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PALEOCEANOGRAPHY

Cariaco Basin Foraminiferal Mg/Ca and SST Reconstruction

Map of data site

Lea, D.W., D.K. Pak, L.C. Peterson, and K.A. Hughen. 2003. Synchroneity of tropical and high-latitude Atlantic temperatures over the last glacial termination. Science 301(5638):1361-1364.

Data Coverage North: 10.7 * South: 10.7
West: -65.95 * East: -65.95
Altitude: -790 m

Start Year: 20648 14C yr BP * End Year: 305 14C yr BP

Data:     Please Cite Data Contributors!
  pl07-39p-tab.txt
 SynTraCE(development): pl07-39p-sytr-tab.txt
  lea2003

Summary:

A high-resolution western tropical Atlantic sea surface temperature (SST) record from the Cariaco Basin on the northern Venezuelan shelf, based on Mg/Ca values in surface-dwelling planktonic foraminifera, reveals that changes in SST over the last glacial termination are synchronous, within ±30 to ±90 years, with the Greenland Ice Sheet Project 2 air temperature proxy record and atmospheric methane record. The most prominent deglacial event in the Cariaco record occurred during the Younger Dryas time interval, when SSTs dropped by 3° to 4°C. A rapid southward shift in the atmospheric intertropical convergence zone could account for the synchroneity of tropical temperature, atmospheric methane, and high-latitude changes during the Younger Dryas.
More Info on Paleoceanography Data

Parameters:

Sea surface temperature from Mg/Ca; calendar years before 1950AD; Magnesium/Calcium ratio; Sea Surface Temperature (C)

Complete XML Record:

noaa-ocean-2585  (Last Revised: 2009-08-21 )

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