Titlebook: Sea-level research: a manual for the collection and evaluation of data; A manual for the col Orson Plassche Book 1986 Orson van de plassche

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Analysis of botanical macro-remainsn the perimarine area of the hinterland. In each case, however, interpretation has to be done very carefully to separate the real changes of sea level from other possible factors such as rate of sedimentation, compaction, influence from the hinterland, and the inflow of fresh water from the rivers.

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Foraminifera as sea-level indicatorsrcumstances, some information concerning sea level can be derived from other foraminiferal assemblages using indirect means. For instance areas which have undergone substantial emergence often contain small basins which, prior to emergence, were marine. The marine sediments at the bottom can be iden

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Diatoms as indicators of sea-level changenations of these. Where an older marine diatom assemblage is replaced by a younger fresh-water assemblage, a marine regression is usually inferred. Similarly, if a fresh-water assemblage is replaced by younger marine diatoms, a transgression is often the cause. The analyst cannot make interpretation

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Book 1986ast, mainly since the end of the last glaciation. Its major objective is to help answer the ques­ tion: "how?", which, of course, is little else but to assist in the gathering of fuel for the burning question: "why?" Good fuel, hopefully, for the less smoke and ashes, and the more heat and light pro

STING

s in the past, mainly since the end of the last glaciation. Its major objective is to help answer the ques­ tion: "how?", which, of course, is little else but to assist in the gathering of fuel for the burning question: "why?" Good fuel, hopefully, for the less smoke and ashes, and the more heat and light pro978-94-010-8370-6978-94-009-4215-8

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Sea-level research: a manual for the collection and evaluation of dataA manual for the col

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Sea-level research: a manual for the collection and evaluation of data978-94-009-4215-8