Reconstructing sea surface temperature in the South Pacific using organic proxies
Sea surface temperature (SST), at the interface between the atmosphere and the ocean, is an important element in the global climate system. Accurate estimates of past SSTs are indispensable for studying global climate and for validating the numerical models used for projections of future climate. SS...
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| Other Authors: | , |
| Format: | Doctoral or Postdoctoral Thesis |
| Language: | English |
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Universität Bremen
2012
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| Online Access: | https://media.suub.uni-bremen.de/handle/elib/429 https://nbn-resolving.org/urn:nbn:de:gbv:46-00102943-16 |
| Summary: | Sea surface temperature (SST), at the interface between the atmosphere and the ocean, is an important element in the global climate system. Accurate estimates of past SSTs are indispensable for studying global climate and for validating the numerical models used for projections of future climate. SSTs prior to the instrumentation era could be reconstructed using climatically sensitive biomarkers such as alkenones and glycerol dialkyl glycerol tetraethers (GDGTs). Herein I use marine sediments, both core-tops and long piston cores, to further examine the applicability of organic SST proxies derived from the aforementioned biomarkers, with an emphasis on the relatively under-studied subantarctic Southeast Pacific. The appraisal of these proxies is based on the correlation of the core-top proxy index values with present-day climatological SST, and the comparison of the SST records inferred from these proxies with other regional SST records. The alkenone index (UK37 and UK 37) values in the South Pacific core-tops display linear relationships with climatological World Ocean Atlas 2009 (WOA09) SST at low temperatures (1 -12°C), with equally high r2 values (>0.93). These results suggest that both alkenone indices are highly correlated to SST even at high latitudes, rendering them appropriate for reconstructing SST in the subantarctic Pacific. However, these indices yield different Pleistocene SST patterns for study sites in the subantarctic sector of the Southern Ocean. Judging from the better structural fit of UK37 SST records with other subantarctic surface proxy records, including foraminiferal 18O and SST records inferred from diatom- and foraminiferal assemblages, it appears that the UK37 index results in more plausible paleo SST records in this region, as opposed to the commonly used UK 37 index. The GDGT index (TEX86 and TEX86L) values in the subpolar and polar core-tops (with overlying SSTs of -2 to 17°C) are not highly correlated (r2 values < 0.3) to the annual mean WOA09 SST. Plotting these indices ... |
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