Simon Jung
University of Edinburgh
14 Papers
54 Citations
Simon Jung is an academic researcher from University of Edinburgh. The author has contributed to research in topics: Glacial period & North Atlantic Deep Water. The author has an hindex of 10, co-authored 14 publications. Previous affiliations of Simon Jung include University of Bern.
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Papers
Consistently dated Atlantic sediment cores over the last 40 thousand years
Claire Waelbroeck,Bryan C Lougheed,Natalia Vázquez Riveiros,Natalia Vázquez Riveiros,Lise Missiaen,Joel B Pedro,Trond Dokken,Irka Hajdas,Lukas Wacker,Peter M Abbott,Peter M Abbott,Jean-Pascal Dumoulin,Jean-Pascal Dumoulin,François Thil,Frédérique Eynaud,Linda Rossignol,Wiem Fersi,Ana Luiza Spadano Albuquerque,Helge W Arz,William E. N. Austin,Rosemarie E Came,Anders E. Carlson,James A Collins,Bernard Dennielou,Stéphanie Desprat,Stéphanie Desprat,Alex Dickson,Mary Elliot,Christa Farmer,Jacques Giraudeau,Julia Gottschalk,Jorijntje Henderiks,Konrad A Hughen,Simon Jung,Paul Cornils Knutz,Susana Martin Lebreiro,David C Lund,Jean Lynch-Stieglitz,Bruno Malaizé,Thomas M Marchitto,Gema Martínez-Méndez,Gesine Mollenhauer,Filipa Naughton,Silvia Osorio Nave,Dirk Nürnberg,Delia W Oppo,Victoria L Peck,Frank Peeters,Aurélie Penaud,Rodrigo Costa Portilho-Ramos,Janne Repschläger,Jenny Roberts,Carsten Rühlemann,Emilia Salgueiro,Maria Fernanda Sanchez Goñi,Maria Fernanda Sanchez Goñi,Joachim Schönfeld,Paolo Scussolini,Luke C Skinner,Charlotte Skonieczny,David Thornalley,Samuel Toucanne,David Van Rooij,Laurence Vidal,Antje H L Voelker,Mélanie Wary,Syee Weldeab,Martin Ziegler +67 more
TL;DR: This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean.
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Deep Atlantic Ocean carbon storage and the rise of 100,000-year glacial cycles
Jesse Farmer,Bärbel Hönisch,Bärbel Hönisch,L. Haynes,L. Haynes,Dick Kroon,Simon Jung,Heather L Ford,Heather L Ford,Maureen E. Raymo,Maureen E. Raymo,Maria Jaume-Seguí,Maria Jaume-Seguí,David B Bell,Steven L. Goldstein,Steven L. Goldstein,Leopoldo D. Pena,M. Yehudai,M. Yehudai,J. Kim +19 more
TL;DR: Foraminiferal trace element (B/Ca, Cd/Ca) and Nd isotope data have been used to demonstrate a close linkage between Atlantic Ocean meridional overturning circulation and deep ocean carbon storage across the mid-Pleistocene transition as discussed by the authors.
The Plio-Pleistocene development of Atlantic deep-water circulation and its influence on climate trends
TL;DR: In this paper, the authors used benthic stable isotope records from 10 sites in the Atlantic Ocean, including two new records from Walvis Ridge in the Southeast Atlantic (Sites 1264 and 1267), to review changes in Atlantic deep-water circulation in the context of Plio-Pleistocene climate.
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A two million year record of low-latitude aridity linked to continental weathering from the Maldives
Tereza Kunkelova,Simon Jung,Erica S. de Leau,Nick Odling,Alexander L. Thomas,Christian Betzler,Gregor P. Eberli,Carlos A. Alvarez-Zarikian,Montserrat Alonso-Garcia,Or M. Bialik,Clara L. Blättler,Junhua Adam Guo,Sébastien Haffen,Senay Horozal,Anna Ling Hui Mee,Mayuri Inoue,Luigi Jovane,Luca Lanci,Juan Carlos Laya,Thomas Lüdmann,Nagender N. Bejugam,Masatoshi Nakakuni,Kaoru Niino,Loren M. Petruny,Santi D. Pratiwi,John J. G. Reijmer,Jesús Reolid,Angela L. Slagle,Craig R. Sloss,Xiang Su,Peter K. Swart,James D. Wright,Zhengquan Yao,Jeremy R. Young,Sebastian Lindhorst,Stephanie Stainbank,Andres Rueggeberg,Silvia Spezzaferri,Igor Carrasqueira,Siyao Yu,Dick Kroon +40 more
TL;DR: In this paper, the authors present X-ray fluorescence (XRF) core-scanning results from International Ocean Discovery Program (IODP) Site U1467 for the past two million years, allowing full investigation of orbital periodicities.
Rapid switch in monsoon-wind induced surface hydrographic conditions of the eastern Arabian Sea during the last deglaciation
TL;DR: In this paper, changes in the composition of fossil planktic foraminiferal assemblages and sea surface temperatures (SST) in sediment core SK17, retrieved from offshore of central India, are used to decipher past changes in sea-surface hydrographic conditions linked mainly to the winter monsoon winds.
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