苏拉威西海周边地区全新世植被演化及气候变化

边叶萍; 李家彪; 翦知湣; 初凤友; 褚智慧; KuhntWolfgang; 叶黎明

doi:10.3799/dqkx.2015.071

Volume 40 Issue 5

May 2015

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Article Navigation > Earth Science > 2015 > 40(5): 870-880

Bian Yeping, Li Jiabiao, Jian Zhimin, Chu Fengyou, Chu Zhihui, Kuhnt Wolfgang, Ye Liming, 2015. Vegetation and Climate Changes around Celebes Sea during Holocene. Earth Science, 40(5): 870-880. doi: 10.3799/dqkx.2015.071

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Bian Yeping, Li Jiabiao, Jian Zhimin, Chu Fengyou, Chu Zhihui, Kuhnt Wolfgang, Ye Liming, 2015. Vegetation and Climate Changes around Celebes Sea during Holocene. Earth Science, 40(5): 870-880. doi: 10.3799/dqkx.2015.071

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Vegetation and Climate Changes around Celebes Sea during Holocene

doi: 10.3799/dqkx.2015.071

1.
The Second Institute of Oceanography, Key Laboratory of Submarine Geoscience, State Oceanic Administration, Hangzhou 310012, China
2.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
3.
Institute of Geosciences, University of Kiel, Kiel 24118, Germany

Received Date: 2014-11-03
Publish Date: 2015-05-15

Abstract

Abstract

The environment and climate information during the Holocene is indispensable data for the global climate modeling and forecasting. Scenarios of regional vegetation and climate changes around the Celebes Sea during the Holocene are explored based on the alynological and oxygen isotope records of core MD98-2178 (3.6200°N, 118.7000°E; 1 984 m water depth) from the northwest Celebes Sea in this study. Sea-level changes are discussed since the marine pollen record of core MD98-2178 is considered as an indicator. The sharp decline in concentration of all pollen groups during the Early Holocene, ~10-7 ka BP, indicates a sea-level rise. All pollen groups at 7-4 ka BP suggest sustaining of a high sea-level. The marine pollen record after 4 ka BP shows a slight fall of sea-level. The significant increase in pollen percentage of the tropical montane forest during the Middle Holocene, 5-4 ka BP, suggests a much cold condition along the Celebes Sea at the time. It is suggested that precipitation along the Celebes Sea has been affected by variations of land-ocean distribution and solar activities. It is implied by fluctuation in fern spores record that precipitation was at a high level during the Early Holocene, but lowered after the Middle Holocene, which is in a similar pattern as indicated by the Indonesian stalagmite records.
- Holocene,
- Celebes Sea,
- pollen analysis,
- sea-level change,
- temperature,
- precipitation,
- climate change,
- vegetation

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