Larisa V Golovatyuk

Dr. Larisa V Golovatyuk


Research Focus & Metrics

Academic Career Length

14Years (2013-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 July 2013 in Arid Ecosystems
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TZT. D. Zinchenko
T. D. Zinchenko
LGLarisa V Golovatyuk
Larisa V Golovatyuk
The review of the salinity tolerance of various macrozoobenthos taxa is based on the published data and the results of our studies. Significant differences in the tolerance of hydrobionts to water salinity in rivers of different arid regions are shown. Leeches, bivalved mollusks, larvae of stoneflies, caddis flies, and mayflies are the most stenohaline species. The taxonomical structure of macrozoobenthos in saline rivers of Lake Elton basin in the arid zone of Russian South is presented.

5 November 2016 in Russian Journal of Ecology
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LGLarisa V Golovatyuk
Larisa V Golovatyuk
VSV. K. Shitikov
V. K. Shitikov

26 September 2019 in Aquatic Ecology
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LGLarisa V Golovatyuk
Larisa V Golovatyuk
TZTatiana D. Zinchenko
Tatiana D. Zinchenko
Larisa NazarovaLarisa Nazarova
Larisa Nazarova

1 May 2021 in Contemporary Problems of Ecology
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LNL. B. Nazarova
L. B. Nazarova
NRN. G. Razjigaeva
N. G. Razjigaeva
LGLarisa V Golovatyuk
Larisa V Golovatyuk
BBB. K. Biskaborn
B. K. Biskaborn
TGT. A. Grebennikova
T. A. Grebennikova
BDB. Diekmann
B. Diekmann
This paper examines a 115 cm long profile section of lacustrine-swamp sediments from the Langou I Bay (eastern part of Primorsky Krai; 44°25′10.16″ N, 135°54′26.08″ E). According to the produced age model, the sediments are 3900 years old. A multiproxy study involving geochemical, chironomid, diatom, and palynological analysis indicates that the climatic and environmental conditions on the seacoast in the eastern part of Primorsky Krai developed in many respects synchronously with known climatic phases of the Late Holocene. The period from ca. 4200 to 2600 cal years BP corresponds to the first and second warm stages of the Jōmon period and the late Jōmon transgression in Japan. The peak of summer temperatures in the vicinity of the Langou I Bay occurred between 2900 and 2600 cal years BP. The cooling that began after 2600 cal years BP was not as severe in the study area as in Japan (cold Jōmon and Kofun stages): the reconstructed temperatures were 1°C lower than now; in Japan, they were 2–3°C below the current level. The Medieval Climate Optimum (Nara–Heian–Kamakura stage in Japan) reconstructed for the eastern part of Primorsky Krai in the period from 1250 to 750 cal years BP featured a humid climate with summer temperatures ca. 1.5°C higher than at present. The period between 750 and 250 cal years BP correlates with the Little Ice Age: summer temperatures had dropped to 1.5–2°C below the modern one. In the last 200 years, the lake has been shallowing and has nearly dried out. This period is marked by temperature fluctuations amid the trend of climate warming.


19 February 2018 in Marine and Freshwater Research
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LGLarisa V Golovatyuk
Larisa V Golovatyuk
TZTatiana D. Zinchenko
Tatiana D. Zinchenko
NSNadezhda N. Sushchik
Nadezhda N. Sushchik
GKGalina S. Kalachova
Galina S. Kalachova
MGMichail I. Gladyshev
Michail I. Gladyshev
We studied species composition, density, biomass and production of larvae of the family Ceratopogonidae in two saline rivers (Volgograd region, Russia). Ceratopoponids make up an important part of macroinvertebrate community in these rivers. Average monthly production (dry weight) of ceratopogonid larvae in the rivers was 3.5–4.8 g m–2 month–1 in May and ~0.9 g m–2 month–1 in August. For the first time, feeding spectra of ceratopogonid larvae, Palpomyia schmidti Goetghebuer, 1934, was studied using fatty acid analyses. The larvae of P. schmidti appeared to selectively consume diatoms and other algae and to avoid bacteria and decomposed dead organic matter (detritus) of low nutritive quality.