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Early Pleistocene Vegetation and Environments near Taurida Cave (Central Crimea) on the Basis of Microphytofossil Data
The existence of vegetation of open environments with a predominance of grass–forb meadow associations and the participation of pine–oak forests was reconstructed on the basis of study of microphytofossils from the Lower Pleistocene deposits of the Taurida cave in central Crimea. These results are c...
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Published in: | Doklady earth sciences 2024-11, Vol.519 (1), p.1906-1911 |
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container_end_page | 1911 |
container_issue | 1 |
container_start_page | 1906 |
container_title | Doklady earth sciences |
container_volume | 519 |
creator | Lopatina, D. A. Zanina, O. G. Lopatin, A. V. |
description | The existence of vegetation of open environments with a predominance of grass–forb meadow associations and the participation of pine–oak forests was reconstructed on the basis of study of microphytofossils from the Lower Pleistocene deposits of the Taurida cave in central Crimea. These results are consistent with data on the composition of land vertebrates from the Taurida locality. The studied spectrum demonstrates similarity with the spore–pollen assemblage of the Berezan horizon of Ukraine with a maximum age of about 1.8 Ma. Based on the abundance of trichomes and plant fibers similar to those of
Ficus carica
Linnaeus, 1753 in the coprolites, it is assumed that the extinct hyenas
Pachycrocuta brevirostris
(Gervais, 1850) ate fig fruits in certain seasons. |
doi_str_mv | 10.1134/S1028334X24603262 |
format | article |
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Ficus carica
Linnaeus, 1753 in the coprolites, it is assumed that the extinct hyenas
Pachycrocuta brevirostris
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Ficus carica
Linnaeus, 1753 in the coprolites, it is assumed that the extinct hyenas
Pachycrocuta brevirostris
(Gervais, 1850) ate fig fruits in certain seasons.</description><subject>Coniferous forests</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fibers</subject><subject>Paleontology</subject><subject>Plant fibers</subject><subject>Pleistocene</subject><subject>Pleistocene deposits</subject><subject>Pleistocene vegetation</subject><subject>Pollen</subject><subject>Spores</subject><subject>Trichomes</subject><subject>Vegetable fibers</subject><subject>Vegetation</subject><subject>Vertebrates</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp1UMlKA0EQbUTBGP0Abw1e9DDa6yxHHeMCioJRvA2VmZpkwqQ7dncC-Xs7RPAgnqrgLVXvEXLK2SXnUl29cSZyKdWnUCmTIhV7ZMC15EkutdqPe4STLX5IjryfM6aU0sWArEfg-g197bHzwdZokH7gFAOEzhoKpqEjs-6cNQs0wVOD4OgYVq5rgJawRnpeRsBBT0vXLRAuaJSFGdIb8J2ntqXPXe3scrYJtrXedz29hQDH5KCF3uPJzxyS97vRuHxInl7uH8vrp6TmRR4SkUGTtrxhGTZFWoPWElBM8omcoMpFjQXHXGiR1inGzEpA1jbFJBO6ESgZk0NytvNdOvu1Qh-quV05E09WkvNMC6Z4Fll8x4qfeu-wrZYxDLhNxVm1rbf6U2_UiJ3GR66Zovt1_l_0DUbWfPc</recordid><startdate>20241101</startdate><enddate>20241101</enddate><creator>Lopatina, D. A.</creator><creator>Zanina, O. G.</creator><creator>Lopatin, A. V.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20241101</creationdate><title>Early Pleistocene Vegetation and Environments near Taurida Cave (Central Crimea) on the Basis of Microphytofossil Data</title><author>Lopatina, D. A. ; Zanina, O. G. ; Lopatin, A. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c198t-27ad6f1d07ed96ca553ae2b8b3be482ce91e82526c6e26242a7fd9b725d2e3003</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Coniferous forests</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fibers</topic><topic>Paleontology</topic><topic>Plant fibers</topic><topic>Pleistocene</topic><topic>Pleistocene deposits</topic><topic>Pleistocene vegetation</topic><topic>Pollen</topic><topic>Spores</topic><topic>Trichomes</topic><topic>Vegetable fibers</topic><topic>Vegetation</topic><topic>Vertebrates</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lopatina, D. A.</creatorcontrib><creatorcontrib>Zanina, O. G.</creatorcontrib><creatorcontrib>Lopatin, A. V.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Doklady earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lopatina, D. A.</au><au>Zanina, O. G.</au><au>Lopatin, A. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Early Pleistocene Vegetation and Environments near Taurida Cave (Central Crimea) on the Basis of Microphytofossil Data</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2024-11-01</date><risdate>2024</risdate><volume>519</volume><issue>1</issue><spage>1906</spage><epage>1911</epage><pages>1906-1911</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>The existence of vegetation of open environments with a predominance of grass–forb meadow associations and the participation of pine–oak forests was reconstructed on the basis of study of microphytofossils from the Lower Pleistocene deposits of the Taurida cave in central Crimea. These results are consistent with data on the composition of land vertebrates from the Taurida locality. The studied spectrum demonstrates similarity with the spore–pollen assemblage of the Berezan horizon of Ukraine with a maximum age of about 1.8 Ma. Based on the abundance of trichomes and plant fibers similar to those of
Ficus carica
Linnaeus, 1753 in the coprolites, it is assumed that the extinct hyenas
Pachycrocuta brevirostris
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subjects | Coniferous forests Earth and Environmental Science Earth Sciences Fibers Paleontology Plant fibers Pleistocene Pleistocene deposits Pleistocene vegetation Pollen Spores Trichomes Vegetable fibers Vegetation Vertebrates |
title | Early Pleistocene Vegetation and Environments near Taurida Cave (Central Crimea) on the Basis of Microphytofossil Data |
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