Changes in surface water masses in the northern East China Sea since the Last Glacial Maximum based on diatom assemblages
Abstract We investigated diatom assemblages for the last 19 ka in a piston core KY07-04 PC01 collected from the northern Okinawa Trough, East China Sea. Most of the diatom taxa in the Core KY07-04 PC01 were subtropical to temperate marine species throughout the core. Pronounced turnover of major dia...
Main Authors: | Keiko Shirota, Yusuke Okazaki, Susumu Konno, Yosuke Miyairi, Yusuke Yokoyama, Yoshimi Kubota |
---|---|
Format: | Article |
Language: | English |
Published: |
SpringerOpen
2021-11-01
|
Series: | Progress in Earth and Planetary Science |
Subjects: | |
Online Access: | https://doi.org/10.1186/s40645-021-00456-1 |
Similar Items
-
The Last Glacial Maximum and deglaciation in central Patagonia, 44°S–49°S
by: M. Mendelova, et al.
Published: (2017-09-01) -
Mineralogical Record for Stepwise Hydroclimatic Changes in Lake Qinghai Sediments Since the Last Glacial Period
by: Yougui Song, et al.
Published: (2020-10-01) -
Desertification and Related Climate Change in the Alashan Plateau since the Last 40 ka of the Last Glacial Period
by: Bingqi Zhu, et al.
Published: (2023-02-01) -
Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
by: Rosa M. Carrasco, et al.
Published: (2020-12-01) -
Detrital input, productivity fluctuations, and water mass circulation in the westernmost Mediterranean Sea since the Last Glacial Maximum
by: F. J. Jimenez‐Espejo, et al.
Published: (2008-11-01)