Arid
DOI10.1890/0012-9658(1999)080[0150:LTCODO]2.0.CO;2
Long-term consequences of disturbance on nitrogen dynamics in an arid ecosystem
Evans, RD; Belnap, J
通讯作者Evans, RD
来源期刊ECOLOGY
ISSN0012-9658
出版年1999
卷号80期号:1页码:150-160
英文摘要

Anthropogenic activity is causing dramatic changes in the nitrogen (N) cycle in many ecosystems. Most research has focused on the increase in N input caused by atmospheric deposition and invasion of N-fixing species, and on their effects on resource availability and species composition. However, in contrast to many ecosystems experiencing large increases in N input, many arid ecosystems are experiencing loss of nutrients due to land-use change. An important component of many arid ecosystems on a worldwide basis is the microbiotic crust, a biological soil crust composed of lichens, cyanobacteria, mosses, and algae. Nitrogen fixation by lichens and cyanobacteria comprising the crust is the primary source of N input in many of these ecosystems. We quantified the long-term consequences of surface disturbance in an arid ecosystem on the Colorado Plateau by comparing pristine sites with those of known disturbance history. Disturbance caused an increase in the abundance of cyanobacteria and a decrease in lichens within the microbiotic crust. Carbon isotope composition (delta(13)C) of the crust reflects this shift in species composition; values for disturbed sites were 4.5 parts per thousand higher than undisturbed sites. Nitrogen isotope composition (delta(15)N) of the microbiotic crust was 1.5-2.2 parts per thousand higher for disturbed sites, probably resulting from relatively greater gaseous N loss from the crust. Historic disturbance has caused a long-term decrease in rates of N fixation by the microbiotic crust; nitrogenase activity in pristine sites was 250% greater than sites intermittently disturbed 30 yr ago. The decrease in N input from fixation and continued gaseous N loss has caused a 25-75% decrease in soil N content. Altering relative rates of N input and loss, coupled with input of N from microbiotic crusts with relatively higher delta(15)N, has caused an increase in soil and plant delta(15)N at disturbed sites. This decrease in soil N caused by disturbance will likely cause changes in species composition similar to those observed in ecosystems that have been disrupted by excess N input from atmospheric deposition.


英文关键词Canyonlands National Park, Utah, USA cryptogamic crusts land-use change microbiotic crusts microphytic crusts mineralization nitrification nitrogen stable isotopes
类型Article
语种英语
国家USA
收录类别SCI-E
WOS记录号WOS:000078045600011
WOS关键词CARBON-ISOTOPE DISCRIMINATION ; CANYONLANDS-NATIONAL-PARK ; FERTILE-SOIL MICROSITES ; PICEA-ABIES FOREST ; CHIHUAHUAN DESERT ; SURFACE DISTURBANCES ; NATURAL ABUNDANCE ; MICROBIAL BIOMASS ; LARREA-TRIDENTATA ; GLOBAL CHANGE
WOS类目Ecology
WOS研究方向Environmental Sciences & Ecology
来源机构United States Geological Survey
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/137240
作者单位(1)Univ Arkansas, Fayetteville, AR 72701 USA;(2)US Geol Serv, Biol Res Div, Moab, UT 84532 USA
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GB/T 7714
Evans, RD,Belnap, J. Long-term consequences of disturbance on nitrogen dynamics in an arid ecosystem[J]. United States Geological Survey,1999,80(1):150-160.
APA Evans, RD,&Belnap, J.(1999).Long-term consequences of disturbance on nitrogen dynamics in an arid ecosystem.ECOLOGY,80(1),150-160.
MLA Evans, RD,et al."Long-term consequences of disturbance on nitrogen dynamics in an arid ecosystem".ECOLOGY 80.1(1999):150-160.
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