Journal
POLAR BIOLOGY
Volume 40, Issue 3, Pages 603-613Publisher
SPRINGER
DOI: 10.1007/s00300-016-1983-1
Keywords
Oligotrophic lakes; Sediments; Antarctica; Polar ecosystems; Material cycle; Freshwater
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Funding
- Centre for the Promotion of Integrated Sciences (CPIS) of the Graduate University for Advanced Studies (SOKENDAI)
- JSPS KAKENHI [26310213, 21810035]
- Grants-in-Aid for Scientific Research [26241020, 21810035, 15K07480, 16H05885, 26310213] Funding Source: KAKEN
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Most freshwater lakes in continental Antarctica are in a paradoxical situation as they are in nutrient-poor conditions despite luxuriant vegetation growth covering the entire lakebed. Although the phytobenthos possibly take up nutrients from inside lakebeds, the amount of nutrients and their utilization by these phytobenthos are unclear. Sediment cores were collected from 17 freshwater lakes in East Antarctica, then dissolved inorganic nitrogen (DIN) and phosphate of the lake waters, and the vertical profiles of the interstitial water in the sediment cores were analyzed. Here we revealed that there are abundant nutrients inside lakebeds surface with 3-220 times the amount of DIN and 2-102 times concentration of phosphate than those in lake water, and the nutrient profile inside the sediment suggested that the phytobenthos can utilize the much nutrients from lakebeds. We also show that nitrogen stable isotope ratios of shallower phytobenthos lying on the small amount of nutrients in a lake are similar to that of terrestrial cyanobacteria possessing N-2 fixation ability.
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