首页 | 本学科首页   官方微博 | 高级检索  
   检索      


Notes towards an optimal sampling strategy in dendroclimatology
Institution:1. Department of Geography, University of Cambridge, CB2 3EN, UK;2. Sukachev Institute of Forest SB RAS, Krasnoyarsk, 660036, Russia;3. Institute of Ecology and Geography, Siberian Federal University, Krasnoyarsk, 660041, Russia;4. Global Change Research Institute CAS, 603 00 Brno, Czech Republic;5. Department of Wood Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, 613 00 Brno, Czech Republic;6. Department of Physical Geography, Stockholm University, SE-106 91 Stockholm, Sweden;7. Navarino Environmental Observatory, GR-24001 Messinia, Greece;8. North-Eastern Federal University, 58 Belinsky Street, Yakutsk, 677000, Russia;9. Melnikov Permafrost Institute, 36 Merzlotnaya Street, Yakutsk, 677010, Russia;10. Swiss Federal Research Institute WSL, CH-8903 Birmensdorf, Switzerland;11. Department of Geography, Masaryk University, 61137, Czech Republic;1. Department of Geography, Johannes Gutenberg University, Mainz, Germany;2. Department of Atmospheric and Environmental Sciences, University at Albany (SUNY), Albany, New York, USA;3. Dendroøkologen A.J. Kirchhefer, Tromsø, Norway;4. Natural Resources Institute Finland, Rovaniemi, Finland;5. Department of Physical Geography, Stockholm University, Stockholm, Sweden;6. Department of Geography, University of Cambridge, UK;7. Swiss Federal Research Institute WSL, Birmensdorf, Switzerland;8. Global Change Research Centre AS CR, Brno, Czech Republic;1. University of Vale do Rio dos Sinos (UNISINOS), Av. Unisinos, 950, Cristo Rei, 93022-750, São Leopoldo, RS, Brazil;2. Université de Lorraine, AgroParisTech, INRA, UMR Silva, 54000 Nancy, France;3. Coimbra University, Department of Life Sciences, Functional Ecology Center, Calçada Martim de Freitas, 3000, no 456, Coimbra, Portugal;4. University Trás-os-Montes e Alto Douro/CITAB, Forestry Department, Quinta de Prados, 5001-801, Vila Real, Portugal;5. Brazilian Agricultural Research Corporation (Embrapa), Embrapa Forestry, Estrada da Ribeira - Km 111, 83411-000, Colombo, PR, Brazil;1. Faculty of Forestry, Ștefan cel Mare University, Suceava, Romania;2. Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, Hungary;3. Stable Isotope Laboratory, Ștefan cel Mare University, Suceava, Romania;4. Departement of Geography, Johannes Gutenberg University, Mainz, Germany;5. Emil Racoviță Institute of Speleology, Romanian Academy, Cluj Napoca, Romania;6. Institute of Biology, Romanian Academy, Bucharest, Romania;7. Marin Dracea National Research and Development Institute for Silviculture, Câmpulung Moldovenesc, Romania;1. Siberian Federal University, 79 Svobodny pr., 660041 Krasnoyarsk, Russia;2. Khakass Technical Institute, Siberian Federal University, 27 Shchetinkina St., 655017, Abakan, Russia;3. Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Zuercherstrasse 111, CH-8903 Birmensdorf, Switzerland;4. V. N. Sukachev Institute of Forest, Siberian Branch of the Russian Academy of Sciences, Akademgorodok 50/28, Krasnoyarsk, 660036, Russia
Abstract:Though the extraction of increment cores is common practice in tree-ring research, there is no standard for the number of samples per tree, or trees per site needed to accurately describe the common growth pattern of a discrete population of trees over space and time. Tree-ring chronologies composed of living, subfossil and archaeological material often combine an uneven distribution of increment cores and disc samples. The effects of taking one or two cores per tree, or even the inclusion of multiple radii measurements from entire discs, on chronology development and quality remain unreported. Here, we present four new larch (Larix cajanderi Mayr) ring width chronologies from the same 20 trees in northeastern Siberia that have been independently developed using different combinations of core and disc samples. Our experiment reveals: i) sawing is much faster than coring, with the latter not always hitting the pith; ii) the disc-based chronology contains fewer locally absent rings, extends further back in time and exhibits more growth coherency; iii) although the sampling design has little impact on the overall chronology behaviour, lower frequency information is more robustly obtained from the disc measurements that also tend to reflect a slightly stronger temperature signal. In quantifying the influence of sampling strategy on the quality of tree-ring width chronologies, and their suitability for climate reconstructions, this study provides useful insights for optimizing fieldwork campaigns, as well as for developing composite chronologies from different wood sources.
Keywords:Sampling design  Disc samples  Increment cores  Climate signal  Northeastern Siberia  Locally absent rings
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号