Science report
| 
28 Oct 2022
Science report |
| 28 Oct 2022
| 28 Oct 2022
A synthesis of monsoon exploration in the Asian marginal seas
Department of Geology and Geophysics, Louisiana State University,
Baton Rouge, LA 70803, USA
Christian Betzler
Institute for Geology, German Research Fleet Coordination Center,
University of Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany
Steven C. Clemens
Department of Earth, Environmental and Planetary Sciences, Box 1846, Brown University, Providence, RI 02912-1846, USA
Beth Christensen
Department of Environmental Science, Rowan University, 201 Mullica
Hill Road, Glassboro, NJ 08028, USA
Gregor P. Eberli
CSL – Center for Carbonate Research, University of Miami, 4600 Rickenbacker Causeway, Miami, FL 33149, USA
Christian France-Lanord
Centre de Recherches Pétrographiques et Géochimiques,
Université de Nancy, CNRS UMR 7358, 54500, Vandoeuvre-lès-Nancy,
France
Stephen Gallagher
School of Geography, Earth and Atmospheric Sciences, The University of Melbourne, Victoria, 3010, Australia
Ann Holbourn
Institute of Geosciences, Christian-Albrecht University,
Olshausenstrasse 40, 24118 Kiel, Germany
Wolfgang Kuhnt
Institute of Geosciences, Christian-Albrecht University,
Olshausenstrasse 40, 24118 Kiel, Germany
Richard W. Murray
Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
Yair Rosenthal
School of Environmental and Biological Sciences, Rutgers, The State University of New Jersey, 71 Dudley Road, New Brunswick, NJ 08901-8520, USA
Ryuji Tada
Department of Earth and Planetary Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-Ku, Tokyo, 113-0033, Japan
Shiming Wan
Key Laboratory of Marine Geology and Environment, Institute of
Oceanology, Chinese Academy of Sciences, 7 Nanhai Road, Qingdao, Shandong
Province, 266071, China
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Sindia M. Sosdian, Karlos G. D. Kochhann, Anya V. Hess, Clara Bolton, Anna Joy Drury, Emily J. Judd, Wolfgang Kuhnt, Caroline H. Lear, Paul Minton, Alexandra Auderset, Sevasti Modestou, and Ann Holbourn
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2026-697, https://doi.org/10.5194/essd-2026-697, 2026
Preprint under review for ESSD
Short summary
Short summary
From 23.0 and 5.3 Million years ago (Miocene epoch), atmospheric carbon dioxide levels were similar to those projected for the future. To assess their impact on global climate, it is crucial to robustly reconst ocean temperatures using proxies, such as the magnesium-to-calcium (Mg/Ca) ratio in microfossils called foraminifera. Here we reevaluate global Miocene foraminiferal Mg/Ca records, and use revised calibrations to recalculate, assessing uncertainties, upper and deep ocean temperatures.
Montserrat Alonso-Garcia, Jesus Reolid, Francisco J. Jimenez-Espejo, Or M. Bialik, Carlos A. Alvarez Zarikian, Juan Carlos Laya, Igor Carrasquiera, Luigi Jovane, John J. G. Reijmer, Gregor P. Eberli, and Christian Betzler
Clim. Past, 20, 547–571, https://doi.org/10.5194/cp-20-547-2024, https://doi.org/10.5194/cp-20-547-2024, 2024
Short summary
Short summary
The Maldives Inner Sea (northern Indian Ocean) offers an excellent study site to explore the impact of climate and sea-level changes on carbonate platforms. The sediments from International Ocean Discovery Program (IODP) Site U1467 have been studied to determine the drivers of carbonate production in the atolls over the last 1.3 million years. Even though sea level is important, the intensity of the summer monsoon and the Indian Ocean dipole probably modulated the production at the atolls.
Fei Guo, Steven Clemens, Yuming Liu, Ting Wang, Huimin Fan, Xingxing Liu, and Youbin Sun
Clim. Past, 18, 1675–1684, https://doi.org/10.5194/cp-18-1675-2022, https://doi.org/10.5194/cp-18-1675-2022, 2022
Short summary
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Our high-resolution loess Ca/Ti record displays millennial monsoon oscillations that persist over the last 650 kyr. Wavelet results indicate the ice volume and GHG co-modulation at the 100 kyr band and GHG and local insolation forcing at the precession band for the magnitude of millennial monsoon variability of loess Ca/Ti. The inferred mechanism calls on dynamic linkages to variability in AMOC. At the precession band, combined effects of GHG and insolation lead to increased extreme rainfall.
Clara T. Bolton, Emmeline Gray, Wolfgang Kuhnt, Ann E. Holbourn, Julia Lübbers, Katharine Grant, Kazuyo Tachikawa, Gianluca Marino, Eelco J. Rohling, Anta-Clarisse Sarr, and Nils Andersen
Clim. Past, 18, 713–738, https://doi.org/10.5194/cp-18-713-2022, https://doi.org/10.5194/cp-18-713-2022, 2022
Short summary
Short summary
The timing of the initiation and evolution of the South Asian monsoon in the geological past is a subject of debate. Here, we present a new age model spanning the late Miocene (9 to 5 million years ago) and high-resolution records of past open-ocean biological productivity from the equatorial Indian Ocean that we interpret to reflect monsoon wind strength. Our data show no long-term intensification; however, strong orbital periodicities suggest insolation forcing of monsoon wind strength.
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Short summary
An integrated campaign of drilling around Asia and Australia was conducted from 2013 to 2016 to reconstruct the monsoon climate. The results provide relatively continuous records spanning the last 24 myr. Asia has shown a steady drying since the late Miocene, while Australia has become wetter. The monsoons are affected by the tectonics of Asia and surrounding seas, as well as orbital forcing, resulting in diachronous evolution of continental climate, ocean currents, and the marine biosphere.
An integrated campaign of drilling around Asia and Australia was conducted from 2013 to 2016 to...
