V. V. Mukhina's research while affiliated with P.P. Shirshov Institute of Oceanology and other places
What is this page?
This page lists the scientific contributions of an author, who either does not have a ResearchGate profile, or has not yet added these contributions to their profile.
It was automatically created by ResearchGate to create a record of this author's body of work. We create such pages to advance our goal of creating and maintaining the most comprehensive scientific repository possible. In doing so, we process publicly available (personal) data relating to the author as a member of the scientific community.
If you're a ResearchGate member, you can follow this page to keep up with this author's work.
If you are this author, and you don't want us to display this page anymore, please let us know.
It was automatically created by ResearchGate to create a record of this author's body of work. We create such pages to advance our goal of creating and maintaining the most comprehensive scientific repository possible. In doing so, we process publicly available (personal) data relating to the author as a member of the scientific community.
If you're a ResearchGate member, you can follow this page to keep up with this author's work.
If you are this author, and you don't want us to display this page anymore, please let us know.
Publications (7)
Diatoms were studied in the KOMEX LV28-34-2 sediment core from the northwestern Sea of Okhotsk. The interval from the penultimate
glacial to the Holocene was subdivided into stratigraphic units based on the distribution of biogeographic groups and individual
index species. The analysis of the diatom assemblages indicated that, during the Last Glaci...
Diatom and nannoplankton microfossils in the samples of the surface bottom sediments and cores from the western part of the
Norwegian Sea (64°–79°N) were studied. The abundance, distribution, taxonomic composition, and structure of the assemblages
are determined by the productivity and temperature of the surface waters, by the distance from the sho...
The study of diatoms and benthic foraminifers from the southeastern shelf of the Laptev Sea shows that their most diverse
and abundant recent assemblages populate the peripheral underwater part of the Lena River delta representing the marginal
filter of the sea. This area is characterized by an intense interaction between the fresh waters of the Si...
The study of diatoms and benthic foraminifers from the southeastern shelf of the Laptev Sea shows that their most diverse and abundant recent assemblages populate the peripheral underwater part of the Lena River delta representing the marginal filter of the sea. This area is characterized by intense interaction between fresh waters of Siberian rive...
A combined examination of the siliceous microfossils (diatoms and radiolarians) and the lithophysical parameters (magnetic susceptibility and contents of the coarse-grained sediment fraction and the ice-rafted detritus) revealed the stratigraphy of the sediment core from the deep northern shelf of the Sea of Okhotsk in the scale of the oxygen-isoto...
Microplankton (coccoliths and diatoms) from the bottom sediments of the Afanasii Nikitin Seamount area (the Indian Ocean) was examined. The species of the calcareous nannoplankton refer to the Late Cretaceous; Paleocene; Eocene; Oligocene; Early, Early Middle, and Late Miocene; Late Pliocene; and Late Pleistocene-Holocene. Within the latter period,...
Citations
... Age models for cores LV27-5-3 (Matul et al., 2003) and GE99-10-3 (Artemova et al., 2019, submitted). The red lines are the levels of last occurrence of radiolarian species. ...
![[object Object]](https://i1.rgstatic.net/ii/profile.image/272537879838720-1441989502066_Q64/Alexander-Matul.jpg)
... The diatom assemblages in the surface sediments of the Arctic seas reflect the physicochemical characteristics of the overlying water bodies (Jousé 1962;Maynard 1976;Kravitz et al. 1987;Polyakova 1988Polyakova , 1989Polyakova , 1997Abelmann 1992;Cremer 1999;Jiang et al. 2001;Matul et al. 2007;Obrezkova et al. 2014;Astakhov et al. 2015;Polyakova et al. 2016;Miettinen 2018) and ice cover distribution (Meguro et al. 1966;Abelmann 1992;Crosta et al. 1997Crosta et al. , 1998Gersonde and Zeilinski 2000;Belt et al. 2015;Fragoso et al. 2018;Tsukazaki et al. 2018;Fukai et al. 2021). Studying the diatoms predominating in the water column and surface sediments of the seas of Eastern Siberia and adjacent regions enables the assessment of the impact of climate change on the environment (Polyakova 1996(Polyakova , 1997Cremer 1998Cremer , 1999Tsoy 2001;Bauch and Polyakova 2003;Polyakova et al. 2005Polyakova et al. , 2011Polyakova et al. , 2014Polyakova et al. , 2016Polyakova et al. , 2019Polyakova et al. , 2021Matul et al. 2007;Poulin et al. 2011;Gusev et al. 2014;Obrezkova et al. 2014;Astakhov et al. 2015;Ren et al. 2020). ...
... We compiled data on N. seminae distribution in various sampling material and geographical areas: (1) marine plankton from the Northwestern North Atlantic [7,8,14] and Western Arctic Ocean between the Bering Strait and point of 85°N in the Arctic Ocean Basin [15]; (2) sediment trap on Station NAP, the Southern Northwind Abyssal Plain in the Western Arctic Ocean [16]; and (3) the Late Pleistocene and Holocene sediments from the Arctic Ocean and Nordic and Arctic Seas [17][18][19][20][21][22][23]. ...
... Calculations show that now we have a peak of CO 2 growth. This is in agreement with other studies, e.g., the analysis of remains of planktonic organisms in bot tom sediments [1,19]. After some time, when unre strained rise in the level of atmospheric CO 2 and land surface temperature was anticipated, the ever growing number of researchers come to the conclusion that in the nearest decades (or centuries), we are to expect cli mate cooling and a decrease in CO 2 in the atmosphere and hydrosphere. ...
