posted on 2014-05-06, 00:00authored byQianggong Zhang, Ke Pan, Shichang Kang, Aijia Zhu, Wen-Xiong Wang
Our
understanding of the biogeochemistry of mercury (Hg) in high-altitude
aquatic environments remains limited. The Tibetan Plateau (TP) is
one of the Earth’s most significant continental-scale high
lands, yet much remains unknown about the Hg bioaccumulation and biomagnification
in these pristine ecosystems. In this study, 166 wild fish samples
of 13 species were collected from 13 rivers and lakes across the southern
TP. Total Hg (THg) and methyl-Hg (MeHg) concentrations in the axial
muscle of fish ranged from 25.1 to 1218 ng g–1 of
wet weight (median ± average deviation of 100.5 ± 149.2
ng g–1) and from 24.9 to 1196 ng g–1 of wet weight (median ± average deviation of 90.7 ± 137.0
ng g–1), respectively. Hg concentrations varied
greatly within and between species. The fish Hg concentrations were
then linked to the limited available environmental Hg data and special
geochemical characteristics in the region, such as Hg loading, pH,
low temperature, and high ultraviolet (UV). The long lifespan and
slow growth of the fish under the low-productivity environments may
be the major biological factors that help to build up the fish Hg
levels comparable to those observed in wild fish growing in human-impacted
areas. δ13C signals suggested that pelagic fish had
higher Hg concentrations, but no relationship was found between the
Hg concentrations and the trophic levels. Zooplankton and benthic
amphipods had typically higher percentages of MeHg compared to the
previously reported values, suggesting the efficient transfer of MeHg
from the base of the aquatic food web. This study sheds some light
on the geochemical and biological controls of Hg bioaccumulation in
fish and biomagnification in the aquatic food web in arid high-altitude
environments.