Pleistocene raised marine deposits on Wrangel Island, northeast Siberia and implications for the presence of an East Siberian ice sheet
العنوان: | Pleistocene raised marine deposits on Wrangel Island, northeast Siberia and implications for the presence of an East Siberian ice sheet |
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المؤلفون: | Sergey L. Vartanyan, Julie Brigham-Grette, Patricia M. Anderson, Lyn Gualtieri |
المصدر: | Quaternary Research. 59:399-410 |
بيانات النشر: | Cambridge University Press (CUP), 2003. |
سنة النشر: | 2003 |
مصطلحات موضوعية: | geography, geography.geographical_feature_category, Pleistocene, Last Glacial Maximum, law.invention, Oceanography, Arts and Humanities (miscellaneous), law, Geochronology, General Earth and Planetary Sciences, Glacial period, Radiocarbon dating, Ice sheet, Geology, Sea level, Earth-Surface Processes, Marine transgression |
الوصف: | Two previously undocumented Pleistocene marine transgressions on Wrangel Island, northeastern Siberia, question the presence of an East Siberian or Beringian ice sheet during the last glacial maximum (LGM). The Tundrovayan Transgression (459,000–780,000 yr B.P.) is represented by raised marine deposits and landforms 15–41 m asl located up to 18 km inland. The presence of high sea level 64,000–73,000 yr ago (the Krasny Flagian Transgression) is preserved in deposits and landforms 4–7 m asl in the Krasny Flag valley. These deposits and landforms were mapped, dated, and described using amino acid geochronology, radiocarbon, optically stimulated luminescence, electron spin resonance, oxygen isotopes, micropaleontology, paleomagnetism, and grain sizes. The marine deposits are eustatic and not isostatic in origin. All marine deposits on Wrangel Island predate the LGM, indicating that neither Wrangel Island nor the East Siberian or Chukchi Seas experienced extensive glaciation over the last 64,000 yr. |
تدمد: | 1096-0287 0033-5894 |
DOI: | 10.1016/s0033-5894(03)00057-7 |
URL الوصول: | https://explore.openaire.eu/search/publication?articleId=doi_________::5a7b5f0713b4800bdb41a32bf9762b7a https://doi.org/10.1016/s0033-5894(03)00057-7 |
Rights: | CLOSED |
رقم الانضمام: | edsair.doi...........5a7b5f0713b4800bdb41a32bf9762b7a |
قاعدة البيانات: | OpenAIRE |
تدمد: | 10960287 00335894 |
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DOI: | 10.1016/s0033-5894(03)00057-7 |