B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1)
Knowledge of past atmospheric pCO2 is important for evaluating the role of greenhouse gases in climate forcing. Ice core records show the tight correlation between climate change and pCO2, but records are limited to the past ~900 kyr. We present surface ocean pH and pCO2 data, reconstructed from bor...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.712921 2024-09-15T18:12:01+00:00 B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1) Hönisch, Bärbel Hemming, N Gary LATITUDE: 4.768700 * LONGITUDE: -20.927000 * DATE/TIME START: 1986-04-14T11:30:00 * DATE/TIME END: 1986-04-15T04:45:00 * MINIMUM ELEVATION: -2693.5 m * MAXIMUM ELEVATION: -2693.5 m 2005 text/tab-separated-values, 308 data points https://doi.pangaea.de/10.1594/PANGAEA.712921 https://doi.org/10.1594/PANGAEA.712921 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.712921 https://doi.org/10.1594/PANGAEA.712921 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Hönisch, Bärbel; Hemming, N Gary (2005): Surface ocean pH response to variations in pCO2 through two full glacial cycles. Earth and Planetary Science Letters, 236(1-2), 305-314, https://doi.org/10.1016/j.epsl.2005.04.027 108-668B AGE Alkalinity total Calculated Calculated from Mg/Ca ratios (Dekens et al. 2002) Carbon dioxide partial pressure DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Globigerinoides ruber Magnesium/Calcium ratio Inductively coupled plasma - mass spectrometry (ICP-MS) Joides Resolution Leg108 standard deviation Mass North Atlantic Ocean Number Ocean Drilling Program ODP pH Salinity Sample code/label Sea level variation Sea surface temperature annual mean Thermal Ionization Mass Spectrometry (TIMS) δ11B δ18O water dataset 2005 ftpangaea https://doi.org/10.1594/PANGAEA.71292110.1016/j.epsl.2005.04.027 2024-08-21T00:02:26Z Knowledge of past atmospheric pCO2 is important for evaluating the role of greenhouse gases in climate forcing. Ice core records show the tight correlation between climate change and pCO2, but records are limited to the past ~900 kyr. We present surface ocean pH and pCO2 data, reconstructed from boron isotopes in planktonic foraminifera over two full glacial cycles (0-140 and 300-420 kyr). The data co-vary strongly with the Vostok pCO2-record and demonstrate that the coupling between surface ocean chemistry and the atmosphere is recorded in marine archives, allowing for quantitative estimation of atmospheric pCO2 beyond the reach of ice cores. Dataset ice core North Atlantic Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-20.927000,-20.927000,4.768700,4.768700) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
108-668B AGE Alkalinity total Calculated Calculated from Mg/Ca ratios (Dekens et al. 2002) Carbon dioxide partial pressure DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Globigerinoides ruber Magnesium/Calcium ratio Inductively coupled plasma - mass spectrometry (ICP-MS) Joides Resolution Leg108 standard deviation Mass North Atlantic Ocean Number Ocean Drilling Program ODP pH Salinity Sample code/label Sea level variation Sea surface temperature annual mean Thermal Ionization Mass Spectrometry (TIMS) δ11B δ18O water |
spellingShingle |
108-668B AGE Alkalinity total Calculated Calculated from Mg/Ca ratios (Dekens et al. 2002) Carbon dioxide partial pressure DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Globigerinoides ruber Magnesium/Calcium ratio Inductively coupled plasma - mass spectrometry (ICP-MS) Joides Resolution Leg108 standard deviation Mass North Atlantic Ocean Number Ocean Drilling Program ODP pH Salinity Sample code/label Sea level variation Sea surface temperature annual mean Thermal Ionization Mass Spectrometry (TIMS) δ11B δ18O water Hönisch, Bärbel Hemming, N Gary B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1) |
topic_facet |
108-668B AGE Alkalinity total Calculated Calculated from Mg/Ca ratios (Dekens et al. 2002) Carbon dioxide partial pressure DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Globigerinoides ruber Magnesium/Calcium ratio Inductively coupled plasma - mass spectrometry (ICP-MS) Joides Resolution Leg108 standard deviation Mass North Atlantic Ocean Number Ocean Drilling Program ODP pH Salinity Sample code/label Sea level variation Sea surface temperature annual mean Thermal Ionization Mass Spectrometry (TIMS) δ11B δ18O water |
description |
Knowledge of past atmospheric pCO2 is important for evaluating the role of greenhouse gases in climate forcing. Ice core records show the tight correlation between climate change and pCO2, but records are limited to the past ~900 kyr. We present surface ocean pH and pCO2 data, reconstructed from boron isotopes in planktonic foraminifera over two full glacial cycles (0-140 and 300-420 kyr). The data co-vary strongly with the Vostok pCO2-record and demonstrate that the coupling between surface ocean chemistry and the atmosphere is recorded in marine archives, allowing for quantitative estimation of atmospheric pCO2 beyond the reach of ice cores. |
format |
Dataset |
author |
Hönisch, Bärbel Hemming, N Gary |
author_facet |
Hönisch, Bärbel Hemming, N Gary |
author_sort |
Hönisch, Bärbel |
title |
B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1) |
title_short |
B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1) |
title_full |
B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1) |
title_fullStr |
B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1) |
title_full_unstemmed |
B-isotope and Mg/Ca ratios of planktonic foraminifera from ODP Hole 108-668B and esimates of salinity, alkalinity and pCO2 (Table 1) |
title_sort |
b-isotope and mg/ca ratios of planktonic foraminifera from odp hole 108-668b and esimates of salinity, alkalinity and pco2 (table 1) |
publisher |
PANGAEA |
publishDate |
2005 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.712921 https://doi.org/10.1594/PANGAEA.712921 |
op_coverage |
LATITUDE: 4.768700 * LONGITUDE: -20.927000 * DATE/TIME START: 1986-04-14T11:30:00 * DATE/TIME END: 1986-04-15T04:45:00 * MINIMUM ELEVATION: -2693.5 m * MAXIMUM ELEVATION: -2693.5 m |
long_lat |
ENVELOPE(-20.927000,-20.927000,4.768700,4.768700) |
genre |
ice core North Atlantic Planktonic foraminifera |
genre_facet |
ice core North Atlantic Planktonic foraminifera |
op_source |
Supplement to: Hönisch, Bärbel; Hemming, N Gary (2005): Surface ocean pH response to variations in pCO2 through two full glacial cycles. Earth and Planetary Science Letters, 236(1-2), 305-314, https://doi.org/10.1016/j.epsl.2005.04.027 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.712921 https://doi.org/10.1594/PANGAEA.712921 |
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.71292110.1016/j.epsl.2005.04.027 |
_version_ |
1810449613511983104 |