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<dc:title xml:lang="en"><![CDATA[Pine litter fall and decay rates along N-S transect]]></dc:title>
<dc:title xml:lang="en"><![CDATA[Patterns of pine ecosystem response to climate on a boreal-temperate transect]]></dc:title>
<dc:title xml:lang="en"><![CDATA[Rate of change of pine litter fall and decay in response to changing climate along N-S transect]]></dc:title>
<dc:title xml:lang="pl"><![CDATA[Pine litter fall and decay rates along N-S transect]]></dc:title>
<dc:title xml:lang="pl"><![CDATA[Patterns of pine ecosystem response to climate on a boreal-temperate transect]]></dc:title>
<dc:title xml:lang="pl"><![CDATA[Rate of change of pine litter fall and decay in response to changing climate along N-S transect]]></dc:title>
<dc:creator><![CDATA[Breymeyer, Alicja]]></dc:creator>
<dc:subject xml:lang="en"><![CDATA[pine ecosystem transect study]]></dc:subject>
<dc:subject xml:lang="en"><![CDATA[litter fall/decay]]></dc:subject>
<dc:subject xml:lang="en"><![CDATA[decomposition]]></dc:subject>
<dc:subject xml:lang="en"><![CDATA[climate change]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[pine ecosystem transect study]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[litter fall/decay]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[decomposition]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[climate change]]></dc:subject>
<dc:description xml:lang="en"><![CDATA[Pages 553-555, 2 pages of plates : illustrations ; 27 cm]]></dc:description>
<dc:description xml:lang="en"><![CDATA[Bibliographical references (page 555)]]></dc:description>
<dc:description xml:lang="en"><![CDATA[The response of pine ecosystems to changing latitude and thermoclimate in Central/Northern Europe was investigated through the measurements of rates of two ecosystem processes: organic matter (litter) production and decomposition. Studies were carried out at nine sites of pine and mixed pine forests placed along the N-S transect of about 2000 km crossing Finland, Estonia, Latvia, Lithuania and Poland. Warmer climates were observed with movement to southern sites; the coefficient of determination (R2) between annual long-term temperature and latitude was at the level of 0.99. The rates of change of both processes were compared in terms of relative increment per 1°C of long-term temperature and per -1° of latitude, and expressed in %. Litter production responds stronger to the southward change of climate: the fall of litter is 18-19% greater per +1°C of average annual temperature and by 8% greater per each -1° of latitude, compared to the decomposition process, which was accelerated at the rate of 9-l2% per 1°C and 4-5% per -1° of latitude. These results are summarized by the statement that in pine ecosystems the OM Production Sub-system is more sensitive to change of climate than the Sub-system of OM Decay, which is more conservative.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Strony 553-555, 2 strony tablic : ilustracje ; 27 cm]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Bibliografia na stronie 555]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[The response of pine ecosystems to changing latitude and thermoclimate in Central/Northern Europe was investigated through the measurements of rates of two ecosystem processes: organic matter (litter) production and decomposition. Studies were carried out at nine sites of pine and mixed pine forests placed along the N-S transect of about 2000 km crossing Finland, Estonia, Latvia, Lithuania and Poland. Warmer climates were observed with movement to southern sites; the coefficient of determination (R2) between annual long-term temperature and latitude was at the level of 0.99. The rates of change of both processes were compared in terms of relative increment per 1°C of long-term temperature and per -1° of latitude, and expressed in %. Litter production responds stronger to the southward change of climate: the fall of litter is 18-19% greater per +1°C of average annual temperature and by 8% greater per each -1° of latitude, compared to the decomposition process, which was accelerated at the rate of 9-l2% per 1°C and 4-5% per -1° of latitude. These results are summarized by the statement that in pine ecosystems the OM Production Sub-system is more sensitive to change of climate than the Sub-system of OM Decay, which is more conservative.]]></dc:description>
<dc:publisher><![CDATA[Polish Academy of Sciences. Institute of Ecology. Publishing Office]]></dc:publisher>
<dc:contributor><![CDATA[Polish Academy of Sciences. Institute of Ecology]]></dc:contributor>
<dc:date><![CDATA[2003]]></dc:date>
<dc:type xml:lang="en"><![CDATA[Text]]></dc:type>
<dc:type xml:lang="pl"><![CDATA[Tekst]]></dc:type>
<dc:identifier><![CDATA[https://rcin.org.pl/miiz/dlibra/publication/91649/edition/117569/content]]></dc:identifier>
<dc:identifier><![CDATA[oai:rcin.org.pl:117569]]></dc:identifier>
<dc:source xml:lang="en"><![CDATA[MiIZ PAN, call no. P.2840]]></dc:source>
<dc:source xml:lang="en"><![CDATA[http://katalog.pan.pl/webpac-bin/228bmiizPL/wgbroker.exe?new+-access+top+search+open+NR+kz2006002718]]></dc:source>
<dc:source xml:lang="pl"><![CDATA[MiIZ PAN, sygn. P.2840]]></dc:source>
<dc:source xml:lang="pl"><![CDATA[http://katalog.pan.pl/webpac-bin/228bmiizPL/wgbroker.exe?new+-access+top+search+open+NR+kz2006002718]]></dc:source>
<dc:language><![CDATA[eng]]></dc:language>
<dc:relation><![CDATA[Polish Journal of Ecology]]></dc:relation>
<dc:relation><![CDATA[Breymeyer A. 2003a - Pine ecosystem response to warming along North-South climatic transect in Europe: Presentation of research project - Pol. J. Ecol. 51 , 4: 403-411.]]></dc:relation>
<dc:relation><![CDATA[Breymeyer A. 2003b - Processes of litter fall and decomposition: boreal-temperate transect studies ofpine ecosystems - Pol. J. Ecol. 51 , 4: 529-543.]]></dc:relation>
<dc:relation><![CDATA[Degórski M. 2003 - Morpholithological genesis and soil properties of the pine forest ecosystems in relation to the North-South transect in Europe - Pol. J. Ecol. 51,4: 441-459.]]></dc:relation>
<dc:relation><![CDATA[Solon J. 2003 - Scots pine forests of the Vaccinio-Piceetea class in Europe: forest sites studied - Pol. J. Ecol. 51,4:421-439.]]></dc:relation>
<dc:relation><![CDATA[Nagel L. M., Vucetich J. A., Reed D. D., Mroz G. D., Parn H. 2003 - Woody biomass and annual production across a latitudinal gradient in northern Scots pine (Pinus sylvestris) forests. - Pol. J. Ecol. 51,4:471-479]]></dc:relation>
<dc:relation><![CDATA[oai:rcin.org.pl:publication:91649]]></dc:relation>
<dc:rights xml:lang="en"><![CDATA[Creative Commons Attribution BY 3.0 PL license]]></dc:rights>
<dc:rights xml:lang="pl"><![CDATA[Licencja Creative Commons Uznanie autorstwa 3.0 Polska]]></dc:rights>
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