Basin-wide sedimentation changes and deglacial lake-level rise in the Hovsgol basin, NW Mongolia
Tài liệu tham khảo
1989, 118
Dorofeyuk, 1998, Vegetation and lake levels in northern Mongolia during the past 12,500 years, according to palynological and diatom analyses, Stratigraphy and Geological Correlation, 6, 73
Fedotov, 2001, Sediments of Lake Hovsgol as a record of paleoclimates of the Holocene and late Pleistocene, Russian Geology and Geophysics, 42, 384
Fedotov, 2004, Changes in the volume and salinity of Lake Khubsugul (Mongolia) in response to global climate changes in the upper Pleistocene and the Holocene, Palaeogeography, Palaeoclimatology, Palaeoecology, 209, 245, 10.1016/j.palaeo.2003.12.022
Grunert, 2000, Paleoclimatic evolution of the Uvs Nuur Basin and adjacent areas (Western Mongolia), Quaternary International, 65/66, 171, 10.1016/S1040-6182(99)00043-9
Karabanov, 2004, Ecological collapse of Lake Baikal and Lake Hovsgol ecosystems during the last glacial and consequences for aquatic species diversity, Palaeogeography, Palaeoclimatology, Palaeoecology, 209, 227, 10.1016/j.palaeo.2004.02.017
Krivonogov, 2003, Lake Hovsgol in the late Pleistocene and Holocene: on-land geological evidence for a change in its level, 187
Krivonogov, S.K., Sheinkman, V.S., Mistryukov, A.A., 2005. Ice damming of the Darhad paleolake (Northern Mongolia) during the late Pleistocene. Quaternary International, this volume doi:10.1016/j.quaint.2004.11.010.
Mortlock, 1989, A simple method for the rapid determination of biogenic opal in pelagic marine sediments, Deep-Sea Research, 36, 1415, 10.1016/0198-0149(89)90092-7
Nakamura, T., Oda, T., Tanaka, A., Horiuchi, K., 2003. High precision 14C age estimation of bottom sediments of Lake Baikal and Lake Hovsgol by AMS. Gekkan Chikyu, Special No. 42. Kaiyoshuppansha, Tokyo, pp. 20–31 (in Japanese).
Nara, F., Tani, Y., Soma, Y., Soma, M., Naraoka, H., Watanabe, T., Horiuchi, K., Kawai, T., Oda, T., Nakamura, T., 2005. Response of phytoplankton productivity to climate change recorded by sedimentary photosynthetic pigments in Lake Hovsgol (Mongolia) for the last 23,000 years. Quaternary International, this volume doi:10.1016/j.quaint.2004.11.009.
Prokopenko, 2003, Changes in the composition of bottom sediments of Lake Hovsgol as an indication of climatic change in the Baikal region 15–14kaBP, Doklady AN, 390, 109
Stuiver, 1993, Extended 14C database and revised CALIB 3.0 14C age calibration program, Radiocarbon, 35, 215, 10.1017/S0033822200013904
Stuiver, 1995, The GISP2 δ18O Climatic Record of the Past 16,500 years and the Role of the Sun, Ocean, and Volcanoes, Quaternary Research, 44, 341, 10.1006/qres.1995.1079
Stuiver, 1998, INTCAL98 radiocarbon age calibration, 24,000-0calBP, Radiocarbon, 40, 1041, 10.1017/S0033822200019123
Telford, 2004, The intercept is a poor estimate of a calibrated radiocarbon age, The Holocene, 14, 296, 10.1191/0959683604hl707fa
Yang, 2004, The evolution of dry lands in northern China and in the Republic of Mongolia since the Last Glacial Maximum, Quaternary International, 118–119, 69, 10.1016/S1040-6182(03)00131-9
Zolotarev, 1989, Relief of Lake Hovsgol basin. Geomorphology of lake bottom, 112