Reappraisal of sea-level lowstand during the Last Glacial Maximum observed in the Bonaparte Gulf sediments, northwestern Australia

Quaternary International

Volumn 397, Issue , 2016, Pages 373-379

  Ishiwa, Takeshige ^a   Yokoyama, Yusuke ^a   Miyairi, Yosuke ^a   Obrochta, Stephen ^a,b   Sasaki, Takenori ^a   Kitamura, Akihisa ^c   Suzuki, Atsushi ^d   Ikehara, Minoru ^e   Ikehara, Ken ^d   Kimoto, Katsunori ^f   Bourget, Julien ^g   Matsuzaki, Hiroyuki ^a  

^a UNIVERSITY OF TOKYO   (Japan)

^b AKITA UNIVERSITY   (Japan)

^c SHIZUOKA UNIVERSITY   (Japan)

^d NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

^e KOCHI UNIVERSITY   (Japan)

^f JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^g UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

Author keywords

Bonaparte Gulf; Far field; Last Glacial Maximum; Radiocarbon dating; Sea level change

Indexed keywords

ISOSTASY; LAST GLACIAL MAXIMUM; MARINE SEDIMENT; PALEOENVIRONMENT; RADIOCARBON DATING; SEA LEVEL CHANGE; SEDIMENT CORE; UPLIFT;

AUSTRALIA; BONAPARTE BASIN; INDIAN OCEAN; TIMOR SEA;

MOLLUSCA;

EID: 84927721162     PISSN: 10406182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quaint.2015.03.032     Document Type: Article

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