| Qingdao Institute of marine geology, China Geological Survey | Host |
| Citation: |
YANG Yingxue, LI Li, YU Jinyong, HE Juan, JIA Guodong. Progresses in the study of organic lipid molecules for reconstruction of paleo-sea temperature[J]. Marine Geology & Quaternary Geology, 2022, 42(6): 131-149. doi: 10.16562/j.cnki.0256-1492.2022042901
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Progresses in the study of organic lipid molecules for reconstruction of paleo-sea temperature
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Abstract
Temperature is a very sensitive and crucial factor in climate change, and an indispensable boundary condition in climate modelling. The reconstruction of paleotemperature is of great significance for understanding paleoclimate system such as the evolution of atmospheric circulation, and ocean currents strength and path, as well as for making more accurate predictions of future climate changes. Along with the development of new analytical techniques, organic temperature proxies have been highly valued as an important tool in paleoclimate research and widely applied in temperature reconstruction globally. In this paper, six organic thermometers are reviewed, i.e.
${\rm U}^{\rm K}_{37} $ -
Keywords:
- paleotemperature reconstruction /
- organic proxy /
- lipids /
- marine environment
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References
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YANG Yingxue, LI Li, YU Jinyong, HE Juan, JIA Guodong. Progresses in the study of organic lipid molecules for reconstruction of paleo-sea temperature[J]. Marine Geology & Quaternary Geology, 2022, 42(6): 131-149. doi: 10.16562/j.cnki.0256-1492.2022042901
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Figure 1.
Structures of long-chain alkenones (a) and representative chromatograms showing distribution of long-chain alkenones in cultures of E. huxleyi grown at different temperatures(b)[6,14]
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Figure 2.
Structures of iGDGTs (a) and representative chromatograms showing distribution of iGDGTs in marine sedimentary sample at different temperatures (b)[35, 42]
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Figure 3.
Structures of ladderane fatty acids (FA: fatty acid) (a) and representative chromatograms showing distribution of ladderane fatty acids in cultures of Candidatus B. fulgida grown at different temperatures(b)[65]
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Figure 4.
Structures of long-chain alkyl diols (a) and representative chromatograms showing distribution of long-chain alkyl diols in marine sedimentary sample at different temperatures (m/z 313:C281, 13-diol, C301,15-diol, m/z341:C301, 13-diol) (b)
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Figure 5.
Structures of OH-GDGTs (a) and representative chromatograms showing distribution of OH-GDGTs in marine sedimentary sample at different temperatures (b)
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Figure 6.
Structures of 3-hydroxy fatty acids (a) and representative chromatograms showing distribution of 3-hydroxy fatty acids in marine sedimentary sample at different temperatures (b)[115,120]
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Figure 7.
Comparison in annual average SST between RAN13 and
${\rm{TEX}}^{\rm H}_{86} $ inversed ones in Site B3 (a) and among the LDI in S101, and${\rm U}^{\rm K'}_{37} $ and${\rm{TEX}}^{\rm H}_{86} $ inversed ones in Site A9