Standard

C/N and δC13 patterns in lake sediments as a source of palaeoenvironmental information for the Mologa-Sheksna region (NW Russia). / Sadokov , D.O.; Knoblauch, Christian; Melles, M.; Mantke, Nicole; Lendt , R.

в: Limnology and Freshwater Biology, № 4, 2020, стр. 444-445.

Результаты исследований: Научные публикации в периодических изданияхстатья в журнале по материалам конференции

Harvard

Sadokov , DO, Knoblauch, C, Melles, M, Mantke, N & Lendt , R 2020, 'C/N and δC13 patterns in lake sediments as a source of palaeoenvironmental information for the Mologa-Sheksna region (NW Russia)', Limnology and Freshwater Biology, № 4, стр. 444-445.

APA

Sadokov , D. O., Knoblauch, C., Melles, M., Mantke, N., & Lendt , R. (2020). C/N and δC13 patterns in lake sediments as a source of palaeoenvironmental information for the Mologa-Sheksna region (NW Russia). Limnology and Freshwater Biology, (4), 444-445.

Vancouver

Sadokov DO, Knoblauch C, Melles M, Mantke N, Lendt R. C/N and δC13 patterns in lake sediments as a source of palaeoenvironmental information for the Mologa-Sheksna region (NW Russia). Limnology and Freshwater Biology. 2020;(4):444-445.

Author

Sadokov , D.O. ; Knoblauch, Christian ; Melles, M. ; Mantke, Nicole ; Lendt , R. / C/N and δC13 patterns in lake sediments as a source of palaeoenvironmental information for the Mologa-Sheksna region (NW Russia). в: Limnology and Freshwater Biology. 2020 ; № 4. стр. 444-445.

BibTeX

@article{47702a744b544f9cac0281c47cdfdef4,
title = "C/N and δC13 patterns in lake sediments as a source of palaeoenvironmental information for the Mologa-Sheksna region (NW Russia)",
abstract = "Organic geochemical proxies (δC13 and C/N) are used to infer changes of plant fossils sources in the sediments of relict mire lakes in Russia. The Pleistocene Holocene transition is described by δC13 and C/N used jointly. Shifts of C/N and δC13 give ideas for the lakes water level and composition of plant remains changes as a consequence of the regional climate alterations. Pre-Holocene cool period (Younger Drias) and preceding warm phase (Aller{\o}d) are supposedly traced in the lake sediments for the north of the Mologa-Sheksna Lowland.",
keywords = "lacustrine sedimentation, organic geochemistry, C/N ratios, δC13 signatures",
author = "D.O. Sadokov and Christian Knoblauch and M. Melles and Nicole Mantke and R. Lendt",
year = "2020",
language = "English",
pages = "444--445",
journal = "Limnology and Freshwater Biology",
issn = "2658-3518",
publisher = "Лимнологический институт Сибирского отделения Российской академии наук",
number = "4",
note = "null ; Conference date: 02-09-2020 Through 04-09-2020",
url = "http://www.lin.irk.ru/paleo2020/ru/",

}

RIS

TY - JOUR

T1 - C/N and δC13 patterns in lake sediments as a source of palaeoenvironmental information for the Mologa-Sheksna region (NW Russia)

AU - Sadokov , D.O.

AU - Knoblauch, Christian

AU - Melles, M.

AU - Mantke, Nicole

AU - Lendt , R.

PY - 2020

Y1 - 2020

N2 - Organic geochemical proxies (δC13 and C/N) are used to infer changes of plant fossils sources in the sediments of relict mire lakes in Russia. The Pleistocene Holocene transition is described by δC13 and C/N used jointly. Shifts of C/N and δC13 give ideas for the lakes water level and composition of plant remains changes as a consequence of the regional climate alterations. Pre-Holocene cool period (Younger Drias) and preceding warm phase (Allerød) are supposedly traced in the lake sediments for the north of the Mologa-Sheksna Lowland.

AB - Organic geochemical proxies (δC13 and C/N) are used to infer changes of plant fossils sources in the sediments of relict mire lakes in Russia. The Pleistocene Holocene transition is described by δC13 and C/N used jointly. Shifts of C/N and δC13 give ideas for the lakes water level and composition of plant remains changes as a consequence of the regional climate alterations. Pre-Holocene cool period (Younger Drias) and preceding warm phase (Allerød) are supposedly traced in the lake sediments for the north of the Mologa-Sheksna Lowland.

KW - lacustrine sedimentation

KW - organic geochemistry

KW - C/N ratios

KW - δC13 signatures

M3 - Conference article

SP - 444

EP - 445

JO - Limnology and Freshwater Biology

JF - Limnology and Freshwater Biology

SN - 2658-3518

IS - 4

Y2 - 2 September 2020 through 4 September 2020

ER -

ID: 92122138