Contrasting Common Era climate and hydrology sensitivities from paired lake sediment dinosterol hydrogen isotope records in the South Pacific Convergence Zone
Contrasting Common Era climate and hydrology sensitivities from paired lake sediment dinosterol hydrogen isotope records in the South Pacific Convergence Zone
Hydroclimate on ‘Uvea (Wallis et Futuna) is controlled by rainfall associated with the South Pacific Convergence Zone (SPCZ), the southern hemisphere's largest precipitation feature. To extend the short observational precipitation record, the hydrogen isotopic composition of the algal lipid biomarker dinosterol (δ2Hdinosterol) was measured in sediment cores from two volcanic crater lakes on ‘Uvea. The modern lakes differ morphologically and chemically but both contain freshwater within the photic zone, support phytoplankton communities inclusive of dinosterol-producing dinoflagellates, and experience identical climate conditions. δ2Hdinosterol values track lake water isotope ratios, ultimately controlled in the tropics by precipitation amount and evaporative enrichment. However, in 88-m-deep Lac Lalolalo a steadily decreasing trend in sedimentary δ2Hdinosterol values from −227‰ around year 988 CE to modern values as low as −303‰, suggests this lake's evolution from an active volcanic setting to the present system strongly influenced δ2Hdinosterol values. Although current hydrology and water isotope systematics may now reflect precipitation and evaporation in this lake, the interaction between these
processes and large changes in basin morphology, geochemistry, and hydrology obstruct the recovery of a climate signal from Lac Lalolalo's sedimentary δ2Hdinosterol records. This work emphasizes the importance of site replication and the use of complementary climate reconstruction tools, especially when using molecular proxies
that may be sensitive to more than one environmental parameter. Contrary to its neighbor, duplicate δ2Hdinosterol records from 23-m-deep Lac Lanutavake varied between −277‰ and −297‰ and indicate slightly drier conditions during the time-period known as the Medieval Climate Anomaly (MCA, 950–1250 CE). The δ2Hdinosterol signal in Lac Lanutavake was muted compared to published records from ‘Upolu (Samoa) and Efate (Vanuatu) indicating that ‘Uvea's location is not as sensitive to precipitation variability at sites farther from the SPCZ central
axis. Lithogenic runoff proxies combined with δ2Hdinosterol support the interpretation of a relatively dry MCA on ‘Uvea, ‘Upolu, and Efate, potentially due to less intense precipitation, a contracted, or a more zonally oriented SPCZ.
Dinosterol, Holocene, Hydrogen isotopes, Lakes, Organic geochemistry, Paleohydrology, Paleolimnology, SPCZ, Sedimentology, Tropical Pacific
Maloney, Ashley
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Richey, Julie
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Nelson, Daniel
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Hing, Samantha
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Sear, David
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Hassall, Jonathan
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Langdon, Peter
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Sichrowsky, Ursula
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Schabetsberger, Robert
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Malau, Atoloto
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Meyer, Jean-Yves
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Croudace, Ian
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Sachs, Julian
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1 April 2022
Maloney, Ashley
b265f80a-f167-48f8-8334-3b9404e214f8
Richey, Julie
ce9b4e08-d14c-40eb-a43d-6fd2a4cf1d46
Nelson, Daniel
30320a3a-ba73-46f6-aecf-f6b745d9ebdf
Hing, Samantha
8f3284c3-d0d5-4126-95a2-be1a107e14d9
Sear, David
ccd892ab-a93d-4073-a11c-b8bca42ecfd3
Hassall, Jonathan
17b719cf-5b7b-496a-8bf7-96c57618baca
Langdon, Peter
95b97671-f9fe-4884-aca6-9aa3cd1a6d7f
Sichrowsky, Ursula
8647cf48-bb1d-4735-9f76-fbf8ae2d9e65
Schabetsberger, Robert
61d0f7e1-14bf-4967-ab4f-2c1c88164ae6
Malau, Atoloto
6e307afc-d663-4c9c-a3cd-2d5a9a00a288
Meyer, Jean-Yves
07f0ac2b-115f-4ab6-b922-5ace6dc80ef3
Croudace, Ian
24deb068-d096-485e-8a23-a32b7a68afaf
Sachs, Julian
18a1cbe0-492e-4c44-bb61-47109eca1e64
Maloney, Ashley, Richey, Julie, Nelson, Daniel, Hing, Samantha, Sear, David, Hassall, Jonathan, Langdon, Peter, Sichrowsky, Ursula, Schabetsberger, Robert, Malau, Atoloto, Meyer, Jean-Yves, Croudace, Ian and Sachs, Julian
(2022)
Contrasting Common Era climate and hydrology sensitivities from paired lake sediment dinosterol hydrogen isotope records in the South Pacific Convergence Zone.
Quaternary Science Reviews, 281, [107421].
(doi:10.1016/j.quascirev.2022.107421).
Abstract
Hydroclimate on ‘Uvea (Wallis et Futuna) is controlled by rainfall associated with the South Pacific Convergence Zone (SPCZ), the southern hemisphere's largest precipitation feature. To extend the short observational precipitation record, the hydrogen isotopic composition of the algal lipid biomarker dinosterol (δ2Hdinosterol) was measured in sediment cores from two volcanic crater lakes on ‘Uvea. The modern lakes differ morphologically and chemically but both contain freshwater within the photic zone, support phytoplankton communities inclusive of dinosterol-producing dinoflagellates, and experience identical climate conditions. δ2Hdinosterol values track lake water isotope ratios, ultimately controlled in the tropics by precipitation amount and evaporative enrichment. However, in 88-m-deep Lac Lalolalo a steadily decreasing trend in sedimentary δ2Hdinosterol values from −227‰ around year 988 CE to modern values as low as −303‰, suggests this lake's evolution from an active volcanic setting to the present system strongly influenced δ2Hdinosterol values. Although current hydrology and water isotope systematics may now reflect precipitation and evaporation in this lake, the interaction between these
processes and large changes in basin morphology, geochemistry, and hydrology obstruct the recovery of a climate signal from Lac Lalolalo's sedimentary δ2Hdinosterol records. This work emphasizes the importance of site replication and the use of complementary climate reconstruction tools, especially when using molecular proxies
that may be sensitive to more than one environmental parameter. Contrary to its neighbor, duplicate δ2Hdinosterol records from 23-m-deep Lac Lanutavake varied between −277‰ and −297‰ and indicate slightly drier conditions during the time-period known as the Medieval Climate Anomaly (MCA, 950–1250 CE). The δ2Hdinosterol signal in Lac Lanutavake was muted compared to published records from ‘Upolu (Samoa) and Efate (Vanuatu) indicating that ‘Uvea's location is not as sensitive to precipitation variability at sites farther from the SPCZ central
axis. Lithogenic runoff proxies combined with δ2Hdinosterol support the interpretation of a relatively dry MCA on ‘Uvea, ‘Upolu, and Efate, potentially due to less intense precipitation, a contracted, or a more zonally oriented SPCZ.
More information
Accepted/In Press date: 10 February 2022
Published date: 1 April 2022
Additional Information:
Funding Information:
This material is based upon work supported by the US National Science Foundation under Grant Nos. 0823503 and 1502417 to J.P.S. A University of Washington Program on Climate Change Fellowship, IGERT Ocean Change Fellowship [grant #NSF1068839], Princeton University Department of Geosciences Harry H. Hess postdoctoral Fellowship, and Simons Foundation Fellowship [732763] provided partial research support for A.E.M; IGERT Ocean Change mini-research awards, and a University of Washington Quaternary Research Center research award to A.E.M. The Explorers Club Exploration Fund Grant, Gilchrist Expedition Grant and Royal Geographical Society (with IBG) Monica Cole Grant assisted with Samoa travel. Lake Lanoto'o data was funded under a Natural Environment Research Council (NERC) Studentship to J.D.H. Funding for Lake Emaotul research was provided by NERC Grant NE/N006674/1. UBA 14C date was funded by a NERC SPITFIRE PhD Scholarship and sampled by Nichola Strandberg. We are grateful for permission from Wallis civic and traditional authorities. Sample collection in ‘Uvea benefitted from the assistance of K. Manufeki, S. Tauvale, C. Manry and others from Service de L'Environment, M. Fotuaika, J.-F. Poncet, P. Nicomette, S. Felomaki, P. Tauvale, C. Chauvet, and the planning assistance from C. Lique, M. Bridoux, and C. Altman. Field work in ‘Upolu, Samoa was kindly permitted by Taule'ale'ausmai Laavasa Malua, Chief Executive Officer, Niualuga Evaimalo and staff in Ministry Natural Resources and Environment; field assistance was provided by Josie Hill, Lucy, Tinifu, Solomano and Ai. Tom Bishop assisted with field work on Vanuatu. M. Wolfshorndl, T. Magee, J. Rodysill, and K. Brady assisted with splitting and scanning cores at LacCore. We thank C. Kaapu-Lyons, N. Wallsgrove, and B. Popp for analyzing Wallis water samples. T. Fonville performed the preliminary assessment of microfossils. M. Wolhowe and J. Gregerson assisted with instrument maintenance and M. Wolhowe made two new Vanuatu δ2Hdinosterol measurements. D. Xue analyzed ions and metals in Lac Lalolalo samples. Conversations with L. Thompson, S. PoChedley, R. Echols, J. Scheff, S. Rushley, D. Battisti, R. Wood, K. Thirumalai, N. Williams, W.J. D'Andrea and constructive comments from A.E. Ingalls, and P. Quay greatly improved this manuscript. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. We thank S.N. Ladd for providing careful feedback on this project and helpful edits on the manuscript. We thank Editor P. Rioual and two anonymous reviewers for their helpful and constructive comments that improved this work.
Funding Information:
This material is based upon work supported by the US National Science Foundation under Grant Nos. 0823503 and 1502417 to J.P.S. A University of Washington Program on Climate Change Fellowship, IGERT Ocean Change Fellowship [grant # NSF1068839 ], Princeton University Department of Geosciences Harry H. Hess postdoctoral Fellowship, and Simons Foundation Fellowship [ 732763 ] provided partial research support for A.E.M; IGERT Ocean Change mini-research awards, and a University of Washington Quaternary Research Center research award to A.E.M. The Explorers Club Exploration Fund Grant, Gilchrist Expedition Grant and Royal Geographical Society (with IBG) Monica Cole Grant assisted with Samoa travel. Lake Lanoto'o data was funded under a Natural Environment Research Council ( NERC ) Studentship to J.D.H. Funding for Lake Emaotul research was provided by NERC Grant NE/N006674/1 . UBA 14 C date was funded by a NERC SPITFIRE PhD Scholarship and sampled by Nichola Strandberg. We are grateful for permission from Wallis civic and traditional authorities. Sample collection in ‘Uvea benefitted from the assistance of K. Manufeki, S. Tauvale, C. Manry and others from Service de L'Environment, M. Fotuaika, J.-F. Poncet, P. Nicomette, S. Felomaki, P. Tauvale, C. Chauvet, and the planning assistance from C. Lique, M. Bridoux, and C. Altman. Field work in ‘Upolu, Samoa was kindly permitted by Taule'ale'ausmai Laavasa Malua, Chief Executive Officer, Niualuga Evaimalo and staff in Ministry Natural Resources and Environment; field assistance was provided by Josie Hill, Lucy, Tinifu, Solomano and Ai. Tom Bishop assisted with field work on Vanuatu. M. Wolfshorndl, T. Magee, J. Rodysill, and K. Brady assisted with splitting and scanning cores at LacCore. We thank C. Kaapu-Lyons, N. Wallsgrove, and B. Popp for analyzing Wallis water samples. T. Fonville performed the preliminary assessment of microfossils. M. Wolhowe and J. Gregerson assisted with instrument maintenance and M. Wolhowe made two new Vanuatu δ 2 H dinosterol measurements. D. Xue analyzed ions and metals in Lac Lalolalo samples. Conversations with L. Thompson, S. PoChedley, R. Echols, J. Scheff, S. Rushley, D. Battisti, R. Wood, K. Thirumalai, N. Williams, W.J. D'Andrea and constructive comments from A.E. Ingalls, and P. Quay greatly improved this manuscript. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government . We thank S.N. Ladd for providing careful feedback on this project and helpful edits on the manuscript. We thank Editor P. Rioual and two anonymous reviewers for their helpful and constructive comments that improved this work.
Publisher Copyright:
© 2022
Keywords:
Dinosterol, Holocene, Hydrogen isotopes, Lakes, Organic geochemistry, Paleohydrology, Paleolimnology, SPCZ, Sedimentology, Tropical Pacific
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Local EPrints ID: 455750
URI: http://eprints.soton.ac.uk/id/eprint/455750
ISSN: 0277-3791
PURE UUID: 7811ad4c-44dd-4f86-9f6f-15dab82b8239
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Date deposited: 31 Mar 2022 17:06
Last modified: 17 Mar 2024 07:10
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