Abstract

The carbon (C) pool in forest ecosystems plays a long-term and sustained role in mitigating the impacts of global warming, and the sequestration of C is closely linked to the nitrogen (N) cycle. Accurate estimates C and N storage (SC, SN) of forest can improve our understanding of C and N cycles and help develop sustainable forest management policies in the content of climate change. In this study, the SC and SN of various forest ecosystems dominated respectively by Castanopsis carlesii and Lithocarpus mairei (EB), Pinus yunnanensis (PY), Pinus armandii (PA), Keteleeria evelyniana (KE), and Quercus semecarpifolia (QS) in the central Yunnan Plateau of China, were estimated on the basis of a field inventory to determine the distribution and altitudinal patterns of SC and SN among various forest ecosystems. The results showed that (1) the forest SC ranged from 179.58 ± 20.57 t hm−1 in QS to 365.89 ± 35.03 t hm−1 in EB. Soil, living biomass and litter contributed an average of 64.73%, 31.72% and 2.86% to forest SC, respectively; (2) the forest SN ranged from 4.47 ± 0.94 t ha−1 in PY to 8.91 ± 1.83 t ha−1 in PA. Soil, plants and litter contributed an average of 86.88%, 10.27% and 2.85% to forest SN, respectively; (3) the forest SC and SN decreased apparently with increasing altitude. The result demonstrates that changes in forest types can strongly affect the forest SC and SN. This study provides baseline information for forestland managers regarding forest resource utilization and C management.

Highlights

  • Forest ­SC is estimated to account for approximately 45% of terrestrial ecosystem ­SC9,10

  • Exploring the distribution patterns of ­SN in forest ecosystems is essential for understanding the C cycle

  • The biomass of the forest ecosystems in the central Yunnan Plateau ranged from 142.36 ± 18.36 to 271.77 ± 34.71 t ­ha−1

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Summary

Introduction

Forest ­SC is estimated to account for approximately 45% of terrestrial ecosystem ­SC9,10. Living biomass has a great capacity to sequester atmospheric C and the aboveground living biomass has been considered as a major C ­pool[14,15]. Soil is another indispensable component of forest ecosystems and acts as an important C pool in terrestrial e­ cosystems[16,17]. Exploring the distribution patterns of ­SN in forest ecosystems is essential for understanding the C cycle. Camellia mairei (Levl.) Melch., Lithocarpus mairei (Schottky) Rehder, Vaccinium bracteatum Thunb., Rhododendron spiciferum Franch., Eurya yunnanensis Hsu, Symplocos anomala Brand, Ternstroemia gymnanthera (Wight et Arn.) Beddome

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