Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera
Stable carbon and oxygen isotopic analyses of the planktonic foraminifera (Globigerinoides ruber) from a deep sea sediment core (GC-1) in the Andaman Sea show high glacial-to-Holocene d 18 O amplitude of 2.1% which is consistent with previously published records from this marginal basin and suggest...
Main Authors: | , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Indian Academy of Sciences
2000
|
Subjects: | |
Online Access: | http://drs.nio.org/drs/handle/2264/357 |
id |
ftnio:oai:dsr.nio.org:2264/357 |
---|---|
record_format |
openpolar |
spelling |
ftnio:oai:dsr.nio.org:2264/357 2023-05-15T18:00:28+02:00 Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera Ahmad, S.M. Patil, D.J. Rao, P.S. Nath, B.N. Rao, B.R. Rajagopalan, G. 2000 91299 bytes application/pdf http://drs.nio.org/drs/handle/2264/357 en eng Indian Academy of Sciences Andaman Sea Globigerinoides ruber Article 2000 ftnio 2012-08-25T20:03:09Z Stable carbon and oxygen isotopic analyses of the planktonic foraminifera (Globigerinoides ruber) from a deep sea sediment core (GC-1) in the Andaman Sea show high glacial-to-Holocene d 18 O amplitude of 2.1% which is consistent with previously published records from this marginal basin and suggest increased salinity and/or decreased temperature in the glacial surface waters of this region. A pulse of 18 O enrichment during the last deglaciation can be attributed to a Younger Dryas cooling event and/or to a sudden decrease of fresh water influx from the Irrawady and Salween rivers into the Andaman Sea. High d 13 C values observed during the isotopic stages 2 and 4 are probably due to the enhanced productivity during glacial times in the Andaman Sea. Article in Journal/Newspaper Planktonic foraminifera National Institute of Oceanography, India: Digital Repository Service (DRS@nio) |
institution |
Open Polar |
collection |
National Institute of Oceanography, India: Digital Repository Service (DRS@nio) |
op_collection_id |
ftnio |
language |
English |
topic |
Andaman Sea Globigerinoides ruber |
spellingShingle |
Andaman Sea Globigerinoides ruber Ahmad, S.M. Patil, D.J. Rao, P.S. Nath, B.N. Rao, B.R. Rajagopalan, G. Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera |
topic_facet |
Andaman Sea Globigerinoides ruber |
description |
Stable carbon and oxygen isotopic analyses of the planktonic foraminifera (Globigerinoides ruber) from a deep sea sediment core (GC-1) in the Andaman Sea show high glacial-to-Holocene d 18 O amplitude of 2.1% which is consistent with previously published records from this marginal basin and suggest increased salinity and/or decreased temperature in the glacial surface waters of this region. A pulse of 18 O enrichment during the last deglaciation can be attributed to a Younger Dryas cooling event and/or to a sudden decrease of fresh water influx from the Irrawady and Salween rivers into the Andaman Sea. High d 13 C values observed during the isotopic stages 2 and 4 are probably due to the enhanced productivity during glacial times in the Andaman Sea. |
format |
Article in Journal/Newspaper |
author |
Ahmad, S.M. Patil, D.J. Rao, P.S. Nath, B.N. Rao, B.R. Rajagopalan, G. |
author_facet |
Ahmad, S.M. Patil, D.J. Rao, P.S. Nath, B.N. Rao, B.R. Rajagopalan, G. |
author_sort |
Ahmad, S.M. |
title |
Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera |
title_short |
Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera |
title_full |
Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera |
title_fullStr |
Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera |
title_full_unstemmed |
Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera |
title_sort |
glacial-interglacial changes in the surface water characteristics of the andaman sea: evidence from stable isotopic ratios of planktonic foraminifera |
publisher |
Indian Academy of Sciences |
publishDate |
2000 |
url |
http://drs.nio.org/drs/handle/2264/357 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
_version_ |
1766169572946214912 |