CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS

Variability of width, maximum density and stable isotopes (δ13C) in tree-rings of Scots pine (Pinus sylvestris L.) were studied in Northern Caucasus. Statistically sufficient agreements between ring width chronologies allow to construct composite chronology for the Elbrus area. Absence or low correl...

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Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Authors: Enrico Brugnoli, Olga Solomina, Luciano Spaccino, Ekaterina Dolgova
Format: Article in Journal/Newspaper
Language:English
Published: Russian Geographical Society 2010
Subjects:
Scots pine;stable isotopes (δ13C);tree-ring width;tree-ring maximum density;Northern Caucasus
Antarctic and Alpine Research
Arctic
Online Access:https://ges.rgo.ru/jour/article/view/233
https://doi.org/10.24057/2071-9388-2010-3-4-4-16
id ftjges:oai:oai.gesj.elpub.ru:article/233
record_format openpolar
institution Open Polar
collection Geography, Environment, Sustainability (E-Journal)
op_collection_id ftjges
language English
topic Scots pine;stable isotopes (δ13C);tree-ring width;tree-ring maximum density;Northern Caucasus
spellingShingle Scots pine;stable isotopes (δ13C);tree-ring width;tree-ring maximum density;Northern Caucasus
Enrico Brugnoli
Olga Solomina
Luciano Spaccino
Ekaterina Dolgova
CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS
topic_facet Scots pine;stable isotopes (δ13C);tree-ring width;tree-ring maximum density;Northern Caucasus
description Variability of width, maximum density and stable isotopes (δ13C) in tree-rings of Scots pine (Pinus sylvestris L.) were studied in Northern Caucasus. Statistically sufficient agreements between ring width chronologies allow to construct composite chronology for the Elbrus area. Absence or low correlation between indices of the ring width and maximum density chronology point out different climatic signal. The influence of temperature and precipitation on these tree-ring parameters was also analyzed. The ring width of pine at the upper tree limit in the Baksan valley correlates positively with the June and July precipitation (r=0.3; 0.3; 0.4, p<0.05). No correlation with temperature parameters was found. The maximum density reflects the warm period temperature (April-October). The similarity in interannual variations of δ13C in annual rings between the individual samples means that their display a coherent common signal. This signal can be largely interpreted as the June and July precipitation.
format Article in Journal/Newspaper
author Enrico Brugnoli
Olga Solomina
Luciano Spaccino
Ekaterina Dolgova
author_facet Enrico Brugnoli
Olga Solomina
Luciano Spaccino
Ekaterina Dolgova
author_sort Enrico Brugnoli
title CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS
title_short CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS
title_full CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS
title_fullStr CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS
title_full_unstemmed CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS
title_sort climate signal in the ring width, density and carbon stable isotopes in pine (pinus silvestris l.) in central caucasus
publisher Russian Geographical Society
publishDate 2010
url https://ges.rgo.ru/jour/article/view/233
https://doi.org/10.24057/2071-9388-2010-3-4-4-16
genre Antarctic and Alpine Research
Arctic
genre_facet Antarctic and Alpine Research
Arctic
op_source GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY; Vol 3, No 4 (2010); 4-16
2542-1565
2071-9388
op_relation https://ges.rgo.ru/jour/article/view/233/230
Brugnoli, E., Farquhar, G.D. (2000). Photosynthetic fractionation of carbon isotopes. In: Photosynthesis
Physiology and Metabolism, Advances in Photosynthesis, eds R.C. Leegood, T.D.
Sharkey and S. von Caemmerer, Kluwer Academic Publishers, the Netherlands, pp. 399–434.
Cook E.R. (1985). A time series analysis approach to tree ring standardization // Ph. D.
dissertation. University of Arizona, Tucson, AZ. 171.
Cook E.R., Kairiukstis L.A. (1990). Methods of dendrochronology. Applications in the
Enviromental Sciences. Dordrecht; Boston, London, Kluwer Acad. Publ.
Dolgova E., Solomina O. (2010). The first quantitative reconstruction of warm period temperature
in Caucasus according to the tree-ring data. Doklady of Academy of Sciecnes.
№ 2, p. 1–5. (in Russian).
Feng X. and Epstein S. (1995). Climatic trends from isotopic records of tree rings: The
past 100–200 years. Climatic Change. Volume 33, Number 4, 551–562, DOI:10.1007/
BF00141704.
Gagen, M., McCarroll, D. (2004). Latewood Width, Maximum Density, and Stable Carbon
Isotope Ratios of Pine as Climate Indicators in a Dry Subalpine Environment, French Alps
Arctic, Antarctic, and Alpine Research, Vol. 36, No. 2, pp. 166–171.
Leavitt, S., and Long, A. (1988). Stable carbon isotope chronologies from trees in the southwestern
United States. Global Biochemical Cycles 2 (3), 189–198.
Leavitt, S.W. (1993). Environmental information from 13C/12C ratios of wood. Geophysical
Monographs 78, 325–331.
Liu, Y., Wu, X., Leavitt, S.W., Hughes, M.K. (1996). Stable carbon isotope in tree rings from
Huangling, China and climatic variation. Science in China D (39) 2, 152–161.
McCarroll D., Loader N.J. (2004). Stable isotopes in tree rings. Quaternary Science Reviews,
771–801
McCarroll, D., Pawellek, F. (2001). Stable carbon isotope ratios of Pinus sylvestris from
northern Finland and the potential for extracting a climate signal from long Fennoscandian
chronologies. The Holocene 11, 517–526.
McCarroll, D. Pettigrew, E. and Luckman A. (2002). Blue Reflectance Provides a Surrogatefor
Latewood Density of High-latitude Pine Tree Rings Arctic, Antarctic, and Alpine Research,
Vol. 34, No. 4, pp. 450–453.
McNulty, S. G., and Swank. W. T. (1995). Wood (delta)^(13) C as a Measure of Annual
Basal Area Growth and Soil Water Stress in a Pinus Strobus Forest. Ecology 76:1581–1586.
[doi:10.2307/1938159]
Schweingruber F.H. (1988). Tree rings: basics and applications of dendrochronology. Dordrecht,
Holland, RPC.
Shahgedanova, M. (2002). The Physical geography of Northern Eurasia, Oxford University
Press. 571.
Solomina, O.N. (1999). Mountain glaciation of Northern Eurasia in Holocene. Moscow,
Nauchny Mir. 264 pp. (in Russian).
Stokes M.A., Smiley T.L. (1968). An introduction to tree-ring dating. Tucson, The University
of Arizona Press.
Stuiver, M. (1978). Atmospheric carbon dioxide and carbon reservoir changes. Science
253–258.
Thomas, R.J. (1991). Wood: formation and morphology. In Lewin, M. and Goldstein, I.S.,
editors, Wood structure and composition, New York: Marcel Dekker Inc.
Turmanina V.I. (1979). Dendrochronology of avalanches in the upperstream of Baksan valley
valleys. Rhythms of Glacial Processes. Mosc. Gos. Univ., Moscow, pp. 128–134. (in Russian).
Waterhouse, J.S., Barker, A.C., Carter, A.H.C., Agafonov, L.I., Loader, N.J. (2000). Stable carbon
isotopes in Scots pine tree rings preserve a record of the flow of the river Ob. Geophysical
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spelling ftjges:oai:oai.gesj.elpub.ru:article/233 2023-05-15T14:14:42+02:00 CLIMATE SIGNAL IN THE RING WIDTH, DENSITY AND CARBON STABLE ISOTOPES IN PINE (PINUS SILVESTRIS L.) IN CENTRAL CAUCASUS Enrico Brugnoli Olga Solomina Luciano Spaccino Ekaterina Dolgova 2010-12-01 application/pdf https://ges.rgo.ru/jour/article/view/233 https://doi.org/10.24057/2071-9388-2010-3-4-4-16 eng eng Russian Geographical Society https://ges.rgo.ru/jour/article/view/233/230 Brugnoli, E., Farquhar, G.D. (2000). Photosynthetic fractionation of carbon isotopes. In: Photosynthesis Physiology and Metabolism, Advances in Photosynthesis, eds R.C. Leegood, T.D. Sharkey and S. von Caemmerer, Kluwer Academic Publishers, the Netherlands, pp. 399–434. Cook E.R. (1985). A time series analysis approach to tree ring standardization // Ph. D. dissertation. University of Arizona, Tucson, AZ. 171. Cook E.R., Kairiukstis L.A. (1990). Methods of dendrochronology. Applications in the Enviromental Sciences. Dordrecht; Boston, London, Kluwer Acad. Publ. Dolgova E., Solomina O. (2010). The first quantitative reconstruction of warm period temperature in Caucasus according to the tree-ring data. Doklady of Academy of Sciecnes. № 2, p. 1–5. (in Russian). Feng X. and Epstein S. (1995). Climatic trends from isotopic records of tree rings: The past 100–200 years. Climatic Change. Volume 33, Number 4, 551–562, DOI:10.1007/ BF00141704. Gagen, M., McCarroll, D. (2004). Latewood Width, Maximum Density, and Stable Carbon Isotope Ratios of Pine as Climate Indicators in a Dry Subalpine Environment, French Alps Arctic, Antarctic, and Alpine Research, Vol. 36, No. 2, pp. 166–171. Leavitt, S., and Long, A. (1988). Stable carbon isotope chronologies from trees in the southwestern United States. Global Biochemical Cycles 2 (3), 189–198. Leavitt, S.W. (1993). Environmental information from 13C/12C ratios of wood. Geophysical Monographs 78, 325–331. Liu, Y., Wu, X., Leavitt, S.W., Hughes, M.K. (1996). Stable carbon isotope in tree rings from Huangling, China and climatic variation. Science in China D (39) 2, 152–161. McCarroll D., Loader N.J. (2004). Stable isotopes in tree rings. Quaternary Science Reviews, 771–801 McCarroll, D., Pawellek, F. (2001). Stable carbon isotope ratios of Pinus sylvestris from northern Finland and the potential for extracting a climate signal from long Fennoscandian chronologies. The Holocene 11, 517–526. McCarroll, D. Pettigrew, E. and Luckman A. (2002). Blue Reflectance Provides a Surrogatefor Latewood Density of High-latitude Pine Tree Rings Arctic, Antarctic, and Alpine Research, Vol. 34, No. 4, pp. 450–453. McNulty, S. G., and Swank. W. T. (1995). Wood (delta)^(13) C as a Measure of Annual Basal Area Growth and Soil Water Stress in a Pinus Strobus Forest. Ecology 76:1581–1586. [doi:10.2307/1938159] Schweingruber F.H. (1988). Tree rings: basics and applications of dendrochronology. Dordrecht, Holland, RPC. Shahgedanova, M. (2002). The Physical geography of Northern Eurasia, Oxford University Press. 571. Solomina, O.N. (1999). Mountain glaciation of Northern Eurasia in Holocene. Moscow, Nauchny Mir. 264 pp. (in Russian). Stokes M.A., Smiley T.L. (1968). An introduction to tree-ring dating. Tucson, The University of Arizona Press. Stuiver, M. (1978). Atmospheric carbon dioxide and carbon reservoir changes. Science 253–258. Thomas, R.J. (1991). Wood: formation and morphology. In Lewin, M. and Goldstein, I.S., editors, Wood structure and composition, New York: Marcel Dekker Inc. Turmanina V.I. (1979). Dendrochronology of avalanches in the upperstream of Baksan valley valleys. Rhythms of Glacial Processes. Mosc. Gos. Univ., Moscow, pp. 128–134. (in Russian). Waterhouse, J.S., Barker, A.C., Carter, A.H.C., Agafonov, L.I., Loader, N.J. (2000). Stable carbon isotopes in Scots pine tree rings preserve a record of the flow of the river Ob. Geophysical Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal the right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors can enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgment of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).The information and opinions presented in the Journal reflect the views of the authors and not of the Journal or its Editorial Board or the Publisher. The GES Journal has used its best endeavors to ensure that the information is correct and current at the time of publication but takes no responsibility for any error, omission, or defect therein. Авторы, публикующие в данном журнале, соглашаются со следующим:Авторы сохраняют за собой авторские права на работу и предоставляют журналу право первой публикации работы на условиях лицензии Creative Commons Attribution License, которая позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Авторы сохраняют право заключать отдельные контрактные договорённости, касающиеся не-эксклюзивного распространения версии работы в опубликованном здесь виде (например, размещение ее в институтском хранилище, публикацию в книге), со ссылкой на ее оригинальную публикацию в этом журнале.Авторы имеют право размещать их работу CC-BY GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY; Vol 3, No 4 (2010); 4-16 2542-1565 2071-9388 Scots pine;stable isotopes (δ13C);tree-ring width;tree-ring maximum density;Northern Caucasus info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2010 ftjges https://doi.org/10.24057/2071-9388-2010-3-4-4-16 https://doi.org/10.2307/1938159 2021-05-21T07:34:48Z Variability of width, maximum density and stable isotopes (δ13C) in tree-rings of Scots pine (Pinus sylvestris L.) were studied in Northern Caucasus. Statistically sufficient agreements between ring width chronologies allow to construct composite chronology for the Elbrus area. Absence or low correlation between indices of the ring width and maximum density chronology point out different climatic signal. The influence of temperature and precipitation on these tree-ring parameters was also analyzed. The ring width of pine at the upper tree limit in the Baksan valley correlates positively with the June and July precipitation (r=0.3; 0.3; 0.4, p<0.05). No correlation with temperature parameters was found. The maximum density reflects the warm period temperature (April-October). The similarity in interannual variations of δ13C in annual rings between the individual samples means that their display a coherent common signal. This signal can be largely interpreted as the June and July precipitation. Article in Journal/Newspaper Antarctic and Alpine Research Arctic Geography, Environment, Sustainability (E-Journal) GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 3 4 4 16

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