Recent increases in air temperature across the Antarctic Peninsula
may prolong the thawing period and directly affect
the soil temperature (Ts) and volumetric soil water content
(SWC) in maritime tundra. Under an 8°C soil warming scenario,
two customized microcosm systems with maritime
Antarctic soils were incubated to investigate the differential
influence of SWC on the bacterial community and degradation
activity of humic substances (HS), the largest constituent
of soil organic carbon and a key component of the terrestrial
ecosystem. When the microcosm soil (KS1-4Feb) was
incubated for 90 days (T = 90) at a constant SWC of ~32%,
the initial HS content (167.0 mg/g of dried soil) decreased to
156.0 mg (approximately 6.6% loss, p < 0.05). However, when
another microcosm soil (KS1-4Apr) was incubated with
SWCs that gradually decreased from 37% to 9% for T = 90,
HS degradation was undetected. The low HS degradative
activity persisted, even after the SWC was restored to 30%
with water supply for an additional T = 30. Overall bacterial
community structure remained relatively stable at a constant
SWC setting (KS1-4Feb). In contrast, we saw marked
shifts in the bacterial community structure with the changing
SWC regimen (KS1-4Apr), suggesting that the soil bacterial
communities are vulnerable to drying and re-wetting
conditions. These microcosm experiments provide new information
regarding the effects of constant SWC and higher
Ts on bacterial communities for HS degradation in maritime
Antarctic tundra soil.
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