The identification of archaeological obsidian sources on Kamchatka Peninsula (Russian Far East) using geochemical and geological data: Current progress

2017 ◽  
Vol 442 ◽  
pp. 95-103 ◽  
Author(s):  
Andrei V. Grebennikov ◽  
Yaroslav V. Kuzmin
2019 ◽  
Vol 53 (1) ◽  
pp. 107-142 ◽  
Author(s):  
D. E. Himelbrant ◽  
I. S. Stepanchikova ◽  
T. Ahti ◽  
V. Yu. Neshataeva

The first lichenological inventory in Koryakia has resulted in the list of 315 species reported from Parapolsky Dale, within and in vicinities of the Koryak State Reserve. Altogether 46 species are published from the Kamchatka Territory for the first time, including Lecanographa grumulosa new to Russia, East Asia and Beringia; Cercidospora trypetheliza, Lecania dubitans, Pertusaria borealis, Piccolia ochrophora, Protoparmelia cupreobadia, Rimularia badioatra and Strangospora moriformis new to Russian Far East; Abrothallus bertianus, Cladonia strepsilis, Physciella melanchra, Rimularia badioatra, Sclerococcum parasiticum, Sphinctrina leucopoda and Strangospora moriformis new to Beringia. The lichen diversity of the study area is relatively poor due to natural reasons. Comparison with neighboring regions (Kamchatka Peninsula, Chukotka, Magadan Region, Yakutia and Alaska) shows that the lichen flora of Parapolsky Dale contains almost no specific species. The majority of the species recorded here are also known from neighboring regions, especially Alaska and Kamchatka Peninsula.


2011 ◽  
Vol 45 ◽  
pp. 150-158 ◽  
Author(s):  
D. E. Himelbrant ◽  
I. S. Stepanchikova

The fir (Abies gracilis) grove (Kamchatka Peninsula, Kronotsky State Nature Reserve) is a unique area for the northern part of the Russian Far East. As a result of revision of herbarium specimens and literature data a list of lichens of the fir grove was compiled, comprising 55 species. Of them, 27 species are new to the Kronotsky Reserve, 30 are firstly reported for the grove. Altogether 36 lichen epiphytes of Abies gracilis are known.


Forests ◽  
2017 ◽  
Vol 8 (9) ◽  
pp. 315 ◽  
Author(s):  
Clara Deck ◽  
Gregory Wiles ◽  
Sarah Frederick ◽  
Vladimir Matsovsky ◽  
Tatiana Kuderina ◽  
...  

Arctoa ◽  
2008 ◽  
Vol 17 (1) ◽  
pp. 49-62 ◽  
Author(s):  
Irina V. Czernyadjeva ◽  
Elena A. Ignatova

Arctoa ◽  
2006 ◽  
Vol 15 (1) ◽  
pp. 183-186 ◽  
Author(s):  
Timo Koponen ◽  
Irina V. Czernyadjeva

Author(s):  
I. V. Enushchenko ◽  
N. S. Probatova

Two new species in the genus Festuca L. (Poaceae) are described, related to F. altaica Trin.: F. itelmenorum Enustschenko et Prob. (Kamchatka Peninsula, Kronotskii Nature Reserve) and F. kozhevnikovii Enustschenko et Prob. (Amur Region and Republic of Buryatia). Leaf blades of the newly described species as well as of F. altaica from different parts of its distribution range have been studied and illustrated.


2016 ◽  
Author(s):  
Vera D. Meyer ◽  
Jens Hefter ◽  
Gerrit Lohmann ◽  
Ralf Tiedemann ◽  
Gesine Mollenhauer

Abstract. Little is known about the climate evolution on the Kamchatka Peninsula during the last deglaciation as existing climate records do not reach beyond 12 ka BP. In this study, a summer-temperature record for the past 20 ka is presented. Branched Glycerol Dialkyl Glycerol Tetraethers, terrigenous biomarkers suitable for continental air temperature reconstructions, were analyzed in a sediment core from the western continental margin off Kamchatka/marginal Northwest Pacific (NW Pacific). The record reveals that summer temperatures on Kamchatka during the Last Glacial Maximum (LGM) equaled modern. We suggest that strong southerly winds associated with a pronounced North Pacific High pressure system over the subarctic NW Pacific accounted for the warm conditions. A comparison with outputs from an Earth System Model reveals discrepancies between model and proxy-based reconstructions for the LGM-temperature and atmospheric circulation in the NW Pacific realm. The deglacial temperature development is characterized by abrupt millennial-scale temperature oscillations. The Bølling/Allerød warm-phase and the Younger Dryas cold-spell are pronounced events, providing evidence for a strong impact of North-Atlantic climate variability on temperature development in southeastern Siberia. Summer insolation and teleconnections with the North Atlantic determine the long-term temperature development during the Holocene.


2020 ◽  
Vol 54 (1) ◽  
pp. 139-148
Author(s):  
I. V. Frolov ◽  
L. V. Gagarina

A revision of 47 specimens of crustose Teloschistaceae (so-called “Caloplaca s. lat.”) from the Russian Far East in the herbarium LE belonging to 21 species is resulted in re-identification of 18 specimens and new records. Blastenia furfuracea from the Kamchatka Peninsula is new to the Russian Far East. Caloplaca fraudans is new to the Kamchatka Peninsula. Records of Blastenia ferruginea, B. hungarica, Caloplaca haematites and Solitaria chrysophthalma are doubtful for the Far East. Placodium haematites var. ussuriense Tomin [≡ Caloplaca haematites var. ussuriensis (Tomin) Zahlbr.] is lectotypified and synonymized under Caloplaca stillicidiorum s. lat.


Radiocarbon ◽  
2007 ◽  
Vol 49 (2) ◽  
pp. 1065-1078 ◽  
Author(s):  
Natalia E Zaretskaya ◽  
Vera V Ponomareva ◽  
Leopold D Sulerzhitsky

Radiocarbon dating is widely used when studying recent volcanic activity in the Kamchatka Peninsula due to the abundance of organic matter that is associated with the volcanic deposits. Here, we present the results of 14C dating of major volcanic events within the active South Kamchatka volcanic zone. South Kamchatka includes 8 recently active volcanic centers (stratovolcanoes, calderas, and large craters) that have been erupting during the Holocene. Their tephras represent useful markers for both the southern part of the peninsula and the Northern Kurile Islands. Since these marker tephra layers facilitate stratigraphic and tephrochronological studies in this area, it was important to determine their ages. We have obtained 73 new individual 14C dates on paleosol, peat, charcoal, and wood associated with the marker tephra layers, then complemented these data with 37 earlier published dates and analyzed the resulting data set. We selected the reliable dates and then obtained average 14C ages of marker tephra layers. The details of these procedures, as well as brief descriptions of South Kamchatka Holocene eruptions and their tephra beds, are presented in the paper.


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