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渤海湾西岸全新世海面变化

DOI: 10.11928/j.issn.1001-7410.2015.02.01, PP. 243-264

Keywords: 渤海湾西岸,海面标志点,驻留时间校正,冰川均衡调整(GIA)

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Abstract:

在讨论海面标志点基本定义的基础上,从渤海湾西岸534个原始数据中获得了136个指示高水位、潮间带或低水位的海面变化标志点,并重建了它们的相对海平面时空分布,进而获得了渤海湾西岸全新世相对海平面变化带.约10cal.kaB.P.时,相对海平面变化带达到-25m,以约6m/1000a(即约6mm/a)的平均速率上升,在6cal.kaB.P.前后达到现代海面的高度;6cal.kaB.P.至今,变化带的高度介于+1m~-2m之间,未发现中全新世相对高海面.再搬运海相贝类和陆相泥炭类样品的14C年龄,分别存在约600年和660年的驻留时间.经过驻留时间校正的新海面变化年代学序列,将渤海湾相对海平面达到现代高度的时间点确定为约6cal.kaB.P.,从而与全球海面变化的对比更为准确.渤海湾盆地的长期稳定下沉和沉积自重压实的共同作用,可能抵消了冰川均衡调整(GIA)引起的中全新世数米高的相对高海面.

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