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• W1970119398 endingPage "151" @default.
• W1970119398 startingPage "121" @default.
• W1970119398 abstract "Over the last 30 years the emphasis in studies of the recovery from low last glaciation sea levels has changed significantly. The search for a eustatic sea level curve having global relevance has ended. Studies into the rheology of the earth's crust, and recognition that the geoid has not remained stable over time, have resulted in the recognition that there must have been regional differences in eustatic response to deglaciation. As a part of this re-appraisal there has been a growing appreciation that crustal isostatic response to the removal of the weight of ice sheets has been accompanied by a consequential hydro-isostatic response, particularly in the areas of the shelf seas. In the later part of the post-war period attention has additionally been focussed on the much greater potential for error over the whole field of palaeoenvironmental reconstruction in the Holocene, including not only errors in dating, but also a large number of possible sources of errors in heighting. As a result of this, an increasing number of scientists are withholding judgement on the nature of sea level rise and, more particularly, on the problem of higher than present late Holocene eustatic sea levels. The problems outstanding in the early 1960s have not yet been resolved but the bases of uncertainty have changed." @default.
• W1970119398 created "2016-06-24" @default.
• W1970119398 creator A5069784105 @default.
• W1970119398 date "1982-01-01" @default.
• W1970119398 modified "2023-10-05" @default.
• W1970119398 title "Sea level changes in the holocene" @default.
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• W1970119398 doi "https://doi.org/10.1016/0277-3791(82)90002-6" @default.

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