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- W2019920563 abstract "Alkenone sediment data from the Nordic seas and North Atlantic are compared to those from Sikes et al. [1997] for the Southern Ocean to evaluate further U K 37 and U K 37′ as proxies to estimate cold temperatures (<10°C) and the effect of salinity and temperature in the relative abundance of 37∶4 to the total abundance of C 37 alkenones (37∶4%). U K 37 and U K 37′ are found to be equally viable as proxies, but there are significant regional differences in their cold temperature dependence. The measurement of 37∶4% in cores from the North Atlantic region can be used to identify situations when U K 37′ is not a reliable paleothermometer. Variations in salinity are probably responsible for changes in the sedimentary record of 37∶4%, and a preliminary calibration has been obtained for 37:4%= f (salinity). This new relationship should be further confirmed through field or laboratory experiments, but it paves the way to derive a molecular proxy to reconstruct paleosalinity in surface waters." @default.
- W2019920563 created "2016-06-24" @default.
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- W2019920563 date "1998-12-01" @default.
- W2019920563 modified "2023-10-14" @default.
- W2019920563 title "Interhemispheric appraisal of the value of alkenone indices as temperature and salinity proxies in high-latitude locations" @default.
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- W2019920563 doi "https://doi.org/10.1029/98pa02355" @default.
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