South-east Atlantic mid-Pleistocene Alkenone Data and SST Reconstruction McClymont, E.L.; Rosell-Melé, A.; Giraudeau, J.; Pierre, C.; Lloyd, J.M. McClymont, E.L. Rosell-Melé, A. Giraudeau, J. Pierre, C. Lloyd, J.M. Sea Surface Temperature Reconstruction earth science/paleoclimate/paleoceanography (age,null,null,radiocarbon year before present,null,paleoceanography,null,null,N,null) earth science/paleoclimate/climate reconstructions|paleoceanography (sea surface temperature,alkenone unsaturation index,null,degree Celsius,null,climate reconstructions|paleoceanography,null,null,N,null) earth science/paleoclimate/paleoceanography (alkenone unsaturation index Uk37 prime,null,null,dimensionless,null,paleoceanography,null,null,N,null) earth science/paleoclimate/paleoceanography (depth,null,null,centimeter,null,paleoceanography,null,null,N,null) earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean (2006-015>LATITUDE -31.47>LONGITUDE 15.32) Successful application of the alkenone palaeothermometer, the Uk'37 index, relies upon the assumption that fossil alkenone synthesisers responded to growth-temperature changes in a similar manner to the modern producers, chiefly the coccolithophores Emiliania huxleyi and Gephyrocapsa oceanica. We compare coccolith and Uk'37 data from ODP Site 1087 in the south-east Atlantic between 1500 and 500 ka, and show that evolutionary events and changes in species dominance within the coccolithophore populations had little impact on the Uk'37 record. The relative abundances of the C37 and C38 alkenones also closely resembled those found in modern populations, and suggest a similar temperature sensitivity of Uk'37 during the early and mid-Pleistocene to that found at present. These results support the application of the Uk'37 index to reconstruct sea-surface temperatures (SSTs) throughout the Quaternary. The Uk'37 record at ODP Site 1087 contains an SST signal that documents the emergence of the 100-kyr cycles that characterise the late Quaternary ice volume records. This is preceded by significant cooling at ODP Site 1087, marked by a negative shift in SSTs and a positive shift in the planktonic d18O some 250-kyr earlier, at ca 1150-1000 ka. This results in a permanent fall in average SSTs of around 1.5 °C. The predicted increase in aridity onshore as a result of this cooling can be identified in a number of published records from southern Africa, and may have played a role in some important evolutionary events of the mid-Pleistocene. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : McClymont, E.L. Investigator : Rosell-Melé, A. Investigator : Giraudeau, J. Investigator : Pierre, C. Investigator : Lloyd, J.M. 2005-07-01 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/2644 https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/odp1087a-tab.txt https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/mcclymont2005b https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/odp1087a-tab.txt https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/mcclymont2005b English https://www.ncdc.noaa.gov/paleo/study/2644 https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/odp1087a-tab.txt https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/mcclymont2005b McClymont, E.L., A. Rosell-Melé, J. Giraudeau, C. Pierre, and J.M. Lloyd. 2005. Alkenone and coccolith records of the mid-Pleistocene in the south-east Atlantic: Implications for the index and South African climate. Quaternary Science Reviews 24, 1559-1572. START YEAR: 1517112 14C yr BP * END YEAR: 497630 14C yr BP 15.32 -31.47 15.32 -31.47