Diatomaceous ooze in a sedimentary core from Mariana Trench: implications for paleoceanography

Zhang, Jinpeng; Witkowski, Andrzej; Tomczak, Michał; Mccartney, Kevin; He, Gaowen; Zgłobicka, Izabela

doi:10.24425/agp.2019.126448

Artykuł - szczegóły

Tytuł artykułu

Diatomaceous ooze in a sedimentary core from Mariana Trench: implications for paleoceanography

Autorzy

Zhang Jinpeng , Witkowski Andrzej , Tomczak Michał , Mccartney Kevin , He Gaowen , Zgłobicka Izabela

Treść / Zawartość

Pełne teksty:

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Identyfikatory

DOI

10.24425/agp.2019.126448

Warianty tytułu

Języki publikacji

Abstrakty

Diatomaceous ooze sampled from near the Mariana Trench sediment surface by gravity corer (Core JL7KGC05) revealed a high sedimentary abundance of Ethmodiscus rex (Rattray, 1890) Wiseman and Hendey, 1953 fragments and tropical open ocean planktonic diatom taxa including Azpeitia nodulifera (Schmidt, 1878) Fryxell and Watkins in Fryxell, Sims and Watkins, 1986 and Alveus marinus (Grunow, 1880) Kaczmarska and Fryxell, 1996. Subsurficial sediments from the ooze are assigned a Marine Isotope Stage 2 age, approximately at the Last Glacial Maximum. The occurrence of Ethmodiscus ooze suggests massive late Pleistocene blooms in the Northwestern Pacific Ocean and provides a plausible link to paleoceanographic and paleoclimatic changes related to Antarctic Intermediate Water mass, which carried a high dissolved silica content as silicon leakage that reduced dissolution rate of diatom frustules. Northward flow of Antarctic Intermediate Water was probably related to surface current migration and southward shift of the Northwest Pacific Gyre to form oligotrophic conditions that triggered Ethmodiscus rex blooms under unusual nutrient recycling conditions within the ocean system. This bloom hypothesis may help explain differential silica dissolution during the last glacial stage.

Słowa kluczowe

diatomaceous ooze diatom Ethmodiscus rex Mariana Trench challenger deep

muł okrzemkowy okrzemki Rów Mariański Głębia Challengera

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2019

Tom

Vol. 69, no. 4

Strony

627--643

Opis fizyczny

Bibliogr. 100 poz., rys., tab.

Twórcy

autor

Zhang Jinpeng

jinpenggmgs@sina.com

Guangzhou Marine Geological Survey, China Geological Survey/Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, 188 Guanghai Rd., 510760 Guangzhou, China
Paleoceanography Unit, Faculty of Geosciences, Institute of Marine and Environmental Sciences, University of Szczecin, Mickiewicza 18, PL-70-383 Szczecin, Poland
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, CAS, Beijingdong 39, 210008 Nanjing, China

autor

Witkowski Andrzej

Paleoceanography Unit, Faculty of Geosciences, Institute of Marine and Environmental Sciences, University of Szczecin, Mickiewicza 18, PL-70-383 Szczecin, Poland

autor

Tomczak Michał

Paleoceanography Unit, Faculty of Geosciences, Institute of Marine and Environmental Sciences, University of Szczecin, Mickiewicza 18, PL-70-383 Szczecin, Poland
Polish Geological Institute – National Research Institute, Pomeranian Branch, Wieniawskiego 20, PL-71-130 Szczecin, Poland

autor

Mccartney Kevin

Department of Environmental Science and Sustainability, University of Maine at Presque Isle, Presque Isle, 04769 ME, USA

autor

He Gaowen

Guangzhou Marine Geological Survey, China Geological Survey/Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, 188 Guanghai Rd., 510760 Guangzhou, China

autor

Zgłobicka Izabela

Faculty of Mechanical Engineering, Białystok University of Technology, Wiejska 45C, PL-15-352 Białystok, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).

Typ dokumentu

Bibliografia

Identyfikator YADDA

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