Zobrazeno 1 - 8
of 8
pro vyhledávání: '"M A Klimin"'
Autor:
N. G. Razjigaeva, L. A. Ganzey, T. A. Grebennikova, T. A. Kopoteva, M. A. Klimin, Kh. A. Arslanov, F. E. Maksimov, A. Yu. Petrov, I. Yu. Chekryzhov, N. Yu. Popov, A. M. Panichev
Publikováno v:
Russian Journal of Pacific Geology. 17:41-53
Autor:
N. G. Razzhigaeva, T. A. Kopoteva, T. R. Makarova, T. A. Grebennikova, M. S. Lyashchevskaya, L. M. Mokhova, L. A. Ganzey, E. P. Kudryavtseva, A. M. Panichev, M. A. Klimin, Kh. A. Arslanov, F. E. Maksimov, A. Yu. Petrov
Publikováno v:
Doklady Earth Sciences. 507:S69-S80
Publikováno v:
Inland Water Biology. 13:111-121
The distribution of organic matter (OM), hydrocarbons, phytopigments and ecological–trophic groups of bacteriobenthos has been investigated in the bottom sediments of the internal estuaries of the small Muchke and Toki rivers. The morphological and
Publikováno v:
Геохимия. 64:206-211
We used Rock Eval pyrolysis to examine a peat collection in the Gursky field (located in the Lower Priamurye) during the early stages of diagenesis. This study focused on the top 350 cm of peat, and it also studied the producers of the organic matter
Publikováno v:
Geochemistry International. 57:227-231
Rock–Eval pyrolysis data were obtained on a collection of peat samples at various diagenesis stages (from depths of 0–350 cm) from the Gurskoe deposit, lower Amur area, and on producers of organic matter (OM). The pyrograms of the peat OM are sup
Publikováno v:
Geography and Natural Resources. 39:239-247
The spatial and temporal dynamics of monsoon in the Holocene has been reconstructed for the Lower Amur area. Four stages of cooling are determined (10300–10800, 8000–8300, 4200–4600 and 2500 yrs. ago). During these periods the intensity of the
Publikováno v:
Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms. :676-680
The Gursky peatbog contains the most complete terrestrial record of environmental changes for the last 13 000 14 C years in the Lower Amur River basin. Pollen and AMS 14 C data were obtained from a 340 cm long section, represented by peat and saprope
Publikováno v:
Radiocarbon. 45:25-32
The Russian Far East is characterized by widespread peat bogs with a sufficiently thick peat accumulation. A series of radiocarbon dates from the studied peat bogs (in Lower Amur) were obtained. Analysis of these dates shows that the total peat forma