(Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ...
Foraminifer count and multispecies isotopic data from Ocean Drilling Program (ODP) Sites 806 (0°N, 165°E) and 847 (0°N, 95°W) are presented for the last 6.4 m.y. Faunal evidence shows a decline of taxa of Miocene origin between 4.5 and 4.0 Ma at both sites. Prior to this decline, Globoturborotalita...
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ftdatacite:10.1594/pangaea.848108 2024-09-15T18:31:04+00:00 (Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ... Chaisson, William P Ravelo, Ana Christina 2000 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.848108 https://doi.pangaea.de/10.1594/PANGAEA.848108 en eng PANGAEA https://dx.doi.org/10.1029/1999pa000442 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Sample code/label DEPTH, sediment/rock AGE Globigerinoides sacculifer sac, δ18O Neogloboquadrina dutertrei, δ18O Globorotalia tumida, δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg130 Leg138 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 2000 ftdatacite https://doi.org/10.1594/pangaea.84810810.1029/1999pa000442 2024-08-01T10:53:02Z Foraminifer count and multispecies isotopic data from Ocean Drilling Program (ODP) Sites 806 (0°N, 165°E) and 847 (0°N, 95°W) are presented for the last 6.4 m.y. Faunal evidence shows a decline of taxa of Miocene origin between 4.5 and 4.0 Ma at both sites. Prior to this decline, Globoturborotalita species and Neogloboquadrina acostaensis dominated Sites 806 and 847 assemblages, respectively. Globoturborotalitids were not replaced by other thermocline dwellers after 4.2 Ma, which suggests a deepening of the thermocline and thickening of the warm pool at Site 806. At Site 847 in the eastern “cold tongue”, N. acostaensis was gradually replaced by N. dutertrei. After 4.2 Ma, there was also a large increase (from 0.7 to 1.3 per mil) in the difference between the d18O values of Globigerinoides sacculifer, a surface dweller, and Neogloboquadrina dutertrei, a seasonal thermocline dweller at Site 847; these data, in conjunction with faunal evidence, suggest that the temperature gradient in the upper photic zone ... : Supplement to: Chaisson, William P; Ravelo, Ana Christina (2000): Pliocene development of the east-west hydrographic gradient in the equatorial Pacific. Paleoceanography, 15(5), 497-505 ... Dataset Planktonic foraminifera DataCite |
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language |
English |
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Event label Sample code/label DEPTH, sediment/rock AGE Globigerinoides sacculifer sac, δ18O Neogloboquadrina dutertrei, δ18O Globorotalia tumida, δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg130 Leg138 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Event label Sample code/label DEPTH, sediment/rock AGE Globigerinoides sacculifer sac, δ18O Neogloboquadrina dutertrei, δ18O Globorotalia tumida, δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg130 Leg138 Joides Resolution Ocean Drilling Program ODP Chaisson, William P Ravelo, Ana Christina (Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ... |
topic_facet |
Event label Sample code/label DEPTH, sediment/rock AGE Globigerinoides sacculifer sac, δ18O Neogloboquadrina dutertrei, δ18O Globorotalia tumida, δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg130 Leg138 Joides Resolution Ocean Drilling Program ODP |
description |
Foraminifer count and multispecies isotopic data from Ocean Drilling Program (ODP) Sites 806 (0°N, 165°E) and 847 (0°N, 95°W) are presented for the last 6.4 m.y. Faunal evidence shows a decline of taxa of Miocene origin between 4.5 and 4.0 Ma at both sites. Prior to this decline, Globoturborotalita species and Neogloboquadrina acostaensis dominated Sites 806 and 847 assemblages, respectively. Globoturborotalitids were not replaced by other thermocline dwellers after 4.2 Ma, which suggests a deepening of the thermocline and thickening of the warm pool at Site 806. At Site 847 in the eastern “cold tongue”, N. acostaensis was gradually replaced by N. dutertrei. After 4.2 Ma, there was also a large increase (from 0.7 to 1.3 per mil) in the difference between the d18O values of Globigerinoides sacculifer, a surface dweller, and Neogloboquadrina dutertrei, a seasonal thermocline dweller at Site 847; these data, in conjunction with faunal evidence, suggest that the temperature gradient in the upper photic zone ... : Supplement to: Chaisson, William P; Ravelo, Ana Christina (2000): Pliocene development of the east-west hydrographic gradient in the equatorial Pacific. Paleoceanography, 15(5), 497-505 ... |
format |
Dataset |
author |
Chaisson, William P Ravelo, Ana Christina |
author_facet |
Chaisson, William P Ravelo, Ana Christina |
author_sort |
Chaisson, William P |
title |
(Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ... |
title_short |
(Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ... |
title_full |
(Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ... |
title_fullStr |
(Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ... |
title_full_unstemmed |
(Table 1) Oxygen isotopic composition of planktonic foraminifera of ODP Holes 130-806B and 138-847B ... |
title_sort |
(table 1) oxygen isotopic composition of planktonic foraminifera of odp holes 130-806b and 138-847b ... |
publisher |
PANGAEA |
publishDate |
2000 |
url |
https://dx.doi.org/10.1594/pangaea.848108 https://doi.pangaea.de/10.1594/PANGAEA.848108 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1029/1999pa000442 |
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.84810810.1029/1999pa000442 |
_version_ |
1810472670153670656 |