Quantitative stable isotope probing with 18O-H2O to measure microbial growth rates in response to warming on the Antarctic Peninsula
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https://www.ncbi.nlm.nih.gov/sra/SRP410868
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Quantitative stable isotope probing with 18O-H2O to measure microbial growth rates in response to warming on the Antarctic Peninsula. Performed at two sites, a recently deglaciated sere and a moss peat bank on the chronosequence of the Marr Ice Piedmont Glacier Chronosequence on Anvers island, West Antarctic Peninsula
创建时间：
2022-12-01
