This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1016/B978-0-323-99931-1.00096-9. This is version 4 of this Preprint.
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Abstract
The molecular remainders of living organisms, found in sedimentary records, reflect past ecological, environmental and climatic conditions. Occurrence, abundance, relative distribution and even isotopic composition of these lipid biomarkers can be linked to climatic conditions. This chapter reviews organic proxies for past temperature, salinity, hydrology, sea ice conditions and biomass burning.
DOI
https://doi.org/10.31223/X54D5P
Subjects
Physical Sciences and Mathematics
Keywords
lipid biomarkers, Long Chain Alkenones, Leaf waxes, IP25, Glycerol dialkyl glycerol tetraethers, TEX86, MBT, paleosalinity, Paleotemperature, paleofire, paleohydrology, past sea ice, hydrogen isotopes
Dates
Published: 2023-08-24 08:47
Last Updated: 2024-10-25 15:30
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License
CC-By Attribution-NonCommercial-NoDerivatives 4.0 International
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Data Availability (Reason not available):
This is a review, no data are published
Comment #112 Rienk H. Smittenberg @ 2023-08-24 21:35
Box 1, second equation is wrong: %GDGT-0 = [GDGT-0] /([Crenarchaeol ] + [GDGT-0)])