogene planktonic foraminifera from the southern Kerguelen Plateau, supplementary data to: Berggren, William A (1992): Neogene planktonic foraminifer magnetostratigraphy of the southern Kerguelen Plateau (Sites 747, 748, 751). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 631-647

    Berggren, William A

    1992  

    Abstract: With the exception of a brief (2 m.y.) late Miocene-early Pliocene hiatus, an essentially complete Neogene record was recovered on the Kerguelen Plateau in a calcareous biofacies. The stratigraphic distribution of about 30 taxa of Neogene planktonic ... ...

    Abstract With the exception of a brief (2 m.y.) late Miocene-early Pliocene hiatus, an essentially complete Neogene record was recovered on the Kerguelen Plateau in a calcareous biofacies. The stratigraphic distribution of about 30 taxa of Neogene planktonic foraminifers recovered at Sites 747, 748,and 751 (Central and Southern Kerguelen plateaus; approximately 54°-58°S) is recorded. Faunas are characterized by low diversity and high dominance and exhibit a gradual decline in species numbers (reflecting a concomitant increase in biosiliceous forms, particularly diatoms) from about 10 in the early Miocene to 5-8 in the middle Miocene, 3-4 in the late Miocene, to essentially a lone (Neogloboquadrina pachyderma) form in the Pliocene-Pleistocene. A provisional sevenfold biostratigraphic zonation has been formulated that, together with the recovery of a representative Neogene magnetostratigraphic record, may ultimately lead to a correlation with low-latitude magnetobiostratigraphies. The initial appearance of Neogloboquadrina pachyderma is associated with magnetic polarity Chron (MPC) 4 (~7 Ma) and MPC 4A (>8 Ma) at Sites 747 and 751, respectively.
    Language English
    Dates of publication 1992-9999
    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.120.153.1992
    DOI 10.1594/PANGAEA.728761
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  6. Book ; Conference proceedings ; Online: Paleogene planktonic foraminifera from the southern Kerguelen Plateau, supplementary data to: Berggren, William A (1992): Paleogene planktonic foraminifer magnetobiostratigraphy of the southern Kerguelen Plateau (sites 747-749). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 551-568

    Berggren, William A

    1992  

    Abstract: An essentially complete Paleogene record was recovered on the Central and Southern Kerguelen plateaus (55?-59?S) in a calcareous biofacies. Recovery deteriorated in the middle Eocene and down to the upper Paleocene because of the presence of interbedded ... ...

    Abstract An essentially complete Paleogene record was recovered on the Central and Southern Kerguelen plateaus (55?-59?S) in a calcareous biofacies. Recovery deteriorated in the middle Eocene and down to the upper Paleocene because of the presence of interbedded cherts and chalks. The stratigraphic distribution of about 70 taxa of planktonic foraminifers recovered at Sites 747-749 is reported in this paper. Faunas exhibited fairly high diversity (approximately 20-25 species) in the early Eocene, followed by a gradual reduction in diversity in the middle Eocene. A brief incursion of tropical keeled morozovellids occurred near the Paleocene/Eocene boundary, similar to that recorded on the Maud Rise (ODP Sites 689 and 690).
    The high-latitude Paleogene zonal scheme developed for ODP Leg 113 sites has been adopted (with minor modifications) for the lower Eocene-Oligocene part of the Kerguelen Plateau record. A representative Oligocene (polarity chronozones 7-13) and late Eocene-late middle Eocene (questionably polarity chronozones 16-18) magnetostratigraphic record has allowed the calibration of several biostratigraphic datum levels to the standard Global Polarity Time Scale (GPTS) and established their essential synchrony between low and high latitudes.
    Language English
    Dates of publication 1992-9999
    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.120.151.1992
    DOI 10.1594/PANGAEA.728718
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  7. Book ; Online: The biostratigraphy and paleobiology of Oligocene planktonic foraminifera from the equatorial Pacific Ocean, supplementary data to: Wade, Bridget S; Berggren, William A; Olsson, Richard K (2007): The biostratigraphy and paleobiology of Oligocene planktonic foraminifera from the equatorial Pacific Ocean (ODP Site 1218). Marine Micropaleontology, 62(3), 167-179

    Wade, Bridget S / Berggren, William A / Olsson, Richard K

    2007  

    Abstract: Planktonic foraminifera from a continuous Oligocene succession with clear magnetochronology and sediment cycles at Ocean Drilling Program Site 1218 (equatorial Pacific Ocean) were studied in the interval from 27 to 30 Ma. Paragloborotalia taxa are common ...

    Abstract Planktonic foraminifera from a continuous Oligocene succession with clear magnetochronology and sediment cycles at Ocean Drilling Program Site 1218 (equatorial Pacific Ocean) were studied in the interval from 27 to 30 Ma. Paragloborotalia taxa are common and we examined their size, relative abundance, and stable isotopes. Multispecies stable isotope data indicate the depth habitats of Oligocene planktonic foraminifera and suggest that "Globoquadrina" venezuelana and Dentoglobigerina globularis were probably mixed-layer dwellers, with paragloborotaliids recording heavier delta18O signatures consistent with a thermocline habitat. Cyclic variations in the abundance of Paragloborotalia match eccentricity (100 kyr) variations in percent carbonate and delta13C, suggesting orbitally forced upwelling in the equatorial Pacific Ocean and that Paragloborotalia were responding directly to changes in surface water productivity. The high-resolution biostratigraphy calibrated to the magnetochronology constrains the extinction of Paragloborotalia opima which marks the top of Planktonic Foraminifera Biozone O5 (P21b) at 27.456 Ma. The highest occurrence of P. opima is associated with a 50% size decrease in Paragloborotalia pseudocontinuosa taxa within Chron 9n. In addition, we find the extinction of Chiloguembelina cubensis is consistent with other deep-sea sections within Chron 10n at 28.426 Ma marking the O4/O5 (P21a/P21b) boundary.
    Language English
    Dates of publication 2007-9999
    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:10.1016/j.marmicro.2006.08.005
    DOI 10.1594/PANGAEA.691329
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  8. Book ; Conference proceedings ; Online: Paleogene benthic foraminifera from the Kerguelen Plateau, supplementary data to: Mackensen, Andreas; Berggren, William A (1992): Paleogene benthic foraminifers from the southern Indian Ocean (Kerguelen Plateau): biostratigraphy and paleoecology. In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 603-630

    Mackensen, Andreas / Berggren, William A

    1992  

    Abstract: Benthic foraminifers were studied from lower Paleocene through upper Oligocene sections from Sites 747 and 748. The composition of the benthic foraminifer species suggests a middle to lower bathyal (600-2000 m) paleodepth during the Neogene and a ... ...

    Abstract Benthic foraminifers were studied from lower Paleocene through upper Oligocene sections from Sites 747 and 748. The composition of the benthic foraminifer species suggests a middle to lower bathyal (600-2000 m) paleodepth during the Neogene and a probable upper abyssal (2000-3000 m) paleodepth during the Paleocene at Site 747. Site 748 is thought to have remained at middle to lower bathyal paleodepths throughout the Cenozoic. Principal component analysis distinguished four major benthic foraminifer assemblages: (1) a Paleocene Stensioina beccariiformis assemblage at Sites 747 and 748, (2) an early Eocene Nuttallides truempyi assemblage at lower bathyal Site 747, (3) an early through middle Eocene Stilostomella-Lenticulina assemblage at middle bathyal Site 748, and (4) a latest Eocene through Oligocene Cibicidoides-Astrononion pusillum assemblage at both sites. Major benthic foraminifer changes, as indicated by the principal components and first and last appearances, occurred at or close to the Paleocene/Eocene boundary, and in the late Eocene close to the middle/late Eocene boundary.
    Language English
    Dates of publication 1992-9999
    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.120.168.1992
    DOI 10.1594/PANGAEA.728746
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  9. Book: Catastrophes and earth history

    Berggren, William A / Van Couvering, John A

    the new uniformitarianism

    1984  

    Author's details W.A. Berggren and John A. Van Couvering, editors
    Keywords Catastrophes (Geology)/Congresses. ; Extinction (Biology)/Congresses. ; Paleontology/Congresses.
    Language English
    Size xii, 464 p. :, ill., maps ;, 25 cm.
    Publisher Princeton University Press
    Publishing place Princeton, N.J
    Document type Book
    Note Papers from a symposium held in the Woods Hole Oceanographic Institution, June 6-10, 1977, and from a symposium held in connection with the Second North American Palaeontological Convention in Aug. 1977 at Lawrence, Kan.
    ISBN 0691083282 ; 0691083290 ; 9780691083285 ; 9780691083292
    Database NAL-Catalogue (AGRICOLA)

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  10. Book ; Conference proceedings: Catastrophes and earth history

    Berggren, William A / Couvering, John A. van

    the new uniformitarianism

    1984  

    Event/congress Symposium in connection with the North American Paleontological Convention (2, 1977.08, LawrenceKan.) ; Woods Hole Oceanographic Institution symposium (1977.06.06-10)
    Author's details W. E. Berggren; John A. van Couvering
    Keywords Catastrophes (Geology)/Congresses ; Extinction (Biology)/Congresses ; Paleontology/Congresses
    Language English
    Size XII, 464 S, graph. Darst
    Publisher Princeton Univ. Press
    Publishing place Princeton, NJ
    Document type Book ; Conference proceedings
    Note Literaturangaben
    ISBN 0691083282 ; 0691083290 ; 9780691083285 ; 9780691083292
    Database Former special subject collection: coastal and deep sea fishing

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