TY - JOUR
T1 - Bryophyte cover on trees as proxy for air humidity in the tropics
AU - Karger, Dirk Nikolaus
AU - Kluge, Jürgen
AU - Abrahamczyk, Stefan
AU - Salazar, Laura
AU - Homeier, Jürgen
AU - Lehnert, Marcus
AU - Amoroso, Victor B.
AU - Kessler, Michael
PY - 2012/9
Y1 - 2012/9
N2 - Climatic conditions are a prime candidate to explain local patterns of biodiversity and consequently there is great need of on-site climatic measurements. Among them, however, air humidity is notoriously difficult and time-consuming to measure, and it has been proposed that the epiphytic bryophyte cover can be used as an indicator of long-term air humidity conditions. Here we explore the utility of visually estimated epiphytic bryophyte cover on large canopy branches as a proxy for air humidity at 26 study sites in tropical forests where we measured microclimate for at least 12 months. Across all sites, bryophyte cover was weakly related to relative air humidity (R 2 = 0.17), but when we separated highland (1800-3500 m elevation) from lowland (<1800 m) sites, relative air humidity showed significant and distinct relations to bryophyte cover (R 2 = 0.36-0.62), whereas temperature was related to bryophyte cover only in the lowlands (R 2 = 0.36). We conclude that epiphytic bryophyte cover can be used as a proxy for air humidity if temperature and elevation are taken into account within a circumscribed study region, but might not be applicable for comparisons across extensive elevational gradients or wide differences in temperature.
AB - Climatic conditions are a prime candidate to explain local patterns of biodiversity and consequently there is great need of on-site climatic measurements. Among them, however, air humidity is notoriously difficult and time-consuming to measure, and it has been proposed that the epiphytic bryophyte cover can be used as an indicator of long-term air humidity conditions. Here we explore the utility of visually estimated epiphytic bryophyte cover on large canopy branches as a proxy for air humidity at 26 study sites in tropical forests where we measured microclimate for at least 12 months. Across all sites, bryophyte cover was weakly related to relative air humidity (R 2 = 0.17), but when we separated highland (1800-3500 m elevation) from lowland (<1800 m) sites, relative air humidity showed significant and distinct relations to bryophyte cover (R 2 = 0.36-0.62), whereas temperature was related to bryophyte cover only in the lowlands (R 2 = 0.36). We conclude that epiphytic bryophyte cover can be used as a proxy for air humidity if temperature and elevation are taken into account within a circumscribed study region, but might not be applicable for comparisons across extensive elevational gradients or wide differences in temperature.
KW - Bryophyte cover
KW - Bryophytes
KW - Elevational gradient
KW - Relative air humidity
KW - Temperature
KW - Vapour pressure deficit
UR - http://www.scopus.com/inward/record.url?scp=84858414639&partnerID=8YFLogxK
U2 - 10.1016/j.ecolind.2012.02.026
DO - 10.1016/j.ecolind.2012.02.026
M3 - Artículo
AN - SCOPUS:84858414639
SN - 1470-160X
VL - 20
SP - 277
EP - 281
JO - Ecological Indicators
JF - Ecological Indicators
ER -