Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

McClymont, Erin L; Rosell-Melé, V; Giraudeau, Jaques; Pierre, Catherine; Lloyd, Jerry M (2005): Sea surface temperature reconstruction of ODP Site 175-1087. PANGAEA, https://doi.org/10.1594/PANGAEA.738377, Supplement to: McClymont, EL et al. (2005): Alkenone and coccolith records of the mid-Pleistocene in the south-east Atlantic: implications for the Uk37' index and South African climate. Quaternary Science Reviews, 24(14-15), 1559-1572, https://doi.org/10.1016/j.quascirev.2004.06.024

Always quote above citation when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
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 delta18O 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.
Project(s):
Coverage:
Latitude: -31.465083 * Longitude: 15.310889
Date/Time Start: 1997-10-03T00:00:00 * Date/Time End: 1997-10-03T00:00:00
Event(s):
175-1087 * Latitude: -31.465083 * Longitude: 15.310889 * Date/Time: 1997-10-03T00:00:00 * Elevation: -1371.6 m * Penetration: 1020.9 m * Recovery: 936.4 m * Location: Benguela Current, South Atlantic Ocean * Campaign: Leg175 * Basis: Joides Resolution * Device: Composite Core (COMPCORE) * Comment: 102 cores; 948.4 m cored; 72.5 m drilled; 98.7% recovery
Size:
2 datasets

Download Data

Download ZIP file containing all datasets as tab-delimited text (use the following character encoding: )