近2 Ma BP以来地球轨道参数周期上全球海平面变化机制

李文宝; 王汝建

doi:10.3799/dqkx.2016.063

Volume 41 Issue 5

May 2016

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Article Navigation > Earth Science > 2016 > 41(5): 742-756

Li Wenbao, Wang Rujian, 2016. Mechanism of Sea Level Change at the Earth Orbital Parameter Cycles during the Last 2 Ma BP. Earth Science, 41(5): 742-756. doi: 10.3799/dqkx.2016.063

Citation:

Li Wenbao, Wang Rujian, 2016. Mechanism of Sea Level Change at the Earth Orbital Parameter Cycles during the Last 2 Ma BP. Earth Science, 41(5): 742-756. doi: 10.3799/dqkx.2016.063

Li Wenbao, Wang Rujian, 2016. Mechanism of Sea Level Change at the Earth Orbital Parameter Cycles during the Last 2 Ma BP. Earth Science, 41(5): 742-756. doi: 10.3799/dqkx.2016.063

Citation:

Li Wenbao, Wang Rujian, 2016. Mechanism of Sea Level Change at the Earth Orbital Parameter Cycles during the Last 2 Ma BP. Earth Science, 41(5): 742-756. doi: 10.3799/dqkx.2016.063

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Mechanism of Sea Level Change at the Earth Orbital Parameter Cycles during the Last 2 Ma BP

doi: 10.3799/dqkx.2016.063

Li Wenbao^{1,2
,},
Wang Rujian^{1
,
,}

1.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 020092, China
2.
Inner Mongolia Autonomous Region Key Laboratory of Water Resources Protecting and Utilization, Inner Mongolia Agricultural University, Hohhot 010018, China

Received Date: 2016-01-11
Publish Date: 2016-05-15

Abstract

Abstract

Sea level change usually has great impact on global (or regional) ecological environment and social economy. Based on the published records of relative sea level (RSL), one new stacked RSL is reconstructed in this paper, and the correlations between the new stacked RSL and original records are analyzed. In addition, the reliability and rationality of the new stacked RSL are tested and verified respectively by Spectrum and Filtering analysis. Furthermore, the evolutionary history and correlations between the stacked RSL and atmospheric CO₂ concentration, sea surface temperature (SST) in middle-high latitudinal oceans and benthic oxygen isotope (δ¹⁸O_B) record are separately discussed in detail. The results show that: (1) the new stacked RSL has the similar change trend to the original RSL records during the last 2 Ma BP, and the correlation coefficients are all nearly 0.9. Meanwhile, the new stacked RSL also responds well to the global climate change events at the earth orbital parameter cycles; (2) The new stacked RSL and LR04-δ¹⁸O_B have high negative correlation in glacial-interglacial cycles during the last 2 Ma BP, with the correlation coefficient of about 0.81, which is much higher than those of the new stacked RSL with SST and atmospheric CO₂ concentration; (3) Based on the cross-spectral analytical results between the new stacked RSL and CO₂, SST and δ¹⁸O_B, individually, the new stacked RSL is nearly in phase with δ¹⁸O_B, and both lags SST and CO₂ at the eccentricity band, and lags SST but leads CO₂ at the obliquity band. It is concluded that the polar ice sheet volume was influenced by changes of SST and atmospheric CO₂ concentration, which might be caused by the change of solar insolation and finally influenced the sea level change at the earth orbital parameter cycles.
- sea level,
- polar ice sheet,
- correlations,
- 2 Ma BP,
- climate change

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References(91)

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Mechanism of Sea Level Change at the Earth Orbital Parameter Cycles during the Last 2 Ma BP

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