<abstract xml:lang="en" xmlns="http://www.w3.org/1999/xhtml">We present results from an analysis of tree ring width and stable carbon and oxygen isotopes in tree ring cellulose of Siberian Spruce collected from remote forest islands in the northwestern Russian tundra. Ring width is often considered a proxy for summer temperatures. The aim of this pilot study was to test whether stable isotopes can provide additional information about climate during the growth of trees in this extreme environment. Comparison of δ13C and δ18O with observed meteorological data shows that there is a link between stable isotopes and winter precipitation. This may be explained by the strong influence that snow exerts on the isotopic composition of soil moisture during spring and early summer, when the new cellulose is formed. Our results show that winter precipitation in the study area was increasing from 1865-1900, and thereafter decreasing until ~ 1930. The 1960-1980 period was again rather humid, followed by a drying trend until 1990. The study highlights the potential of stable carbon and oxygen isotopes in tree rings as proxies for winter precipitation.</abstract>

We present results from an analysis of tree ring width and stable carbon and oxygen isotopes in tree ring cellulose of Siberian Spruce collected from remote forest islands in the northwestern Russian tundra. Ring width is often considered a proxy for summer temperatures. The aim of this pilot study was to test whether stable isotopes can provide additional information about climate during the growth of trees in this extreme environment. Comparison of δ13C and δ18O with observed meteorological data shows that there is a link between stable isotopes and winter precipitation. This may be explained by the strong influence that snow exerts on the isotopic composition of soil moisture during spring and early summer, when the new cellulose is formed. Our results show that winter precipitation in the study area was increasing from 1865-1900, and thereafter decreasing until ~ 1930. The 1960-1980 period was again rather humid, followed by a drying trend until 1990. The study highlights the potential of stable carbon and oxygen isotopes in tree rings as proxies for winter precipitation.

Stable Isotopes in Tree Rings as Proxies for Winter Precipitation Changes in the Russian Arctic over the Past 150 Years

Department of Physical Geography and Quaternary Geology, Stockholm University, 10691 Stockholm, Sweden

Department of Geology, University of Helsinki, P.O.Box 64, Gustaf Hällströmin katu 2a, FI-00014 University of Helsinki, Finland

Radiocarbon Dating Laboratory, University of Helsinki, P.O.Box 64, Gustaf Hällströmin katu 2a, FI-00014 University of Helsinki, Finland

Geochronometria

We present results from an analysis of tree ring width and stable carbon and oxygen isotopes in tree ring cellulose of Siberian Spruce collected from remote...

Stable Isotopes in Tree Rings as Proxies for Winter Precipitation Changes in the Russian Arctic over the Past 150 Years

Publicado en línea: 27 mar 2009

Páginas: 37 - 46

DOI: https://doi.org/10.2478/v10003-008-0025-6

Palabras clave
tree rings, stable isotopes, Russian Arctic

This content is open access.

Stable Isotopes in Tree Rings as Proxies for Winter Precipitation Changes in the Russian Arctic over the Past 150 Years

Publicado en línea: 27 mar 2009

Páginas: 37 - 46

DOI: https://doi.org/10.2478/v10003-008-0025-6

Palabras clavetree rings, stable isotopes, Russian Arctic

This content is open access.

Palabras clave
tree rings, stable isotopes, Russian Arctic