A diatom record of mid- to late Holocene palaeoenvironmental changes in the southern Okinawa Trough

Author:

LI DONGLING1,JIANG HUI2,KNUDSEN KAREN LUISE3,BJÖRCK SVANTE4,OLSEN JESPER5,ZHAO MEIXUN6,LI TIEGANG7,LI JIALIN1

Affiliation:

1. Department of City Science; Ningbo University; Ningbo China

2. Key Laboratory of Geographic Information Science; East China Normal University; Shanghai China

3. Department of Geoscience; Aarhus University; Aarhus Denmark

4. Department of Geology; Lund University; Lund Sweden

5. Department of Physics and Astronomy; AMS C Dating Centre, Aarhus University; Aarhus Denmark

6. Key Laboratory of Marine Chemistry Theory and Technology of the Ministry of Education; Ocean University of China; Qingdao China

7. Key Laboratory of Marine Geology and Environment; Institute of Oceanology, Chinese Academy of Sciences; Qingdao China

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Reference115 articles.

1. Discharge of the Changjiang (Yangtze River) into the East China Sea;Beardsley;Continental Shelf Research,1985

2. Insolation values for the climate of the last 10 million years;Berger;Quaternary Science Reviews,1991

3. Sediment properties and water characteristics of the Taiwan shelf and slope;Boggs;Acta Oceanographica Taiwanica,1979

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