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对较年青的碳酸盐的研究日益三维化。大西洋全新世礁厚度和生长速率方面积累的资料,促进了把生物群落接续和礁的形态与波浪作用的变异和海平面的变化之间联系起来的综合研究。就大堡礁来说,在大约6000到4000年前生长最为迅速,而在集群前期和当礁达到稳定的海平面及其以后,生长速度则较慢。 在做过很多研究的佛罗里达海湾,几个岛屿的全新世岩心说明,海侵或海退沉积作用与海平面的涨落没有必然的联系,但与堆积作用的速率变化有关。在
The research on younger carbonates has been increasingly three-dimensional. The accumulated data on the thickness and growth rate of the entire New Atlantic at the Atlantic Ocean have led to a comprehensive study linking the succession of biota and reef morphology with the variation of wave effects and sea-level changes. In the case of the Great Barrier Reef, it grew most rapidly about 6,000 to 4,000 years ago, and grew more slowly after the beginning of the cluster and when the sea reached a stable sea level. In the Gulf of Florida, where many studies have been conducted, the Holocene cores of several islands show that the transgressive or regressive sedimentation does not necessarily correlate with sea level fluctuations, but is related to the rate of accumulation. in