Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ...

Quantitative analysis was performed on the Quaternary planktonic foraminiferal fauna from Site 516, near the crest of the Rio Grande Rise, and Site 518, on the lower western flank of the Rise. From Hole 516, 46 samples were taken, and from Hole 518, 80 samples were taken. The mean interval between s...

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Main Authors: Barash, Max S, Oskina, Natalia S, Blyum, Natalia S
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1983
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.811803
https://doi.pangaea.de/10.1594/PANGAEA.811803
id ftdatacite:10.1594/pangaea.811803
record_format openpolar
spelling ftdatacite:10.1594/pangaea.811803 2024-09-15T18:31:03+00:00 Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ... Barash, Max S Oskina, Natalia S Blyum, Natalia S 1983 application/zip https://dx.doi.org/10.1594/pangaea.811803 https://doi.pangaea.de/10.1594/PANGAEA.811803 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.72.142.1983 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg72 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1983 ftdatacite https://doi.org/10.1594/pangaea.81180310.2973/dsdp.proc.72.142.1983 2024-08-01T10:51:01Z Quantitative analysis was performed on the Quaternary planktonic foraminiferal fauna from Site 516, near the crest of the Rio Grande Rise, and Site 518, on the lower western flank of the Rise. From Hole 516, 46 samples were taken, and from Hole 518, 80 samples were taken. The mean interval between samples is 20 to 25 cm. About 50 species of Quaternary and Pliocene planktonic foraminifers were identified. Quaternary sediments, dated by the initial evolutionary appearance of Globorotalia truncatulinoides and other criteria, have thickness, of 9.8 m in Hole 516 and 16 m in Hole 518. The Globorotalia truncatulinoides Zone is subdivided into four subzones or biostratigraphic horizons (from lower to upper): (1) Globorotalia crassaformis viola, (2) Globorotalia crassaformis hessi, (3) Globigerina calida calida, and (4) Globigerinoides ruber (pink). Thickness of these horizons in Hole 516 establishes the age of the boundaries between them as 1.47, 0.81, and 0.28 Ma, respectively. All the Quaternary planktonic ... : Supplement to: Barash, Max S; Oskina, Natalia S; Blyum, Natalia S (1983): Quaternary biostratigraphy and surface paleotemperatures based on planktonic foraminifers. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 849-869 ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg72
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Leg72
Glomar Challenger
Deep Sea Drilling Project DSDP
Barash, Max S
Oskina, Natalia S
Blyum, Natalia S
Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ...
topic_facet Drilling/drill rig
Leg72
Glomar Challenger
Deep Sea Drilling Project DSDP
description Quantitative analysis was performed on the Quaternary planktonic foraminiferal fauna from Site 516, near the crest of the Rio Grande Rise, and Site 518, on the lower western flank of the Rise. From Hole 516, 46 samples were taken, and from Hole 518, 80 samples were taken. The mean interval between samples is 20 to 25 cm. About 50 species of Quaternary and Pliocene planktonic foraminifers were identified. Quaternary sediments, dated by the initial evolutionary appearance of Globorotalia truncatulinoides and other criteria, have thickness, of 9.8 m in Hole 516 and 16 m in Hole 518. The Globorotalia truncatulinoides Zone is subdivided into four subzones or biostratigraphic horizons (from lower to upper): (1) Globorotalia crassaformis viola, (2) Globorotalia crassaformis hessi, (3) Globigerina calida calida, and (4) Globigerinoides ruber (pink). Thickness of these horizons in Hole 516 establishes the age of the boundaries between them as 1.47, 0.81, and 0.28 Ma, respectively. All the Quaternary planktonic ... : Supplement to: Barash, Max S; Oskina, Natalia S; Blyum, Natalia S (1983): Quaternary biostratigraphy and surface paleotemperatures based on planktonic foraminifers. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 849-869 ...
format Article in Journal/Newspaper
author Barash, Max S
Oskina, Natalia S
Blyum, Natalia S
author_facet Barash, Max S
Oskina, Natalia S
Blyum, Natalia S
author_sort Barash, Max S
title Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ...
title_short Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ...
title_full Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ...
title_fullStr Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ...
title_full_unstemmed Planktonic foraminifera at DSDP Holes 72-516 and 72-518 ...
title_sort planktonic foraminifera at dsdp holes 72-516 and 72-518 ...
publisher PANGAEA
publishDate 1983
url https://dx.doi.org/10.1594/pangaea.811803
https://doi.pangaea.de/10.1594/PANGAEA.811803
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.2973/dsdp.proc.72.142.1983
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.81180310.2973/dsdp.proc.72.142.1983
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