author_facet Aparin, Boris
Grabovsky, Alexander
Sukhacheva, Elena
Mingareeva, Elena
Janson, Svetlana
Shevchuk, Evgeny
Terleev, Vitaly
Nikonorov, Aleksandr
Akimov, Luka
Aparin, Boris
Grabovsky, Alexander
Sukhacheva, Elena
Mingareeva, Elena
Janson, Svetlana
Shevchuk, Evgeny
Terleev, Vitaly
Nikonorov, Aleksandr
Akimov, Luka
author Aparin, Boris
Grabovsky, Alexander
Sukhacheva, Elena
Mingareeva, Elena
Janson, Svetlana
Shevchuk, Evgeny
Terleev, Vitaly
Nikonorov, Aleksandr
Akimov, Luka
spellingShingle Aparin, Boris
Grabovsky, Alexander
Sukhacheva, Elena
Mingareeva, Elena
Janson, Svetlana
Shevchuk, Evgeny
Terleev, Vitaly
Nikonorov, Aleksandr
Akimov, Luka
E3S Web of Conferences
Organic matter of sediments of South Chukotka
Pulmonary and Respiratory Medicine
Pediatrics, Perinatology, and Child Health
author_sort aparin, boris
spelling Aparin, Boris Grabovsky, Alexander Sukhacheva, Elena Mingareeva, Elena Janson, Svetlana Shevchuk, Evgeny Terleev, Vitaly Nikonorov, Aleksandr Akimov, Luka 2267-1242 EDP Sciences Pulmonary and Respiratory Medicine Pediatrics, Perinatology, and Child Health http://dx.doi.org/10.1051/e3sconf/202015702016 <jats:p>The article discusses data on paleosol, mineralogy, and paleobotany obtained as a result of studying material collected from the Maastricht-Early Paleocene sediments of the Tanyurer Formation of South Chukotka. The burial of organic matter in the sedimentary rock of the Tanyurer Formation is associated with deflationary processes during the period of activation of volcanic activity. On the drained volcanic plateau of soil formation, a sod humus-accumulative process prevailed under the steppe vegetation. Humic substance dispersed in sedimentary rock was represented by a group of humins resistant to microbial decomposition. As a result of exposure to high pressures and temperatures, the colloidal form of humus was transformed into kerogen. Organic compounds (cellulose, lignin) in the plant tissue of buried tree trunks were replaced by silicon compounds. Weathering processes have affected the thin surface layer of dense sedimentary rock. Under the influence of the temperature and humidity gradient, loosening of loose rock and disintegration of clots of colloidal forms of humus occurred.</jats:p> Organic matter of sediments of South Chukotka E3S Web of Conferences
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title Organic matter of sediments of South Chukotka
title_unstemmed Organic matter of sediments of South Chukotka
title_full Organic matter of sediments of South Chukotka
title_fullStr Organic matter of sediments of South Chukotka
title_full_unstemmed Organic matter of sediments of South Chukotka
title_short Organic matter of sediments of South Chukotka
title_sort organic matter of sediments of south chukotka
topic Pulmonary and Respiratory Medicine
Pediatrics, Perinatology, and Child Health
url http://dx.doi.org/10.1051/e3sconf/202015702016
publishDate 2020
physical 02016
description <jats:p>The article discusses data on paleosol, mineralogy, and paleobotany obtained as a result of studying material collected from the Maastricht-Early Paleocene sediments of the Tanyurer Formation of South Chukotka. The burial of organic matter in the sedimentary rock of the Tanyurer Formation is associated with deflationary processes during the period of activation of volcanic activity. On the drained volcanic plateau of soil formation, a sod humus-accumulative process prevailed under the steppe vegetation. Humic substance dispersed in sedimentary rock was represented by a group of humins resistant to microbial decomposition. As a result of exposure to high pressures and temperatures, the colloidal form of humus was transformed into kerogen. Organic compounds (cellulose, lignin) in the plant tissue of buried tree trunks were replaced by silicon compounds. Weathering processes have affected the thin surface layer of dense sedimentary rock. Under the influence of the temperature and humidity gradient, loosening of loose rock and disintegration of clots of colloidal forms of humus occurred.</jats:p>
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author Aparin, Boris, Grabovsky, Alexander, Sukhacheva, Elena, Mingareeva, Elena, Janson, Svetlana, Shevchuk, Evgeny, Terleev, Vitaly, Nikonorov, Aleksandr, Akimov, Luka
author_facet Aparin, Boris, Grabovsky, Alexander, Sukhacheva, Elena, Mingareeva, Elena, Janson, Svetlana, Shevchuk, Evgeny, Terleev, Vitaly, Nikonorov, Aleksandr, Akimov, Luka, Aparin, Boris, Grabovsky, Alexander, Sukhacheva, Elena, Mingareeva, Elena, Janson, Svetlana, Shevchuk, Evgeny, Terleev, Vitaly, Nikonorov, Aleksandr, Akimov, Luka
author_sort aparin, boris
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description <jats:p>The article discusses data on paleosol, mineralogy, and paleobotany obtained as a result of studying material collected from the Maastricht-Early Paleocene sediments of the Tanyurer Formation of South Chukotka. The burial of organic matter in the sedimentary rock of the Tanyurer Formation is associated with deflationary processes during the period of activation of volcanic activity. On the drained volcanic plateau of soil formation, a sod humus-accumulative process prevailed under the steppe vegetation. Humic substance dispersed in sedimentary rock was represented by a group of humins resistant to microbial decomposition. As a result of exposure to high pressures and temperatures, the colloidal form of humus was transformed into kerogen. Organic compounds (cellulose, lignin) in the plant tissue of buried tree trunks were replaced by silicon compounds. Weathering processes have affected the thin surface layer of dense sedimentary rock. Under the influence of the temperature and humidity gradient, loosening of loose rock and disintegration of clots of colloidal forms of humus occurred.</jats:p>
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spelling Aparin, Boris Grabovsky, Alexander Sukhacheva, Elena Mingareeva, Elena Janson, Svetlana Shevchuk, Evgeny Terleev, Vitaly Nikonorov, Aleksandr Akimov, Luka 2267-1242 EDP Sciences Pulmonary and Respiratory Medicine Pediatrics, Perinatology, and Child Health http://dx.doi.org/10.1051/e3sconf/202015702016 <jats:p>The article discusses data on paleosol, mineralogy, and paleobotany obtained as a result of studying material collected from the Maastricht-Early Paleocene sediments of the Tanyurer Formation of South Chukotka. The burial of organic matter in the sedimentary rock of the Tanyurer Formation is associated with deflationary processes during the period of activation of volcanic activity. On the drained volcanic plateau of soil formation, a sod humus-accumulative process prevailed under the steppe vegetation. Humic substance dispersed in sedimentary rock was represented by a group of humins resistant to microbial decomposition. As a result of exposure to high pressures and temperatures, the colloidal form of humus was transformed into kerogen. Organic compounds (cellulose, lignin) in the plant tissue of buried tree trunks were replaced by silicon compounds. Weathering processes have affected the thin surface layer of dense sedimentary rock. Under the influence of the temperature and humidity gradient, loosening of loose rock and disintegration of clots of colloidal forms of humus occurred.</jats:p> Organic matter of sediments of South Chukotka E3S Web of Conferences
spellingShingle Aparin, Boris, Grabovsky, Alexander, Sukhacheva, Elena, Mingareeva, Elena, Janson, Svetlana, Shevchuk, Evgeny, Terleev, Vitaly, Nikonorov, Aleksandr, Akimov, Luka, E3S Web of Conferences, Organic matter of sediments of South Chukotka, Pulmonary and Respiratory Medicine, Pediatrics, Perinatology, and Child Health
title Organic matter of sediments of South Chukotka
title_full Organic matter of sediments of South Chukotka
title_fullStr Organic matter of sediments of South Chukotka
title_full_unstemmed Organic matter of sediments of South Chukotka
title_short Organic matter of sediments of South Chukotka
title_sort organic matter of sediments of south chukotka
title_unstemmed Organic matter of sediments of South Chukotka
topic Pulmonary and Respiratory Medicine, Pediatrics, Perinatology, and Child Health
url http://dx.doi.org/10.1051/e3sconf/202015702016