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Sedimentation and Accumulation of Elements in the Vydrino Peat Bog (Southern Baikal Region). / Bogush, A. A.; Bobrov, V. A.; Klimin, M. A. et al.

In: Russian Geology and Geophysics, Vol. 60, No. 2, 02.2019, p. 163-175.

Research output: Contribution to journal › Article › peer-review

Harvard

Bogush, AA, Bobrov, VA, Klimin, MA, Bychinskii, VA, Leonova, GA, Krivonogov, SK, Kondrat'eva, LM & Preis, YI 2019, 'Sedimentation and Accumulation of Elements in the Vydrino Peat Bog (Southern Baikal Region)', Russian Geology and Geophysics, vol. 60, no. 2, pp. 163-175. https://doi.org/10.15372/RGG2019012

APA

Bogush, A. A., Bobrov, V. A., Klimin, M. A., Bychinskii, V. A., Leonova, G. A., Krivonogov, S. K., Kondrat'eva, L. M., & Preis, Y. I. (2019). Sedimentation and Accumulation of Elements in the Vydrino Peat Bog (Southern Baikal Region). Russian Geology and Geophysics, 60(2), 163-175. https://doi.org/10.15372/RGG2019012

Vancouver

Bogush AA, Bobrov VA, Klimin MA, Bychinskii VA, Leonova GA, Krivonogov SK et al. Sedimentation and Accumulation of Elements in the Vydrino Peat Bog (Southern Baikal Region). Russian Geology and Geophysics. 2019 Feb;60(2):163-175. doi: 10.15372/RGG2019012

Author

Bogush, A. A. ; Bobrov, V. A. ; Klimin, M. A. et al. / Sedimentation and Accumulation of Elements in the Vydrino Peat Bog (Southern Baikal Region). In: Russian Geology and Geophysics. 2019 ; Vol. 60, No. 2. pp. 163-175.

BibTeX

@article{89d4d146f05b4c80b2aab24ede38ea7f,
title = "Sedimentation and Accumulation of Elements in the Vydrino Peat Bog (Southern Baikal Region)",
abstract = "The evolution of peat deposits of the Vydrino bog (southern Baikal region) and concentration of elements in them are discussed. The bog peat massif more than 4 m in thickness formed mostly during the Holocene. The beginning of peat formation dates back to the late Allerod (13.1 ka). At present, the Vydrino bog is a biogeocoenosis of the high-moor type with a transitional peat deposit. We have established that the bog nonuniformly accumulated chemical elements during its formation. Concentration of Pb, Sn, Cd, Zn, and Sb in recent vegetation and in the upper layer of the peat bog is mainly due to forest fires and anthropogenic air pollution. The anomalous enrichment of peat with Zn and Cu in the Early Holocene (12.1-8.8 ka) horizons proceeded through the periodic inflow of thermal groundwater into the bottom part of the peat deposit. Authigenic Zn and Cu sulfides formed on the inner membrane of the cell wall of sphagnum moss. Geochemical modeling has shown that Zn and Cu sulfides can form abiotically.",
keywords = "peat bog, concentration of elements, genesis, rate of peat accumulation, pigment profile, geochemical modeling, Holocene, East Siberia, ATMOSPHERIC LEAD, JURA MOUNTAINS, DEPOSITION, PB, ZR, TI",
author = "Bogush, {A. A.} and Bobrov, {V. A.} and Klimin, {M. A.} and Bychinskii, {V. A.} and Leonova, {G. A.} and Krivonogov, {S. K.} and Kondrat'eva, {L. M.} and Preis, {Yu. I.}",
year = "2019",
month = feb,
doi = "10.15372/RGG2019012",
language = "English",
volume = "60",
pages = "163--175",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "2",

}

RIS

TY - JOUR

T1 - Sedimentation and Accumulation of Elements in the Vydrino Peat Bog (Southern Baikal Region)

AU - Bogush, A. A.

AU - Bobrov, V. A.

AU - Klimin, M. A.

AU - Bychinskii, V. A.

AU - Leonova, G. A.

AU - Krivonogov, S. K.

AU - Kondrat'eva, L. M.

AU - Preis, Yu. I.

PY - 2019/2

Y1 - 2019/2

N2 - The evolution of peat deposits of the Vydrino bog (southern Baikal region) and concentration of elements in them are discussed. The bog peat massif more than 4 m in thickness formed mostly during the Holocene. The beginning of peat formation dates back to the late Allerod (13.1 ka). At present, the Vydrino bog is a biogeocoenosis of the high-moor type with a transitional peat deposit. We have established that the bog nonuniformly accumulated chemical elements during its formation. Concentration of Pb, Sn, Cd, Zn, and Sb in recent vegetation and in the upper layer of the peat bog is mainly due to forest fires and anthropogenic air pollution. The anomalous enrichment of peat with Zn and Cu in the Early Holocene (12.1-8.8 ka) horizons proceeded through the periodic inflow of thermal groundwater into the bottom part of the peat deposit. Authigenic Zn and Cu sulfides formed on the inner membrane of the cell wall of sphagnum moss. Geochemical modeling has shown that Zn and Cu sulfides can form abiotically.

AB - The evolution of peat deposits of the Vydrino bog (southern Baikal region) and concentration of elements in them are discussed. The bog peat massif more than 4 m in thickness formed mostly during the Holocene. The beginning of peat formation dates back to the late Allerod (13.1 ka). At present, the Vydrino bog is a biogeocoenosis of the high-moor type with a transitional peat deposit. We have established that the bog nonuniformly accumulated chemical elements during its formation. Concentration of Pb, Sn, Cd, Zn, and Sb in recent vegetation and in the upper layer of the peat bog is mainly due to forest fires and anthropogenic air pollution. The anomalous enrichment of peat with Zn and Cu in the Early Holocene (12.1-8.8 ka) horizons proceeded through the periodic inflow of thermal groundwater into the bottom part of the peat deposit. Authigenic Zn and Cu sulfides formed on the inner membrane of the cell wall of sphagnum moss. Geochemical modeling has shown that Zn and Cu sulfides can form abiotically.

KW - peat bog

KW - concentration of elements

KW - genesis

KW - rate of peat accumulation

KW - pigment profile

KW - geochemical modeling

KW - Holocene

KW - East Siberia

KW - ATMOSPHERIC LEAD

KW - JURA MOUNTAINS

KW - DEPOSITION

KW - PB

KW - ZR

KW - TI

U2 - 10.15372/RGG2019012

DO - 10.15372/RGG2019012

M3 - Article

VL - 60

SP - 163

EP - 175

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 2

ER -

ID: 23292096