First finding of a mammoth female (<Emphasis Type="Italic">Mammuthus primigenius</Emphasis> Blum.) on the Taimyr Peninsula     

I. V. Kirillova  F. K. Shidlovskiy  B. F. Khasanov 《Doklady Earth Sciences》2011,436(2):193-196

The first finding of a mammoth female skeleton from the Kastykhtakh River valley, Taimyr Peninsula, is described. The skeleton consists of 104 elements including the skull and lower jaw; small distal limb bones, tail vertebrae, and one tusk are absent. There are teeth of the two last changes in the jaws. The skeleton elements have individual features: sigmoid contact of the low second and third molars, crack in the neural arch of the atlas, and false joint and calluses on places of the rib fractures. The calibrated radiocarbon dating of the tubular bone is 32 070-30 565 yr (Kargin interglacial time).  相似文献   

Analysis of Diatoms of the Water Column and Bottom Sediments of Lake Shira(Khakassia,Russia)     

Galina BOLOBANSCHIKOVA  Denis ROGOZIN 《《地质学报》英文版》2014,88(Z1):56-57

正Meromictic lakes are interesting objects for study in terms of paleolimnology.The lamination of the bottom sediments well expressed in these lakes.It is related with permanent stratification of the water column.Through this  相似文献   

Buchia faunas and biostratigraphy of the Jurassic-Cretaceous boundary deposits in the Komsomolsk section (Russian Far East)     

O. S. Urman  O. S. Dzyuba  G. L. Kirillova  B. N. Shurygin 《Russian Journal of Pacific Geology》2014,8(5):346-359

Abundant Buchiidae (Bivalvia) from the Upper Volgian-Lower Valanginian sediments of the Northern Sikhote-Alin (Russian Far East) were studied in the key section at right bank of the Amur River opposite to Komsomolsk-on Amur. The analysis of the Buchiidae stratigraphic distribution in the section allowed us to reveal the sequence of Buchia-bearing beds: this is well correlated with the Buchia zonal scales of many Arctic regions. Here, from the base upward, there have been recognized the following: beds with Buchia terebratuloides, beds with B. unschensis and B. terebratuloides, beds with B. volgensis, and beds with B. inflata and B. keyserlingi. The beds with B. unschensis and B. terebratuloides also yielded the Berriasian ammonite Pseudosubplanites? sp. of Tethyan affinity. The obtained paleontological data confirm the occurrence of a large syncline in the studied section. The data also permit one to refine the age spans of the local stratigraphic units.  相似文献   

Supercritically accreting stellar mass black holes as ultraluminous X-ray sources     

Juri Poutanen  Galina Lipunova  Sergei Fabrika  Alexey G. Butkevich  Pavel Abolmasov 《Monthly notices of the Royal Astronomical Society》2007,377(3):1187-1194

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On the 70th birthday of Vladimir Nikolaevich Voevodin     

A. I. Khanchuk  S. M. Rodionov  G. L. Kirillova 《Russian Journal of Pacific Geology》2007,1(3):302-303

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Problems of sedimentogenesis and tectonics at the IV International Symposium “Paleoclimates of the Cretaceous Period in Asia and Their Global Correlation”     

G. L. Kirillova 《Russian Journal of Pacific Geology》2010,4(4):355-360

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Vyacheslav Ivanovich Kovalenko (on his 70th birthday)     

A. I. Khanchuk  S. M. Rodionov  G. L. Kirillova 《Geotectonics》2006,40(6):483-484

Chronicle

Vyacheslav Ivanovich Kovalenko (on his 70th birthday)  相似文献   

Gold fineness and Au/Ag ratios of pyrite-containing ores as additional indicators of physico-chemical conditions of hydrothermal ore formation     

Galina Palyanova 《Journal of Geochemical Exploration》2009

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Magnetic,paleomagnetic and palynologic studies of Paleolithic depositions of the Akhshtyrskaya cave (Russia)     

Genrietta A. Pospelova  Elżbieta Król  Galina M. Levkovskaya  Jadwiga Kruczyk  Magdalena Kądziałko-Hofmokl  Sergey A. Kulakov 《Acta Geophysica》2007,55(4):619-639

The paper presents the results of experimental rock-magnetic, paleomagnetic and palynologic study of Paleolithic sediments sampled along two profiles in the Akhshtyrskaya cave, situated in the vicinity of Black Sea shore. In the upper part of profiles, some magnetite was observed; in the middle and lower parts, strongly oxidized non-stoichiometric magnetite and hematite prevail. Thin maghemite covers on the surface of fine magnetite grains are present in the majority of specimens. Natural remanence has one characteristic component (CHRM), mostly of chemical origin, although in few specimens containing magnetite it may be sedimentary. Directions of CHRM obtained by standard paleomagnetic methods revealed anomalous pattern only in layer 3/2, which is slightly older than the overlying layer 3/1 whose age was established as (35±2)×10³ years BP by the U-Th method. This suggests that this paleomagnetic anomaly (PMA) can be correlated with Kargapolovo excursion dated on about (45−39)×10³ years BP. In the remaining overlying and underlying layers, directions of CHRM are grouped around the present geomagnetic field. Depth distributions of scalar magnetic parameters generally coincide with the lithological division of the profiles. Palynologic study revealed the presence of 22 pollen zones. Five thermomers separated with colder periods were found in the middle and lower parts of profile. The non-magnetite composition of magnetic fraction of the majority of studied sediments — oxidized nonstoichiometric magnetite and hematite — resulted in the lack of correlations between paleoclimatic and scalar magnetic characteristics.  相似文献   

Paleoenvironmental proxy records from Lake Hovsgol, Mongolia, and a synthesis of Holocene climate change in the Lake Baikal watershed   总被引：1，自引：0，他引：1  

Alexander A. Prokopenko  Galina K. Khursevich  Mikhail I. Kuzmin  Douglas F. Williams  Nataliya V. Kulagina  Anna A. Abzaeva 《Quaternary Research》2007,68(1):2-17

Here we discuss paleoenvironmental evolution in the Baikal region during the Holocene using new records of aquatic (diatom) and terrestrial vegetation changes from Hovsgol, Mongolia's largest and deepest lake. We reconcile previous contradictory Baikal timescales by constraining reservoir corrections of AMS dates on bulk sedimentary organic carbon. Synthesis of the Holocene records in the Baikal watershed reveals a northward progression in landscape/vegetation changes and an anti-phase behavior of diatom and biogenic silica proxies in neighboring rift lakes. In Lake Baikal, these proxies appear to be responsive to annual temperature increases after 6 ka, whereas in Lake Hovsgol they respond to higher precipitation/runoff from 11 to 7 ka. Unlike around Lake Baikal, warmer summers between 6 and 3.5 ka resulted in the decline, not expansion, of forest vegetation around Lake Hovsgol, apparently as a result of higher soil temperatures and lower moisture availability. The regional climatic proxy data are consistent with a series of 500-yr time slice Holocene GCM simulations for continental Eurasia. Our results allow reevaluation of the concepts of ‘the Holocene optimum’ and a ‘maximum of the Asian summer monsoon’, as applied to paleoclimate records from continental Asia.  相似文献