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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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 |
_version_ |
1810472643513548800 |