Saved in:
| Main Authors: | , , , , , |
|---|---|
| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
2000
|
| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.855339 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| _version_ | 1867169512567078912 |
|---|---|
| author | Kim, Jung-Moo Kennett, James P Park, Byong-Kwon Kim, Dae-Choul Kim, Gil Young Roark, E Brendan |
| author_facet | Kim, Jung-Moo Kennett, James P Park, Byong-Kwon Kim, Dae-Choul Kim, Gil Young Roark, E Brendan |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Foraminiferal assemblage and stable isotopic data are presented for three Quaternary piston cores from Ulleung Basin, East Sea of Korea ((ESK) Japan Sea) near the Korean Peninsula. Major changes in both temperature and salinity strongly affected surface and deep waters of the ESK during the transition from the Last Glacial Maximum (LGM) to the middle Holocene. Local environmental effects dominated during the LGM and the Bølling/Allerød (B/A) when the ESK became semi-isolated from the Pacific Ocean. Regional/global influences dominated following the B/A, after sufficient reconnection with the Pacific. This is reflected in the foraminiferal d18O record which was largely salinity-controlled before the Younger Dryas (YD) and temperature-controlled after the YD. Paleoceanographic changes in the ESK during the last deglaciation reflect sequential reconnection with the Pacific Ocean, through gateways, first (B/A) in the north (Tsugaru Strait) and later (Holocene) in the south (Korea Strait). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_855339 |
| institution | PANGAEA |
| language | en |
| publishDate | 2000 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Planktonic foraminifera and stable isotopic record of sediments from the east Sea of Korea Kim, Jung-Moo Kennett, James P Park, Byong-Kwon Kim, Dae-Choul Kim, Gil Young Roark, E Brendan Foraminiferal assemblage and stable isotopic data are presented for three Quaternary piston cores from Ulleung Basin, East Sea of Korea ((ESK) Japan Sea) near the Korean Peninsula. Major changes in both temperature and salinity strongly affected surface and deep waters of the ESK during the transition from the Last Glacial Maximum (LGM) to the middle Holocene. Local environmental effects dominated during the LGM and the Bølling/Allerød (B/A) when the ESK became semi-isolated from the Pacific Ocean. Regional/global influences dominated following the B/A, after sufficient reconnection with the Pacific. This is reflected in the foraminiferal d18O record which was largely salinity-controlled before the Younger Dryas (YD) and temperature-controlled after the YD. Paleoceanographic changes in the ESK during the last deglaciation reflect sequential reconnection with the Pacific Ocean, through gateways, first (B/A) in the north (Tsugaru Strait) and later (Holocene) in the south (Korea Strait). |
| title | Planktonic foraminifera and stable isotopic record of sediments from the east Sea of Korea |
| topic | |
| url | https://doi.org/10.1594/PANGAEA.855339 |