Visually assessing the level of development and soil surface stability of cyanobacterially dominated biological soil crusts

被引:125
作者
Belnap, J. [1 ]
Phillips, S. L. [1 ]
Witwicki, D. L. [1 ]
Miller, M. E. [2 ]
机构
[1] US Geol Survey, SW Biol Sci Ctr, Moab, UT 84532 USA
[2] US Geol Survey, SW Biol Sci Ctr, Kanab, UT 84741 USA
关键词
arid kind; desert; dryland; erosion; microbiotic soil crust;
D O I
10.1016/j.jaridenv.2008.02.019
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Biological soil crusts (BSCs) are an integral part of dryland ecosystems and often included in long-term ecological monitoring programs. Estimating moss and lichen cover is fairly easy and non-destructive, but documenting cyanobacterial level of development (LOD) is more difficult, It requires sample collection for laboratory analysis, which causes soil surface disturbance. Assessing soil surface stability also requires surface disturbance. Here we present a visual technique to assess cyanobacterial LOD and soil surface stability. We define six development levels of cyanobacterially dominated soils based on soil surface darkness. We sampled chlorophyll a concentrations (the most common way of assessing cyanobacterial biomass), exopolysaccharide concentrations, and soil surface aggregate stability from representative areas of each LOD class. We found that, in the laboratory and field, LOD classes were effective at predicting chlorophyll a soil concentrations (R-2 = 68-81%), exopolysaccharide concentrations (R-2 = 71%), and soil aggregate stability (R-2 = 77%). We took representative photos of these classes to construct a field guide. We then tested the ability of field crews to distinguish these classes and found this technique was highly repeatable among observers, We also discuss how to adjust this index for the different types of BSCs found in various dryland regions. Published by Elsevier Ltd.
引用
收藏
页码:1257 / 1264
页数:8
相关论文
共 20 条
[1]  
[Anonymous], 20055197 US GEOL SUR
[2]  
Barger, 2003, BIOGEOCHEMICAL CYCLI
[3]  
BELNAP J, 1993, GREAT BASIN NAT, V53, P40
[4]  
Belnap J, 2001, ECOL STUD-ANAL SYNTH, V150, P3
[5]   Vulnerability of desert biological soil crusts to wind erosion: the influences of crust development, soil texture, and disturbance [J].
Belnap, J ;
Gillette, DA .
JOURNAL OF ARID ENVIRONMENTS, 1998, 39 (02) :133-142
[6]  
Belnap J, 1997, LAND DEGRAD DEV, V8, P355, DOI 10.1002/(SICI)1099-145X(199712)8:4<355::AID-LDR266>3.0.CO
[7]  
2-H
[8]  
Belnap J., 2013, BIOL SOIL CRUSTS STR
[9]   Temporal variation in community composition, pigmentation, and Fv/Fm of desert cyanobacterial soil crusts [J].
Bowker, MA ;
Reed, SC ;
Belnap, J ;
Phillips, SL .
MICROBIAL ECOLOGY, 2002, 43 (01) :13-25
[10]  
deCano MS, 1997, PHYTON-INT J EXP BOT, V60, P33