Levels of biogenic-abiogenic interaction and structural organization of soils and soil-like bodies in Antarctica

Aleksei V. Lupachev, Stanislav V. Gubin, Evgeny V. Abakumov

Результат исследований: Публикации в книгах, отчётах, сборниках, трудах конференцийглава/раздел

Выдержка

Pedogenic processes of transformation and accumulation of organogenic matter and its interaction with the mineral matrix of the soils are very poor-expressed in Antarctica. Very often, these processes show up in a very special ways that can rarely be observed in the well-studied soils of moderate latitudes and even in the northern polar environments. The majority of the Antarctic soils do not develop well-expressed uppermost organomineral horizons. Mostly they are presented with the poorly aggregated mix of mosses’ and lichens’ detritus with the coarse-textured debris and rarely show macromorphological evidences of biogenic-abiogenic interaction. Using of state-of-the-art modern methods of soil science (scanning electron microscopy, micro- and mesomorphological analysis etc.) along with the regular methods of morphological analysis of soil profiles and spatial analysis of the soil cover allow distinguishing different levels of the structural organization of soils in the Antarctic region. The fine earth adhesion, forming of the organomineral coatings and films, deep alteration of primary minerals and ornithogenic impact on the soil material and profile structure is evident at all the studied levels of soil organization. Their manifestation degree rises from the continental Antarctica to the Subantarctic regions and from the soil-like bodies with no or very poor-expressed vegetation to the soils with relatively well-developed uppermost organo-horizons.

Язык оригиналаанглийский
Название основной публикацииProcesses and Phenomena on the Boundary Between Biogenic and Abiogenic Nature
Подзаголовок основной публикацииConference proceedings
РедакторыOlga V. Frank-Kamenetskaya, Dmitry Yu. Vlasov, Elena G. Panova, Sofia N. Lessovaia
Место публикацииCham
ИздательSpringer
Страницы481-500
Число страниц20
ISBN (электронное издание)9783030216146
ISBN (печатное издание)9783030216139
DOI
СостояниеОпубликовано - 2020
СобытиеVI International Symposium "Biogenic-abiogenic interactions in natural and anthropogenic systems" devoted to the 150th anniversary of the Saint Petersburg Naturalists Society - СПбГУ, Санкт-Петербург, Российская Федерация
Продолжительность: 24 сен 201827 сен 2018
Номер конференции: VI

Серия публикаций

НазваниеLecture Notes in Earth System Sciences
ISSN (печатное издание)2193-8571
ISSN (электронное издание)2193-858X

Конференция

КонференцияVI International Symposium "Biogenic-abiogenic interactions in natural and anthropogenic systems" devoted to the 150th anniversary of the Saint Petersburg Naturalists Society
СтранаРоссийская Федерация
ГородСанкт-Петербург
Период24/09/1827/09/18

Отпечаток

Soils
soil
subantarctic region
Antarctica
Minerals
soil cover
mineral
soil science
adhesion
spatial analysis
lichen
moss
detritus
soil profile
coating
scanning electron microscopy
Debris
matrix
Adhesion
vegetation

Предметные области Scopus

  • Компьютерные технологии в науках о земле
  • Планетоведение и науки о земле (все)

Цитировать

Lupachev, A. V., Gubin, S. V., & Abakumov, E. V. (2020). Levels of biogenic-abiogenic interaction and structural organization of soils and soil-like bodies in Antarctica. В O. V. Frank-Kamenetskaya, D. Y. Vlasov, E. G. Panova, & S. N. Lessovaia (Ред.), Processes and Phenomena on the Boundary Between Biogenic and Abiogenic Nature: Conference proceedings (стр. 481-500). (Lecture Notes in Earth System Sciences). Cham: Springer. https://doi.org/10.1007/978-3-030-21614-6_26
Lupachev, Aleksei V. ; Gubin, Stanislav V. ; Abakumov, Evgeny V. / Levels of biogenic-abiogenic interaction and structural organization of soils and soil-like bodies in Antarctica. Processes and Phenomena on the Boundary Between Biogenic and Abiogenic Nature: Conference proceedings. редактор / Olga V. Frank-Kamenetskaya ; Dmitry Yu. Vlasov ; Elena G. Panova ; Sofia N. Lessovaia. Cham : Springer, 2020. стр. 481-500 (Lecture Notes in Earth System Sciences).
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Lupachev, AV, Gubin, SV & Abakumov, EV 2020, Levels of biogenic-abiogenic interaction and structural organization of soils and soil-like bodies in Antarctica. в OV Frank-Kamenetskaya, DY Vlasov, EG Panova & SN Lessovaia (ред.), Processes and Phenomena on the Boundary Between Biogenic and Abiogenic Nature: Conference proceedings. Lecture Notes in Earth System Sciences, Springer, Cham, стр. 481-500, VI International Symposium "Biogenic-abiogenic interactions in natural and anthropogenic systems" devoted to the 150th anniversary of the Saint Petersburg Naturalists Society, Санкт-Петербург, Российская Федерация, 24/09/18. https://doi.org/10.1007/978-3-030-21614-6_26

Levels of biogenic-abiogenic interaction and structural organization of soils and soil-like bodies in Antarctica. / Lupachev, Aleksei V.; Gubin, Stanislav V.; Abakumov, Evgeny V.

Processes and Phenomena on the Boundary Between Biogenic and Abiogenic Nature: Conference proceedings. ред. / Olga V. Frank-Kamenetskaya; Dmitry Yu. Vlasov; Elena G. Panova; Sofia N. Lessovaia. Cham : Springer, 2020. стр. 481-500 (Lecture Notes in Earth System Sciences).

Результат исследований: Публикации в книгах, отчётах, сборниках, трудах конференцийглава/раздел

TY - CHAP

T1 - Levels of biogenic-abiogenic interaction and structural organization of soils and soil-like bodies in Antarctica

AU - Lupachev, Aleksei V.

AU - Gubin, Stanislav V.

AU - Abakumov, Evgeny V.

PY - 2020

Y1 - 2020

N2 - Pedogenic processes of transformation and accumulation of organogenic matter and its interaction with the mineral matrix of the soils are very poor-expressed in Antarctica. Very often, these processes show up in a very special ways that can rarely be observed in the well-studied soils of moderate latitudes and even in the northern polar environments. The majority of the Antarctic soils do not develop well-expressed uppermost organomineral horizons. Mostly they are presented with the poorly aggregated mix of mosses’ and lichens’ detritus with the coarse-textured debris and rarely show macromorphological evidences of biogenic-abiogenic interaction. Using of state-of-the-art modern methods of soil science (scanning electron microscopy, micro- and mesomorphological analysis etc.) along with the regular methods of morphological analysis of soil profiles and spatial analysis of the soil cover allow distinguishing different levels of the structural organization of soils in the Antarctic region. The fine earth adhesion, forming of the organomineral coatings and films, deep alteration of primary minerals and ornithogenic impact on the soil material and profile structure is evident at all the studied levels of soil organization. Their manifestation degree rises from the continental Antarctica to the Subantarctic regions and from the soil-like bodies with no or very poor-expressed vegetation to the soils with relatively well-developed uppermost organo-horizons.

AB - Pedogenic processes of transformation and accumulation of organogenic matter and its interaction with the mineral matrix of the soils are very poor-expressed in Antarctica. Very often, these processes show up in a very special ways that can rarely be observed in the well-studied soils of moderate latitudes and even in the northern polar environments. The majority of the Antarctic soils do not develop well-expressed uppermost organomineral horizons. Mostly they are presented with the poorly aggregated mix of mosses’ and lichens’ detritus with the coarse-textured debris and rarely show macromorphological evidences of biogenic-abiogenic interaction. Using of state-of-the-art modern methods of soil science (scanning electron microscopy, micro- and mesomorphological analysis etc.) along with the regular methods of morphological analysis of soil profiles and spatial analysis of the soil cover allow distinguishing different levels of the structural organization of soils in the Antarctic region. The fine earth adhesion, forming of the organomineral coatings and films, deep alteration of primary minerals and ornithogenic impact on the soil material and profile structure is evident at all the studied levels of soil organization. Their manifestation degree rises from the continental Antarctica to the Subantarctic regions and from the soil-like bodies with no or very poor-expressed vegetation to the soils with relatively well-developed uppermost organo-horizons.

KW - Antarctica

KW - Cryosols

KW - Leptosols

KW - Micromorphological analysis

KW - Scanning electron microscopy

KW - Soils

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Lupachev AV, Gubin SV, Abakumov EV. Levels of biogenic-abiogenic interaction and structural organization of soils and soil-like bodies in Antarctica. В Frank-Kamenetskaya OV, Vlasov DY, Panova EG, Lessovaia SN, редакторы, Processes and Phenomena on the Boundary Between Biogenic and Abiogenic Nature: Conference proceedings. Cham: Springer. 2020. стр. 481-500. (Lecture Notes in Earth System Sciences). https://doi.org/10.1007/978-3-030-21614-6_26