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Journal ArticleDOI

Respiration as the main determinant of carbon balance in European forests

TLDR
Data of net ecosystem carbon exchange, collected between 1996 and 1998 from 15 European forests, confirm that many European forest ecosystems act as carbon sinks and indicate that, in general, ecosystem respiration determines netcosystem carbon exchange.
Abstract
Carbon exchange between the terrestrial biosphere and the atmosphere is one of the key processes that need to be assessed in the context of the Kyoto Protocol1. Several studies suggest that the terrestrial biosphere is gaining carbon2,3,4,5,6,7,8, but these estimates are obtained primarily by indirect methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange, collected between 1996 and 1998 from 15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines net ecosystem carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference vegetation index or estimates based on forest inventories may not be sufficient.

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Journal ArticleDOI

Plumbing the Global Carbon Cycle: Integrating Inland Waters into the Terrestrial Carbon Budget

TL;DR: In this paper, the role of inland water ecosystems in the global carbon cycle has been investigated and it is shown that roughly twice as much C enters inland aquatic systems from land as is exported from land to the sea, roughly equally as inorganic and organic carbon.
Journal ArticleDOI

Effects of Size and Temperature on Metabolic Rate

TL;DR: A general model is derived, based on principles of biochemical kinetics and allometry, that characterizes the effects of temperature and body mass on metabolic rate of microbes, ectotherms, endotherms (including those in hibernation), and plants in temperatures ranging from 0° to 40°C.
Book

Principles of Terrestrial Ecosystem Ecology

TL;DR: In this paper, the Ecosystem Concept is used to describe the Earth's Climate System and Geology and Soils, and the ecosystem concept is used for managing and sustaining ecosystems.
References
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Book

Biogeochemistry : An Analysis of Global Change

TL;DR: In this paper, the authors present a perspective of the global cycle of nitrogen and phosphorous, the global water cycle, and the global sulfur cycle from a global point of view.
Journal ArticleDOI

Increased plant growth in the northern high latitudes from 1981 to 1991

TL;DR: In this paper, the authors present evidence from satellite data that the photosynthetic activity of terrestrial vegetation increased from 1981 to 1991 in a manner that is suggestive of an increase in plant growth associated with a lengthening of the active growing season.
Journal ArticleDOI

Carbon pools and flux of global forest ecosystems.

TL;DR: Slowing deforestation, combined with an increase in forestation and other management measures to improve forest ecosystem productivity, could conserve or sequester significant quantities of carbon.
Journal ArticleDOI

Soil carbon pools and world life zones

TL;DR: In this article, an analysis of 2,700 soil profiles, organized on a climate basis using the Holdridge life-zone classification system, indicates relationships between soil carbon density and climate, a major soil forming factor.
Journal ArticleDOI

The temperature dependence of soil organic matter decomposition, and the effect of global warming on soil organic C storage

TL;DR: In this article, the authors surveyed the literature to obtain the temperature dependencies of soil respiration and N dynamics reported in different studies and found that the sensitivity of decomposition processes to temperature has been observed at low temperatures, whereas the sensitivity became more similar at higher temperatures.
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