Holocene Relative Sea-Level History of Novaya Zemlya, Russia, and Implications for Late Weichselian Ice-Sheet Loading
Abstract We present six new radiocarbon-dated emergence curves that provide a detailed record of postglacial emergence of northern Novaya Zemlya and ages which constrain the emergence of Vaygach Island in the southern archipelago. Radiocarbon ages on Hiatella sp. from a lateral moraine in Russkaya G...
| Published in: | Quaternary Research |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
2001
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1006/qres.2001.2256 http://api.elsevier.com/content/article/PII:S0033589401922562?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589401922562?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400010267 |
| Summary: | Abstract We present six new radiocarbon-dated emergence curves that provide a detailed record of postglacial emergence of northern Novaya Zemlya and ages which constrain the emergence of Vaygach Island in the southern archipelago. Radiocarbon ages on Hiatella sp. from a lateral moraine in Russkaya Gavan' and abundances of foraminifea in a marine core from Nordenskiold Bay, 300 km south of our study area, indicate that coastal deglaciation occurred prior to ∼10,000 cal yr B.P. However, postglacial emergence commenced ∼7000 cal yr B.P., with stabilization of global sea level. The total emergence is 13–11 m above sea level (asl) with apparent uplift rates of 1–2 mm/yr for the past 2000 yr, indicating modest glacier loads (<1 km), early (>11,000 cal yr B.P.) deglaciation, or both. The isobase pattern, showing no east–west tilt across Novaya Zemlya, and offshore moraines suggest a separate ice-dispersal center over Novaya Zemlya for the later stages of the Late Weichselian glacial cycle and possibly earlier. |
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