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Earthquake and typhoon trigger unprecedented transient shifts in shallow hydrothermal vents biogeochemistry ArchiMer
Lebrato, Mario; Wang, Yiming V.; Tseng, Li-chun; Achterberg, Eric P.; Chen, Xue-gang; Molinero, Juan-carlos; Bremer, Karen; Westernstroeer, Ulrike; Soeding, Emanuel; Dahms, Hans-uwe; Kueter, Marie; Heinath, Verena; Joehnck, Janika; Konstantinou, Kostas I.; Yang, Yiing J.; Hwang, Jiang-shiou; Garbe-schoenberg, Dieter.
Shallow hydrothermal vents are of pivotal relevance for ocean biogeochemical cycles, including seawater dissolved heavy metals and trace elements as well as the carbonate system balance. The Kueishan Tao (KST) stratovolcano off Taiwan is associated with numerous hydrothermal vents emitting warm sulfur-rich fluids at so-called White Vents (WV) and Yellow Vent (YV) that impact the surrounding seawater masses and habitats. The morphological and biogeochemical consequences caused by a M5.8 earthquake and a C5 typhoon ("Nepartak") hitting KST (12th May, and 2nd-10th July, 2016) were studied within a 10-year time series (2009-2018) combining aerial drone imagery, technical diving, and hydrographic surveys. The catastrophic disturbances triggered landslides that...
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Ano: 2019 URL: https://archimer.ifremer.fr/doc/00593/70518/68670.pdf
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Northern and southern hemisphere controls on seasonal sea surface temperatures in the Indian Ocean during the last deglaciation ArchiMer
Wang, Yiming V.; Leduc, Guillaume; Regenberg, Marcus; Andersen, Nils; Larsen, Thomas; Blanz, Thomas; Schneider, Ralph R..
Different proxies for sea surface temperature (SST) often exhibit divergent trends for deglacial warming in tropical regions, hampering our understanding of the phase relationship between tropical SSTs and continental ice volume at glacial terminations. To reconcile divergent SST trends, we report reconstructions of two commonly used paleothermometers (the foraminifera G. ruber Mg/Ca and the alkenone unsaturation index) from a marine sediment core collected in the southwestern tropical Indian Ocean encompassing the last 37,000 years. Our results show that SSTs derived from the alkenone unsaturation index (U-37(K)) are consistently warmer than those derived from Mg/Ca by similar to 2-3 degrees C except for the Heinrich Event 1. In addition, the initial...
Tipo: Text Palavras-chave: Sea surface temperature; Tropical Indian Ocean; Last Deglacial.
Ano: 2013 URL: https://archimer.ifremer.fr/doc/00291/40174/39037.pdf
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