Influence of desertification on vegetation pattern variations in the cold semi-arid grasslands of Qinghai-Tibet Plateau, North-west China

نویسنده

  • G. R. Dong
چکیده

In arid and semi-arid grassland, many models hypothesize that desertification leads to the replacement of grassland by shrubland vegetation; however, the theoretical interpretations are open to debate. Therefore, a field study was conducted in the Guinan desertified grassland of the Qinghai-Tibet plateau, North-west China, to test the hypotheses on a regional scale. We used four field sites to represent the four stages of desert development: slight, moderate, severe and very severe. A total of 40 quadrates were investigated in each site. Plant coverage, aboveground biomass, species richness and life-form were recorded; species diversity was calculated using the Simpson index and soil parameters were also measured. Our results indicate that the proportion of silt decreases from 12% in the slight stage to 1% in the very severe stage, clay from 71% to 42% and sand from 17% to 93%. Soil water-holding capacity clearly decreases from the slight to the very severe stage. Soil organic matter (OM) is also reduced with desert development, which leads to destruction of the stability of soil physical structure and nutrient content, such as progressive N, P and K loss in surface and subsoil layers. In response to changes in soil properties, vegetation altered as regards species composition, species diversity, coverage, structure and life-form. Consequently, with desert development, herbaceous species, especially grasses, were lost from the community composition and replaced by xerophytic shrubs or semi-shrubs. Finally, psammophytic annual plants-dominated vegetation composition, while shrub maintained a low coverage. Although our results partially support previous hypotheses at the regional scale, it is considered that, apart from soil texture, soil OM and see front matter r 2005 Elsevier Ltd. All rights reserved. .jaridenv.2005.06.011 nding author. Fax: +86931 827 3894. dress: [email protected] (X.R. Li).

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Eco-environmental effects of the Qinghai-Tibet Plateau uplift during the Quaternary in China

L. Fengquan 7 B. Jianmin College of Environment and Construction Engineering Changchun University of Science and Technology, Changchun City. 130026. P.R. China Abstract The Qinghai–Tibet Plateau uplifted 13000 m in the Quaternary period. The average rate of uplift was 1–1.1 mm/year. The uplifting has remolded the geomorphology of China. The landform in China was changed from west-low and east-h...

متن کامل

Desertification and its relationship with permafrost degradation in Qinghai-Xizang (Tibet) plateau

Desertification in Qinghai-Xizang (Tibet) Plateau is part of Chinese desertification. In the past decades, due to the climate warming, the climate condition in Qinghai-Xizang (Tibet) Plateau has been relatively dry. This has resulted in permafrost degradation and other environmental problems. In addition, the vegetation and the soil layer were also destroyed by unreasonable economic activities....

متن کامل

The Influences of Climate Change and Human Activities on Vegetation Dynamics in the Qinghai-Tibet Plateau

Grasslands occupy nearly three quarters of the land surface of the Qinghai-Tibet plateau (QTP) and play a critical role in regulating the ecological functions of the QTP. Ongoing climate change and human interference have greatly affected grasslands on the QTP. Differentiating human-induced and climate-driven vegetation changes is vital for both ecological understanding and the management of hu...

متن کامل

Desert Transformation or D‌esertification Control?

The UNCCD has been ratified by over 190 countries. It is the attempt by nations, both rich and poor to control the scourge of desertification. The definition of which is “land degradation in arid, semiarid, and dry subhumid areas resulting from various factors, including climatic variations and human activities. It is now widely accepted that desertification is not the relentless advance of des...

متن کامل

The Loess Plateau

The Loess Plateau (34°–40°N, 103°–114°E) is situated in the northern part of Central China (Fig. 2.1). It borders on North China Plain in the east, adjoins Qinghai-Tibet Plateau in the west, stands in the north of Qinling Mountains, and neighbors Inner Mongolia Plateau in the north. The Loess Plateau is a part of the dryland region in northwest China, with its altitude in the range of 800–3000 ...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2005