Dynamics of soil carbon following destruction of tropical rainforest and the subsequent establishment ofImperatagrassland in Indonesian Borneo using stable carbon isotopes-Reference-Cited by-同舟云学术

Dynamics of soil carbon following destruction of tropical rainforest and the subsequent establishment ofImperatagrassland in Indonesian Borneo using stable carbon isotopes

Published:2012-05-18 Issue:8 Volume:18 Page:2606-2616
ISSN:1354-1013
Container-title:Global Change Biology
language:en
Short-container-title:Glob Change Biol

Author:

Yonekura Yusuke¹,Ohta Seiichi¹,Kiyono Yoshiyuki²,Aksa Darul³,Morisada Kazuhito²,Tanaka Nagaharu²,Tayasu Ichiro⁴

Affiliation:

1. Laboratory of Tropical Forest Resources & Environments; Graduate School of Agriculture; Kyoto University; Kitashirakawa Oiwake-cho, Sakyo-ku; Kyoto; 606-8502; Japan

2. Forestry and Forest Products Research Institute; Matsunosato 1, Tsukuba; Ibaraki; 305-8687; Japan

3. Tropical Rain Forest Research Centre; Mulawarman University; Kampus Gunung Kelua, Jl. Kihajar Dewantara; Samarinda; 75123; East Kalimantan; Indonesia

4. Centre for Ecological Research; Kyoto University; 2-509-3 Hirano, Otsu; Shiga; 520-2113; Japan

Publisher

Wiley

Subject

General Environmental Science,Ecology,Environmental Chemistry,Global and Planetary Change

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2486.2012.02722.x/fullpdf

Reference43 articles.

1. Modelling organic carbon turnover in cleared temperate forest soils converted to maize cropping by using 13C natural abundance measurements;Arrouays;Plant and Soil,1995

2. The use of stable carbon isotopes for estimating soil organic matter turnover rates;Bernoux;Geoderma,1998

3. Changes in Organic Matter in an Oxisol from the Central Amazonian Forest During Eight Years as Pasture, Determined by 13C Isotopic Composition

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