Svetlana S. Trofimova
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Previous Organizations / Institutes
The organizations / institutes from the scholar's other articles in the past ten years
Research Subjects
Svetlana S. Trofimova has a total of 28 co-authors. Here are the top co-authors by number of shared publications:
- Elena G. Lapteva
Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences
5 shared publications - Evgeniya L. Lychagina
Пермский государственный национальный исследовательский университет; Пермский государственный гуманитарно-педагогический университет (г. Пермь, Россия)
2 shared publications - Irina Vladimirovna Kirillova
Institute of Geography, Russian Academy of Sciences, Moscow, Russia
2 shared publications - Nataliya E. Zaretskaya
Institute of Geography, Russian Academy of Sciences
2 shared publications - Oksana Zanina
Institute of Physico-Chemical and Biological Problems of Soil Science of the Russian Academy of Sciences
2 shared publications - Ol'GA F. Chernova
Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Moscow, Russia
2 shared publications
Latest Publications
- 20 March 2023
- Published by Springer Nature in Vegetation History and Archaeobotany
- Vol. 32 (4) , 361-385
Holocene vegetation dynamics, river valley evolution and human settlement of the upper Kama valley, Ural region, Russia
- 20 March 2023
- Published by Springer Nature in Vegetation History and Archaeobotany
- Vol. 32 (4) , 361-385
Holocene vegetation dynamics, river valley evolution and human settlement of the upper Kama valley, Ural region, Russia
- Open Access
- 26 February 2021
- Published by Tyumen Scientific Center of the SB RAS in Vestnik Arheologii, Antropologii i Etnografii
- No. 1(52),p. 5-19
Human palaeoenvironment in the Upper Kama River basin: experience of reconstruction
Here, we present the results of comprehensive (archaeological and palaeoecological) studies undertaken in 2014–2018 in the basin of the Upper Kama River in the north of Perm Region, eastern part of the East European Plain. The main objects for the research were archaeological sites, primarily their chronological attribution and localization specifics. In total, 100 sites belonging to a wide chronological range from the Mesolithic to the Late Middle Ages were identified in the study area. The palaeochannel method was used to identify the association of the archaeological sites to certain landscapes within the river valley. As a result, five morphologically diverse sectors have been identified. For the reconstruction of natural landscapes and plant communities, palynological and plant macrofossil methods were used. Radiocarbon analysis was used to date these events. The initial human habitation of the Upper Kama region took place in the early Holocene, after the formation of the 2nd and 1st river terraces. The Mesolithic sites have been dated to this period. They were located either on the second river terrace, or on the bedrock valley side. In the Middle Holocene, along with the spread of broad-leaved species in forests, 6th–5th floodplain generations were formed, and the river was characterized by high water content. The Neolithic sites located on the Kama river terraces belong to this period. In the end of the Middle Holocene, the maximum distribution of spruce forests began. This was the time of existence of the Garin Chalcolithic Culture settlements. They were located either on the 4th–5th floodplain generations, or on the bedrock valley side. In the end of the Subboreal and first half of the Subatlantic periods, a key role in the forest stand was played by pine, forming southern taiga light coniferous forests. The water content of the Kama decreased. The sites of the Early Iron Age, located on low terraces or in the floodplain, are dated to this time. In the second half of the Subatlantic period of the Holocene, forests acquired modern mid-taiga appearane, which coincided with the arrival of the medieval population. Medieval hillforts were located on the bedrock valley sides, and the settlements were associated with river terraces, shores of oxbow lakes and floodplains of small rivers.
- 26 February 2021
- Published by Tyumen Scientific Center of the SB RAS in Vestnik Arheologii, Antropologii i Etnografii
- No. 1(52),p. 5-19
Open AccessHuman palaeoenvironment in the Upper Kama River basin: experience of reconstruction
Here, we present the results of comprehensive (archaeological and palaeoecological) studies undertaken in 2014–2018 in the basin of the Upper Kama River in the north of Perm Region, eastern part of the East European Plain. The main objects for the research were archaeological sites, primarily their chronological attribution and localization specifics. In total, 100 sites belonging to a wide chronological range from the Mesolithic to the Late Middle Ages were identified in the study area. The palaeochannel method was used to identify the association of the archaeological sites to certain landscapes within the river valley. As a result, five morphologically diverse sectors have been identified. For the reconstruction of natural landscapes and plant communities, palynological and plant macrofossil methods were used. Radiocarbon analysis was used to date these events. The initial human habitation of the Upper Kama region took place in the early Holocene, after the formation of the 2nd and 1st river terraces. The Mesolithic sites have been dated to this period. They were located either on the second river terrace, or on the bedrock valley side. In the Middle Holocene, along with the spread of broad-leaved species in forests, 6th–5th floodplain generations were formed, and the river was characterized by high water content. The Neolithic sites located on the Kama river terraces belong to this period. In the end of the Middle Holocene, the maximum distribution of spruce forests began. This was the time of existence of the Garin Chalcolithic Culture settlements. They were located either on the 4th–5th floodplain generations, or on the bedrock valley side. In the end of the Subboreal and first half of the Subatlantic periods, a key role in the forest stand was played by pine, forming southern taiga light coniferous forests. The water content of the Kama decreased. The sites of the Early Iron Age, located on low terraces or in the floodplain, are dated to this time. In the second half of the Subatlantic period of the Holocene, forests acquired modern mid-taiga appearane, which coincided with the arrival of the medieval population. Medieval hillforts were located on the bedrock valley sides, and the settlements were associated with river terraces, shores of oxbow lakes and floodplains of small rivers.
- 1 December 2019
- Published by Pleiades Publishing Ltd in Biology Bulletin
- Vol. 46 (8) , 850-863
Crustacea (Branchiopoda) among Organic Remains from Mammoth Hair
The purpose of this study is to analyze the taxonomic composition of the branchiopod crustaceans (Crustacea: Branchiopoda) from the assemblage of animal and plant remains recovered from fossil mammoth hair found in the Allaikha River basin, Sakha Republic, Russian Federation. We studied the hair structure. AMS radiocarbon dating of both the hair itself and the remains demonstrated their different ages. We found different animal and plant remains in the hair taphocoenosis. The most diverse and numerous remains belong to branchiopod crustaceans: resting eggs and distal portions of the mandibles of Anostraca, distal portions of the mandibles of Notostraca, filtering limbs of some Anostraca or Daphniidae, ephippia of Daphnia (Daphnia) curvirostris, Daphnia (Ctenodaphnia) atkinsoni, and D. (C.) magna. No representatives of D. (Ctenodaphnia) now occur in northeastern Eurasia, but our findings of numerous ephippia in the fossil hair of two mammoths, one from the Allaikha River and the other, studied previously, from the Bol’shaya Chukochya River basin (see Kirillova et al., 2016), show that Daphnia (Ctenodaphnia) taxa occurred in the region at least in the past and were probably common and widely distributed there. The reasons for the extinction of Daphnia (Ctenodaphnia) in northeastern Eurasia require additional special study. We also emphasize the need for further studies of the morphology of ephippia, resting eggs, and mandibles of recent Branchiopoda, which would be essential for adequate identification of Pleistocene remains.
- 1 December 2019
- Published by Pleiades Publishing Ltd in Biology Bulletin
- Vol. 46 (8) , 850-863
Crustacea (Branchiopoda) among Organic Remains from Mammoth Hair
The purpose of this study is to analyze the taxonomic composition of the branchiopod crustaceans (Crustacea: Branchiopoda) from the assemblage of animal and plant remains recovered from fossil mammoth hair found in the Allaikha River basin, Sakha Republic, Russian Federation. We studied the hair structure. AMS radiocarbon dating of both the hair itself and the remains demonstrated their different ages. We found different animal and plant remains in the hair taphocoenosis. The most diverse and numerous remains belong to branchiopod crustaceans: resting eggs and distal portions of the mandibles of Anostraca, distal portions of the mandibles of Notostraca, filtering limbs of some Anostraca or Daphniidae, ephippia of Daphnia (Daphnia) curvirostris, Daphnia (Ctenodaphnia) atkinsoni, and D. (C.) magna. No representatives of D. (Ctenodaphnia) now occur in northeastern Eurasia, but our findings of numerous ephippia in the fossil hair of two mammoths, one from the Allaikha River and the other, studied previously, from the Bol’shaya Chukochya River basin (see Kirillova et al., 2016), show that Daphnia (Ctenodaphnia) taxa occurred in the region at least in the past and were probably common and widely distributed there. The reasons for the extinction of Daphnia (Ctenodaphnia) in northeastern Eurasia require additional special study. We also emphasize the need for further studies of the morphology of ephippia, resting eggs, and mandibles of recent Branchiopoda, which would be essential for adequate identification of Pleistocene remains.
- 1 November 2019
- Published by Pleiades Publishing Ltd in Russian Journal of Ecology
- Vol. 50 (6) , 543-550
Methods of Paleoecological Investigations: A Case Study of the Holocene Environmental Reconstruction
— This work reconstructs changes in the Holocene paleolandscape, plants, and climate conditions of the Upper Kama Region based on integrated analysis of data collected through paleochannel,...
- 1 November 2019
- Published by Pleiades Publishing Ltd in Russian Journal of Ecology
- Vol. 50 (6) , 543-550
Methods of Paleoecological Investigations: A Case Study of the Holocene Environmental Reconstruction
— This work reconstructs changes in the Holocene paleolandscape, plants, and climate conditions of the Upper Kama Region based on integrated analysis of data collected through paleochannel,...
- 1 March 2014
- Published by Pleiades Publishing Ltd in Doklady Biological Sciences
- Vol. 455 (1) , 83-86
The first reconstruction of the late glacial plant communities on the Yamal peninsula based on plant macrofossils
- 1 March 2014
- Published by Pleiades Publishing Ltd in Doklady Biological Sciences
- Vol. 455 (1) , 83-86
The first reconstruction of the late glacial plant communities on the Yamal peninsula based on plant macrofossils
- 1 September 2013
- Published by Pleiades Publishing Ltd in Doklady Biological Sciences
- Vol. 452 (1) , 296-299
The first finding of a frozen Holocene bison (Bison priscus Bojanus, 1827) carcass in Chukotka
- 1 September 2013
- Published by Pleiades Publishing Ltd in Doklady Biological Sciences
- Vol. 452 (1) , 296-299
The first finding of a frozen Holocene bison (Bison priscus Bojanus, 1827) carcass in Chukotka
- 22 June 2010
- Published by Pleiades Publishing Ltd in Doklady Biological Sciences
- Vol. 432 (1) , 209-211
The intestinal contents of a baby Woolly mammoth (Mammuthus primigenius Blumenbach, 1799) from the Yuribey River (Yamal Peninsula)
- 22 June 2010
- Published by Pleiades Publishing Ltd in Doklady Biological Sciences
- Vol. 432 (1) , 209-211
The intestinal contents of a baby Woolly mammoth (Mammuthus primigenius Blumenbach, 1799) from the Yuribey River (Yamal Peninsula)