Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-p2v8j Total loading time: 0 Render date: 2024-06-08T15:04:13.948Z Has data issue: false hasContentIssue false

13 - Restoration of high-altitude peatlands on the Ruoergai Plateau (Northeastern Tibetan Plateau, China)

from Part II - Perspectives on peatland restoration

Published online by Cambridge University Press:  05 June 2016

Xiaohong Zhang
Affiliation:
Wetlands International China Offi ce, Beijing, China
Martin Schumann
Affiliation:
Ernst Moritz Arndt University of Greifswald, Germany
Yongheng Gao
Affiliation:
Chinese Academy of Sciences, Chengdu, China
J. Marc Foggin
Affiliation:
Institute of Asian Research, University of British Columbia, Canada
Shengzhong Wang
Affiliation:
Northeast Normal University Changchun, China
Hans Joosten
Affiliation:
University of Greifswald
Aletta Bonn
Affiliation:
German Centre für Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig
Tim Allott
Affiliation:
University of Manchester
Martin Evans
Affiliation:
University of Manchester
Hans Joosten
Affiliation:
Institute of Botany and Landscape Ecology
Rob Stoneman
Affiliation:
Yorkshire Wildlife Trust
Get access

Summary

Introduction

All over the world, high-altitude peatlands are the product of co-evolution between nature and pastoral communities. Over thousands of years, people, looking for subsistence and resources, have changed the character of fragile mountain landscapes and their peatlands through deforestation and livestock grazing (Trimble and Mendel 1995). Increasing population pressure, the quest for mineral resources and perverse policies have in recent times intensified these changes.

The character of high-altitude peatlands can be paraphrased as ‘cold and steep and wet and sheep’. The high altitude induces colder and more humid conditions and – upwind of the mountain – more precipitation. Excessive exposure to ultraviolet radiation at high altitudes requires special adaptation of the biota, whereas the climatic island character explains the disjunct distribution of species and the high degree of endemism (Körner 2003, 2008; Spehn et al. 2010). The colder climate also discourages arable agriculture so that pastoralism – with a wide variety of livestock – is the principal form of subsistence. High rainfall and relatively steep slopes generate surface runoff, exposing the landscape and the sensitive peatlands to strong erosive forces (Evans and Warburton 2007).

The world's largest concentration of high-altitude peatlands is found in the northeastern part of the Qinghai–Tibetan Plateau (China). There, in the provinces of Sichuan and Gansu right in the heart of China (Figure 13.1), the Ruoergai (or Zoige) Plateau is located at an altitude of about 3500 m a.s.l. In contrast to the drier western and central parts of Tibet, the Ruoergai Plateau, a plain glacial landscape with low mountain ranges of some hundred metres in height, has a humid climate with long winters and short summers (Lehmkuhl and Liu 1994) which have facilitated the development of 474 000 ha of peatlands (Schumann, Thevs and Joosten 2008).

In this chapter, we explore the history and drivers of peatland degradation on the Ruoergai Plateau, the loss of important ecosystem services and the impact of such loss on livelihoods. We discuss how integrated projects may facilitate the restoration of ecosystem services and biodiversity while contributing to poverty alleviation. Case studies present the various approaches and illustrate how participatory community involvement is integral to the successful implementation of peatland conservation and restoration programmes.

Type
Chapter
Information
Peatland Restoration and Ecosystem Services
Science, Policy and Practice
, pp. 234 - 252
Publisher: Cambridge University Press
Print publication year: 2016

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×