(Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C
The carbon dioxide content of the atmosphere [measured as the partial pressure of CO2 (pCO2)] affects the content of the surface ocean, which in turn affects seawater pH. The boron isotope composition (d11B) of contemporaneous planktonic foraminifera that calcified their tests at different water dep...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.769847 2024-09-15T18:31:00+00:00 (Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C Pearson, Paul N Palmer, Martin R LATITUDE: 18.440400 * LONGITUDE: -179.555000 * DATE/TIME START: 1992-04-04T01:30:00 * DATE/TIME END: 1992-04-04T14:15:00 * MINIMUM ELEVATION: -1528.0 m * MAXIMUM ELEVATION: -1528.0 m 1999 text/tab-separated-values, 168 data points https://doi.pangaea.de/10.1594/PANGAEA.769847 https://doi.org/10.1594/PANGAEA.769847 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.769847 https://doi.org/10.1594/PANGAEA.769847 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Pearson, Paul N; Palmer, Martin R (1999): Middle Eocene Seawater pH and Atmospheric Carbon Dioxide Concentrations. Science, 284(5421), 1824-1826, https://doi.org/10.1126/science.284.5421.1824 143-865C Comment DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg143 North Pacific Ocean Ocean Drilling Program ODP Sample code/label Size Species δ11B standard deviation dataset 1999 ftpangaea https://doi.org/10.1594/PANGAEA.76984710.1126/science.284.5421.1824 2024-07-24T02:31:31Z The carbon dioxide content of the atmosphere [measured as the partial pressure of CO2 (pCO2)] affects the content of the surface ocean, which in turn affects seawater pH. The boron isotope composition (d11B) of contemporaneous planktonic foraminifera that calcified their tests at different water depths can be used to reconstruct the pH-depth profile of ancient seawater. Construction of a pH profile for the middle Eocene tropical Pacific Ocean shows that atmospheric pCO2 was probably similar to modern concentrations or slightly higher. Dataset Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-179.555000,-179.555000,18.440400,18.440400) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
143-865C Comment DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg143 North Pacific Ocean Ocean Drilling Program ODP Sample code/label Size Species δ11B standard deviation |
spellingShingle |
143-865C Comment DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg143 North Pacific Ocean Ocean Drilling Program ODP Sample code/label Size Species δ11B standard deviation Pearson, Paul N Palmer, Martin R (Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C |
topic_facet |
143-865C Comment DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg143 North Pacific Ocean Ocean Drilling Program ODP Sample code/label Size Species δ11B standard deviation |
description |
The carbon dioxide content of the atmosphere [measured as the partial pressure of CO2 (pCO2)] affects the content of the surface ocean, which in turn affects seawater pH. The boron isotope composition (d11B) of contemporaneous planktonic foraminifera that calcified their tests at different water depths can be used to reconstruct the pH-depth profile of ancient seawater. Construction of a pH profile for the middle Eocene tropical Pacific Ocean shows that atmospheric pCO2 was probably similar to modern concentrations or slightly higher. |
format |
Dataset |
author |
Pearson, Paul N Palmer, Martin R |
author_facet |
Pearson, Paul N Palmer, Martin R |
author_sort |
Pearson, Paul N |
title |
(Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C |
title_short |
(Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C |
title_full |
(Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C |
title_fullStr |
(Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C |
title_full_unstemmed |
(Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C |
title_sort |
(table 1) boron-isotope measurements of foraminifera of odp hole 143-865c |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.769847 https://doi.org/10.1594/PANGAEA.769847 |
op_coverage |
LATITUDE: 18.440400 * LONGITUDE: -179.555000 * DATE/TIME START: 1992-04-04T01:30:00 * DATE/TIME END: 1992-04-04T14:15:00 * MINIMUM ELEVATION: -1528.0 m * MAXIMUM ELEVATION: -1528.0 m |
long_lat |
ENVELOPE(-179.555000,-179.555000,18.440400,18.440400) |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Supplement to: Pearson, Paul N; Palmer, Martin R (1999): Middle Eocene Seawater pH and Atmospheric Carbon Dioxide Concentrations. Science, 284(5421), 1824-1826, https://doi.org/10.1126/science.284.5421.1824 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.769847 https://doi.org/10.1594/PANGAEA.769847 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.76984710.1126/science.284.5421.1824 |
_version_ |
1810472595178389504 |