Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ...
Production of Globigerina bulloides generally increases during upwelling in the tropical ocean and, in particular, during southwest monsoon season in the Arabian Sea. We studied the d13C signatures of G. bulloides from Ocean Drilling Program (ODP) site 723A located in the intense upwelling area alon...
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ftdatacite:10.1594/pangaea.678266 2024-09-15T18:31:04+00:00 Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ... Naidu, Pothuri Divakar Niitsuma, Nobuaki 2004 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.678266 https://doi.pangaea.de/10.1594/PANGAEA.678266 en eng PANGAEA https://dx.doi.org/10.1016/j.marmicro.2004.01.005 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock AGE Globigerina bulloides, δ13C Drilling/drill rig Mass spectrometer Finnigan MAT 250 Leg117 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 2004 ftdatacite https://doi.org/10.1594/pangaea.67826610.1016/j.marmicro.2004.01.005 2024-08-01T10:59:11Z Production of Globigerina bulloides generally increases during upwelling in the tropical ocean and, in particular, during southwest monsoon season in the Arabian Sea. We studied the d13C signatures of G. bulloides from Ocean Drilling Program (ODP) site 723A located in the intense upwelling area along the Oman Margin, Arabian Sea. The delta13C signature of G. bulloides from the Oman Margin during the last 19 ka ranges from -2.65‰ to -1.13‰. Strikingly, the delta13C values of G. bulloides are about 1‰ lower than that of benthic foraminifera Uvigerina excellens at this site. Apparently, the vital effects induced carbon isotopic fractionation in G. bulloides results in abnormal delta13C values. During upwelling seasons, G. bulloides calcifies faster, perhaps because of high-nutrient availability. Faster calcification rates in this species require higher respiration, which involves more respired CO2 enriched with 12C accounting for nearly 10% of shell carbon. Therefore, the combination the foraminifera of faster ... : Age after Naidu and Malmgren (1996) data set doi:10.1594/PANGAEA.52692. For carbon isotope data of Uvigerina excellens see Niitsuma et al. (1991) data set doi:10.1594/PANGAEA.695216, for oxygen isotope data of Globigerina bulloides see Naidu and Niitsuma (2003) data set doi:10.1594/PANGAEA.695217 ... Dataset Planktonic foraminifera DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock AGE Globigerina bulloides, δ13C Drilling/drill rig Mass spectrometer Finnigan MAT 250 Leg117 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
DEPTH, sediment/rock AGE Globigerina bulloides, δ13C Drilling/drill rig Mass spectrometer Finnigan MAT 250 Leg117 Joides Resolution Ocean Drilling Program ODP Naidu, Pothuri Divakar Niitsuma, Nobuaki Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ... |
topic_facet |
DEPTH, sediment/rock AGE Globigerina bulloides, δ13C Drilling/drill rig Mass spectrometer Finnigan MAT 250 Leg117 Joides Resolution Ocean Drilling Program ODP |
description |
Production of Globigerina bulloides generally increases during upwelling in the tropical ocean and, in particular, during southwest monsoon season in the Arabian Sea. We studied the d13C signatures of G. bulloides from Ocean Drilling Program (ODP) site 723A located in the intense upwelling area along the Oman Margin, Arabian Sea. The delta13C signature of G. bulloides from the Oman Margin during the last 19 ka ranges from -2.65‰ to -1.13‰. Strikingly, the delta13C values of G. bulloides are about 1‰ lower than that of benthic foraminifera Uvigerina excellens at this site. Apparently, the vital effects induced carbon isotopic fractionation in G. bulloides results in abnormal delta13C values. During upwelling seasons, G. bulloides calcifies faster, perhaps because of high-nutrient availability. Faster calcification rates in this species require higher respiration, which involves more respired CO2 enriched with 12C accounting for nearly 10% of shell carbon. Therefore, the combination the foraminifera of faster ... : Age after Naidu and Malmgren (1996) data set doi:10.1594/PANGAEA.52692. For carbon isotope data of Uvigerina excellens see Niitsuma et al. (1991) data set doi:10.1594/PANGAEA.695216, for oxygen isotope data of Globigerina bulloides see Naidu and Niitsuma (2003) data set doi:10.1594/PANGAEA.695217 ... |
format |
Dataset |
author |
Naidu, Pothuri Divakar Niitsuma, Nobuaki |
author_facet |
Naidu, Pothuri Divakar Niitsuma, Nobuaki |
author_sort |
Naidu, Pothuri Divakar |
title |
Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ... |
title_short |
Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ... |
title_full |
Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ... |
title_fullStr |
Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ... |
title_full_unstemmed |
Stable carbon isotope ratios of the planktonic foraminifera Globigerina bulloides in ODP Hole 117-723A from the Arabian Sea (Table 2) ... |
title_sort |
stable carbon isotope ratios of the planktonic foraminifera globigerina bulloides in odp hole 117-723a from the arabian sea (table 2) ... |
publisher |
PANGAEA |
publishDate |
2004 |
url |
https://dx.doi.org/10.1594/pangaea.678266 https://doi.pangaea.de/10.1594/PANGAEA.678266 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1016/j.marmicro.2004.01.005 |
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.67826610.1016/j.marmicro.2004.01.005 |
_version_ |
1810472667316224000 |