Articles | Volume 14, issue 11
https://doi.org/10.5194/cp-14-1783-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-1783-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
23 Nov 2018
Research article |
| 23 Nov 2018
| 23 Nov 2018
A Late Quaternary climate record based on long-chain diol proxies from the Chilean margin
Marijke W. de Bar
CORRESPONDING AUTHOR
Department of Marine Microbiology and Biogeochemistry, NIOZ Royal
Netherlands Institute for Sea Research, and Utrecht University, Den Burg,
Texel, 1790 AB, the Netherlands
Dave J. Stolwijk
Department of Marine Microbiology and Biogeochemistry, NIOZ Royal
Netherlands Institute for Sea Research, and Utrecht University, Den Burg,
Texel, 1790 AB, the Netherlands
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, 3584 CB, the Netherlands
Jerry F. McManus
Lamont-Doherty Earth Observatory, Columbia University, New York
10964, USA
Jaap S. Sinninghe Damsté
Department of Marine Microbiology and Biogeochemistry, NIOZ Royal
Netherlands Institute for Sea Research, and Utrecht University, Den Burg,
Texel, 1790 AB, the Netherlands
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, 3584 CB, the Netherlands
Stefan Schouten
Department of Marine Microbiology and Biogeochemistry, NIOZ Royal
Netherlands Institute for Sea Research, and Utrecht University, Den Burg,
Texel, 1790 AB, the Netherlands
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, 3584 CB, the Netherlands
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Cited
24 citations as recorded by crossref.
- Long chain diol index (LDI) as a potential measure to estimate annual mean sea surface temperature in the northern South China Sea X. Zhu et al. 10.1016/j.ecss.2019.03.012
- Long chain 1,14-diols as potential indicators for upper water stratification in the open South China Sea X. Zhu et al. 10.1016/j.ecolind.2019.105900
- The Sediment Green‐Blue Color Ratio as a Proxy for Biogenic Silica Productivity Along the Chilean Margin C. Li et al. 10.1029/2022GC010350
- Mediterranean-like “fall dump” events in the Baltic Sea J. Kaiser et al. 10.1177/09596836231219479
- A multiproxy study of past environmental changes in the Sea of Okhotsk during the last 1.5 Ma J. Lattaud et al. 10.1016/j.orggeochem.2019.04.003
- Glacial–interglacial seawater isotope change near the Chilean Margin as reflected by δ2H values of C37 alkenones K. Hättig et al. 10.5194/cp-19-1919-2023
- Detection of new long-chain mid-chain keto-ol isomers from marine sediments by means of HPLC–APCI-MS and comparison with long-chain mid-chain diols from the same samples G. Versteegh & J. Lipp 10.1016/j.orggeochem.2019.04.004
- The Novel Hydroxylated Tetraether Index RI‐OH′ as a Sea Surface Temperature Proxy for the 160‐45 ka BP Period Off the Iberian Margin N. Davtian et al. 10.1029/2020PA004077
- A marine record of Patagonian ice sheet changes over the past 140,000 years J. Hagemann et al. 10.1073/pnas.2302983121
- A new age model for the Pliocene of the southern North Sea basin: a multi-proxy climate reconstruction E. Dearing Crampton-Flood et al. 10.5194/cp-16-523-2020
- Paleosensitivity of Hydrogen Isotope Ratios of Long‐Chain Alkenones to Salinity Changes at the Chile Margin G. Weiss et al. 10.1029/2019PA003591
- Alkenone δ2H values – a viable seawater isotope proxy? New core-top δ2HC37:3 and δ2HC37:2 data suggest inter-alkenone and alkenone-water hydrogen isotope fractionation are independent of temperature and salinity B. Mitsunaga et al. 10.1016/j.gca.2022.10.024
- Constraining Water Depth Influence on Organic Paleotemperature Proxies Using Sedimentary Archives D. Varma et al. 10.1029/2022PA004533
- Evaluation of environmental proxies based on long chain alkyl diols in the East China Sea L. He et al. 10.1016/j.orggeochem.2019.103948
- Assessment of the nutrient diol index (NDI) as a sea surface nutrient proxy using sinking particles in the East Sea J. Gal et al. 10.1016/j.marchem.2021.103937
- Long-chain alkyl diols as indicators of local riverine input, temperature, and upwelling in a shelf south of the Yangtze River Estuary in the East China Sea L. Chen et al. 10.1016/j.margeo.2021.106573
- Applicability of the Long Chain Diol Index (LDI) as a Sea Surface Temperature Proxy in the Arabian Sea Z. Erdem et al. 10.1029/2021PA004255
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Constraining the applicability of organic paleotemperature proxies for the last 90 Myrs M. de Bar et al. 10.1016/j.orggeochem.2018.12.005
- Global temperature calibration of the Long chain Diol Index in marine surface sediments M. de Bar et al. 10.1016/j.orggeochem.2020.103983
- Southern Ocean temperature records and ice-sheet models demonstrate rapid Antarctic ice sheet retreat under low atmospheric CO2 during Marine Isotope Stage 31 C. Beltran et al. 10.1016/j.quascirev.2019.106069
- Assessing the applicability of the long-chain diol (LDI) temperature proxy in the high-temperature South China Sea Y. Yang et al. 10.1016/j.orggeochem.2020.104017
- The last two glacial cycles in central Patagonia: A precise record from the Ñirehuao glacier lobe C. Peltier et al. 10.1016/j.quascirev.2022.107873
- A Late Quaternary climate record based on long-chain diol proxies from the Chilean margin M. de Bar et al. 10.5194/cp-14-1783-2018
23 citations as recorded by crossref.
- Long chain diol index (LDI) as a potential measure to estimate annual mean sea surface temperature in the northern South China Sea X. Zhu et al. 10.1016/j.ecss.2019.03.012
- Long chain 1,14-diols as potential indicators for upper water stratification in the open South China Sea X. Zhu et al. 10.1016/j.ecolind.2019.105900
- The Sediment Green‐Blue Color Ratio as a Proxy for Biogenic Silica Productivity Along the Chilean Margin C. Li et al. 10.1029/2022GC010350
- Mediterranean-like “fall dump” events in the Baltic Sea J. Kaiser et al. 10.1177/09596836231219479
- A multiproxy study of past environmental changes in the Sea of Okhotsk during the last 1.5 Ma J. Lattaud et al. 10.1016/j.orggeochem.2019.04.003
- Glacial–interglacial seawater isotope change near the Chilean Margin as reflected by δ2H values of C37 alkenones K. Hättig et al. 10.5194/cp-19-1919-2023
- Detection of new long-chain mid-chain keto-ol isomers from marine sediments by means of HPLC–APCI-MS and comparison with long-chain mid-chain diols from the same samples G. Versteegh & J. Lipp 10.1016/j.orggeochem.2019.04.004
- The Novel Hydroxylated Tetraether Index RI‐OH′ as a Sea Surface Temperature Proxy for the 160‐45 ka BP Period Off the Iberian Margin N. Davtian et al. 10.1029/2020PA004077
- A marine record of Patagonian ice sheet changes over the past 140,000 years J. Hagemann et al. 10.1073/pnas.2302983121
- A new age model for the Pliocene of the southern North Sea basin: a multi-proxy climate reconstruction E. Dearing Crampton-Flood et al. 10.5194/cp-16-523-2020
- Paleosensitivity of Hydrogen Isotope Ratios of Long‐Chain Alkenones to Salinity Changes at the Chile Margin G. Weiss et al. 10.1029/2019PA003591
- Alkenone δ2H values – a viable seawater isotope proxy? New core-top δ2HC37:3 and δ2HC37:2 data suggest inter-alkenone and alkenone-water hydrogen isotope fractionation are independent of temperature and salinity B. Mitsunaga et al. 10.1016/j.gca.2022.10.024
- Constraining Water Depth Influence on Organic Paleotemperature Proxies Using Sedimentary Archives D. Varma et al. 10.1029/2022PA004533
- Evaluation of environmental proxies based on long chain alkyl diols in the East China Sea L. He et al. 10.1016/j.orggeochem.2019.103948
- Assessment of the nutrient diol index (NDI) as a sea surface nutrient proxy using sinking particles in the East Sea J. Gal et al. 10.1016/j.marchem.2021.103937
- Long-chain alkyl diols as indicators of local riverine input, temperature, and upwelling in a shelf south of the Yangtze River Estuary in the East China Sea L. Chen et al. 10.1016/j.margeo.2021.106573
- Applicability of the Long Chain Diol Index (LDI) as a Sea Surface Temperature Proxy in the Arabian Sea Z. Erdem et al. 10.1029/2021PA004255
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Constraining the applicability of organic paleotemperature proxies for the last 90 Myrs M. de Bar et al. 10.1016/j.orggeochem.2018.12.005
- Global temperature calibration of the Long chain Diol Index in marine surface sediments M. de Bar et al. 10.1016/j.orggeochem.2020.103983
- Southern Ocean temperature records and ice-sheet models demonstrate rapid Antarctic ice sheet retreat under low atmospheric CO2 during Marine Isotope Stage 31 C. Beltran et al. 10.1016/j.quascirev.2019.106069
- Assessing the applicability of the long-chain diol (LDI) temperature proxy in the high-temperature South China Sea Y. Yang et al. 10.1016/j.orggeochem.2020.104017
- The last two glacial cycles in central Patagonia: A precise record from the Ñirehuao glacier lobe C. Peltier et al. 10.1016/j.quascirev.2022.107873
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
We present a past sea surface temperature and paleoproductivity record over the last 150 000 years for ODP Site 1234 (Chilean margin). We tested the applicability of long-chain diol proxies for the reconstrucion of SST (LDI), past upwelling conditions (diol index), and nutrient concentrations (NDI). The LDI likely reflects past temperature changes, but the diol index and NDI are perhaps more indicative of Proboscia diatom productivity rather than upwelling and/or nutrient conditions.
We present a past sea surface temperature and paleoproductivity record over the last 150 000...
