A 28-ka history of sea surface tempeture, primary productivity and planktonic community variability in the western Arabian Sea

Ali Pourmand, Franco Marcantonio, Thomas S. Bianchi, Elizabeth A. Canuel, Elizabeth J. Waterson

Research output: Contribution to journalArticle

16 Citations (Scopus)

Abstract

Uranium series radionuclides and organic biomarkers, which represent major groups of planktonic organisms, were measured in western Arabian Sea sediments that span the past 28 ka. Variability in the past strength of the southwest and northeast monsoons and its influence on primary productivity, sea surface temperature (SST), and planktonic community structure were investigated. The average alkenone-derived SST for the last glacial period was ∼3°C lower than that measured for the Holocene. Prior to the deglacial, the lowest SSTs coincide with the highest measured fluxes of organic biomarkers, which represent primarily a planktonic suite of diatoms, coccolithophorids, dinoflagellates, and zooplankton. We propose that intensification of winter northeast monsoon winds during the last glacial period resulted in deep convective mixing, cold SSTs and enhanced primary productivity. In contrast, postdeglacial (<17 ka) SSTs are warmer during times in which biomarker fluxes are high. Associated with this transition is a planktonic community structure change, in which the ratio of the average cumulative flux of diatom biomarkers to the cumulative flux of coccolithophorid biomarkers is twice as high during the deglacial and Holocene than the average ratio during the last glacial period. We suggest that this temporal transition represents a shift from a winter northeast monsoon-dominated (pre-17 ka) to a summer southwest monsoon-dominated (post-17 ka) wind system.

Original languageEnglish (US)
Article numberPA4208
JournalPaleoceanography
Volume22
Issue number4
DOIs
StatePublished - Dec 2007
Externally publishedYes

Fingerprint

biomarker
sea surface
sea surface temperature
monsoon
Last Glacial
productivity
history
community structure
diatom
Holocene
alkenone
winter
dinoflagellate
radionuclide
uranium
zooplankton
sea
summer
sediment

ASJC Scopus subject areas

  • Oceanography
  • Palaeontology

Cite this

A 28-ka history of sea surface tempeture, primary productivity and planktonic community variability in the western Arabian Sea. / Pourmand, Ali; Marcantonio, Franco; Bianchi, Thomas S.; Canuel, Elizabeth A.; Waterson, Elizabeth J.

In: Paleoceanography, Vol. 22, No. 4, PA4208, 12.2007.

Research output: Contribution to journalArticle

Pourmand, Ali ; Marcantonio, Franco ; Bianchi, Thomas S. ; Canuel, Elizabeth A. ; Waterson, Elizabeth J. / A 28-ka history of sea surface tempeture, primary productivity and planktonic community variability in the western Arabian Sea. In: Paleoceanography. 2007 ; Vol. 22, No. 4.
@article{ccd9058f5e4b4ec5969110be2fc4d644,
title = "A 28-ka history of sea surface tempeture, primary productivity and planktonic community variability in the western Arabian Sea",
abstract = "Uranium series radionuclides and organic biomarkers, which represent major groups of planktonic organisms, were measured in western Arabian Sea sediments that span the past 28 ka. Variability in the past strength of the southwest and northeast monsoons and its influence on primary productivity, sea surface temperature (SST), and planktonic community structure were investigated. The average alkenone-derived SST for the last glacial period was ∼3°C lower than that measured for the Holocene. Prior to the deglacial, the lowest SSTs coincide with the highest measured fluxes of organic biomarkers, which represent primarily a planktonic suite of diatoms, coccolithophorids, dinoflagellates, and zooplankton. We propose that intensification of winter northeast monsoon winds during the last glacial period resulted in deep convective mixing, cold SSTs and enhanced primary productivity. In contrast, postdeglacial (<17 ka) SSTs are warmer during times in which biomarker fluxes are high. Associated with this transition is a planktonic community structure change, in which the ratio of the average cumulative flux of diatom biomarkers to the cumulative flux of coccolithophorid biomarkers is twice as high during the deglacial and Holocene than the average ratio during the last glacial period. We suggest that this temporal transition represents a shift from a winter northeast monsoon-dominated (pre-17 ka) to a summer southwest monsoon-dominated (post-17 ka) wind system.",
author = "Ali Pourmand and Franco Marcantonio and Bianchi, {Thomas S.} and Canuel, {Elizabeth A.} and Waterson, {Elizabeth J.}",
year = "2007",
month = "12",
doi = "10.1029/2007PA001502",
language = "English (US)",
volume = "22",
journal = "Paleoceanography and Paleoclimatology",
issn = "2572-4517",
publisher = "American Geophysical Union",
number = "4",

}

TY - JOUR

T1 - A 28-ka history of sea surface tempeture, primary productivity and planktonic community variability in the western Arabian Sea

AU - Pourmand, Ali

AU - Marcantonio, Franco

AU - Bianchi, Thomas S.

AU - Canuel, Elizabeth A.

AU - Waterson, Elizabeth J.

PY - 2007/12

Y1 - 2007/12

N2 - Uranium series radionuclides and organic biomarkers, which represent major groups of planktonic organisms, were measured in western Arabian Sea sediments that span the past 28 ka. Variability in the past strength of the southwest and northeast monsoons and its influence on primary productivity, sea surface temperature (SST), and planktonic community structure were investigated. The average alkenone-derived SST for the last glacial period was ∼3°C lower than that measured for the Holocene. Prior to the deglacial, the lowest SSTs coincide with the highest measured fluxes of organic biomarkers, which represent primarily a planktonic suite of diatoms, coccolithophorids, dinoflagellates, and zooplankton. We propose that intensification of winter northeast monsoon winds during the last glacial period resulted in deep convective mixing, cold SSTs and enhanced primary productivity. In contrast, postdeglacial (<17 ka) SSTs are warmer during times in which biomarker fluxes are high. Associated with this transition is a planktonic community structure change, in which the ratio of the average cumulative flux of diatom biomarkers to the cumulative flux of coccolithophorid biomarkers is twice as high during the deglacial and Holocene than the average ratio during the last glacial period. We suggest that this temporal transition represents a shift from a winter northeast monsoon-dominated (pre-17 ka) to a summer southwest monsoon-dominated (post-17 ka) wind system.

AB - Uranium series radionuclides and organic biomarkers, which represent major groups of planktonic organisms, were measured in western Arabian Sea sediments that span the past 28 ka. Variability in the past strength of the southwest and northeast monsoons and its influence on primary productivity, sea surface temperature (SST), and planktonic community structure were investigated. The average alkenone-derived SST for the last glacial period was ∼3°C lower than that measured for the Holocene. Prior to the deglacial, the lowest SSTs coincide with the highest measured fluxes of organic biomarkers, which represent primarily a planktonic suite of diatoms, coccolithophorids, dinoflagellates, and zooplankton. We propose that intensification of winter northeast monsoon winds during the last glacial period resulted in deep convective mixing, cold SSTs and enhanced primary productivity. In contrast, postdeglacial (<17 ka) SSTs are warmer during times in which biomarker fluxes are high. Associated with this transition is a planktonic community structure change, in which the ratio of the average cumulative flux of diatom biomarkers to the cumulative flux of coccolithophorid biomarkers is twice as high during the deglacial and Holocene than the average ratio during the last glacial period. We suggest that this temporal transition represents a shift from a winter northeast monsoon-dominated (pre-17 ka) to a summer southwest monsoon-dominated (post-17 ka) wind system.

UR - http://www.scopus.com/inward/record.url?scp=39749139383&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=39749139383&partnerID=8YFLogxK

U2 - 10.1029/2007PA001502

DO - 10.1029/2007PA001502

M3 - Article

AN - SCOPUS:39749139383

VL - 22

JO - Paleoceanography and Paleoclimatology

JF - Paleoceanography and Paleoclimatology

SN - 2572-4517

IS - 4

M1 - PA4208

ER -