2005年6月
Ecosystem development and carbon cycle on a glacier foreland in the high Arctic, Ny-Alesund, Svalbard
JOURNAL OF PLANT RESEARCH
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- 巻
- 118
- 号
- 3
- 開始ページ
- 173
- 終了ページ
- 179
- 記述言語
- 英語
- 掲載種別
- 研究論文(学術雑誌)
- DOI
- 10.1007/s10265-005-0211-9
- 出版者・発行元
- SPRINGER TOKYO
The Arctic terrestrial ecosystem is thought to be extremely susceptible to climate change. However, because of the diverse responses of ecosystem components to change. an overall response of the ecosystem carbon cycle to climate change is still hard to predict. In this review, we focus on several recent studies conducted to clarify the pattern of the carbon cycle on the deglaciated area of Ny-angstrom lesund. Svalbard in the high Arctic. Vegetation cover and soil carbon pools tended to increase with the progress of succession. However, even in the latter stages of succession, the size of the soil carbon pool was much smaller than those reported for the low Arctic tundra. Cryptogams contributed the major proportion of phytomass in the later stages. However, because of water limitation, their net primary production was smaller than that of the vascular plants. The compartment model that incorporated major carbon pools and flows suggested that the ecosystem of the later stages is likely to be a net sink of carbon at least for the summer season. Based on the eco-physiological characteristics of the major ecosystem components, we suggest several possible scenarios of future changes in the ecosystem carbon cycle.
- リンク情報
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- DOI
- https://doi.org/10.1007/s10265-005-0211-9
- CiNii Articles
- http://ci.nii.ac.jp/naid/10016578447
- PubMed
- https://www.ncbi.nlm.nih.gov/pubmed/15917988
- Web of Science
- https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000230362600002&DestApp=WOS_CPL
- ID情報
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- DOI : 10.1007/s10265-005-0211-9
- ISSN : 0918-9440
- CiNii Articles ID : 10016578447
- PubMed ID : 15917988
- Web of Science ID : WOS:000230362600002