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Showing 1 through 8 of 8
Northeast Pacific Uk37 Paleo-Temperatures [NOAA_NCDC_PALEO_2001-035]
This data set consists of Northeast Pacific Uk37 Paleo-Temperatures. Sediment core JT96-09 48° 54.7'N Latitude 126° 53.4'W Longitude 920 m Water depth Variable name and unit in each column from ...
Coral Sea ODP820 Alkenone Data and SST Reconstruction [NOAA_NCDC_PALEO_2006-073]
Recent chronostratigraphic evidence suggests that the central Australian Great Barrier Reef formed within the past 780 k.y. Periplatform sediments of the same age recovered from the western Coral ...
Equatorial Atlantic SST [NOAA_NCDC_PALEO_95-030]
Comparison of SST estimates for the equatorial atlantic derived from foraminferal assemblages, stable isotopes, and alkenone unsaturation ratios from core 12PC51 (0.25'N, 22 59.89'W, 3870M depth).
Equatorial Pacific ODP 806/849 mid-Pleistocene Uk37 Data and SST Reconstruction [NOAA_NCDC_PALEO_2006-014]
This data set consists of Equatorial Pacific ODP 806/849 mid-Pleistocene Uk37 Data and SST Reconstruction. UK37' and SST data from ODP 806 Site B. The samples from ODP 805 Site C used to bridge ...
Relationship of the Tetra-unsaturated C37 Alkenone to Salinity and Temperature [NOAA_NCDC_PALEO_2003-013]
Water column or sediment trap alkenone, SST, and salinity data from numerous locations around the world ocean.
Santa Barbara Basin Alkenones [NOAA_NCDC_PALEO_96-015]
Annual variations in alkenone unsaturation in laminated sediments in the Santa Barbara basin reveal increases in water temperature which can be linked directly to the observed sequence of El Nino ...
South China Sea Alkenone Deglacial SST Estimates [NOAA_NCDC_PALEO_2002-034]
This data set consists of alkenone (UK37') sea surface temperature estimates and planktonic foraminiferal (G.ruber) d18O data from the southern South China Sea. Data sets presented versus depth, ...
South-east Atlantic mid-Pleistocene Alkenone Data and SST Reconstruction [NOAA_NCDC_PALEO_2006-015]
Successful application of the alkenone palaeothermometer, the Uk37' index, relies upon the assumption that fossil alkenone synthesisers responded to growth-temperature changes in a similar manner ...
Showing 1 through 8 of 8
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Responsible NASA Official:
Dr. Stephen Wharton
Last updated: August 2016