McMurdo LTER Publications
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Heterotrophic protists as useful models for studying microbial food webs in a model soil ecosystem and the universality of complex unicellular life. . Department of Biology. 2019;PhD. Available at: https://www.proquest.com/docview/2310631977.
. The hydroecology of an ephemeral wetland in the McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research: Biogeosciences. 2019. doi:10.1029/2019JG005153.
In a PICL: The sedimentary deposits and facies of perennially ice-covered lakes. Sedimentology. 2019;66(3). doi:10.1111/sed.12522.
. Nematodes in a polar desert reveal the relative role of biotic interactions in the coexistence of soil animals. Communications Biology. 2019;2(1). doi:10.1038/s42003-018-0260-y.
The polar regions in a 2°C warmer world. Science Advances. 2019;5(12):eaaw9883. doi:10.1126/sciadv.aaw9883.
Provisional checklist of terrestrial heterotrophic protists from Antarctica. Antarctic Science. 2019. doi:10.1017/S0954102019000361.
. Soil nematode abundance and functional group composition at a global scale. Nature. 2019;572(7768). doi:10.1038/s41586-019-1418-6.
Soil nematode abundance and functional group composition at a global scale. Nature. 2019;572(7768). doi:10.1038/s41586-019-1418-6.
Soil nematode abundance and functional group composition at a global scale. Nature. 2019;572(7768). doi:10.1038/s41586-019-1418-6.
Aeolian material transport and its role in landscape connectivity in the McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research: Earth Surface. 2018;123(12):3323 - 3337. doi:10.1029/2017JF004589.
BioTIME: A database of biodiversity time series for the Anthropocene. Global Ecology and Biogeography. 2018;27(7):760-786. doi:10.1111/geb.12729.
BioTIME: A database of biodiversity time series for the Anthropocene. Global Ecology and Biogeography. 2018;27(7):760-786. doi:10.1111/geb.12729.
BioTIME: A database of biodiversity time series for the Anthropocene. Global Ecology and Biogeography. 2018;27(7):760-786. doi:10.1111/geb.12729.
BioTIME: A database of biodiversity time series for the Anthropocene. Global Ecology and Biogeography. 2018;27(7):760-786. doi:10.1111/geb.12729.
BioTIME: A database of biodiversity time series for the Anthropocene. Global Ecology and Biogeography. 2018;27(7):760-786. doi:10.1111/geb.12729.
BioTIME: A database of biodiversity time series for the Anthropocene. Global Ecology and Biogeography. 2018;27(7):760-786. doi:10.1111/geb.12729.
BioTIME: A database of biodiversity time series for the Anthropocene. Global Ecology and Biogeography. 2018;27(7):760-786. doi:10.1111/geb.12729.
Genomics and transcriptomics of Antarctic nematodes reveal drivers of life history evolution and genome evolution. Department of Biology. 2018;Ph.D. Available at: https://search.proquest.com/docview/2081899003.
. Microbial and CO2 responses to water stresses show decreased productivity and diversity through time. Department of Plant and Wildlife Sciences. 2018;M.S. Available at: https://scholarsarchive.byu.edu/etd/6830.
. Observed trends of soil fauna in the Antarctic Dry Valleys: early signs of shifts predicted under climate change. Ecology. 2018;99(2):312 - 321. doi:10.1002/ecy.2090.
. Observed trends of soil fauna in the Antarctic Dry Valleys: early signs of shifts predicted under climate change. Ecology. 2018;99(2):312 - 321. doi:10.1002/ecy.2090.
. Photoecology of the Antarctic cyanobacterium Leptolyngbya sp. BC1307 brought to light through community analysis, comparative genomics and in vitro photophysiology. Molecular Ecology. 2018;27(24):5279 - 5293. doi:10.1111/mec.14953.
. Soil biological responses to C, N and P fertilization in a polar desert of Antarctica. Soil Biology and Biochemistry. 2018;122. doi:10.1016/j.soilbio.2018.03.025.
. Soil Moisture Controls the Thermal Habitat of Active Layer Soils in the McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research: Biogeosciences. 2018;123(1). doi:10.1002/2017JG004018.
. Spatial and temporal patterns of microbial mats and associated invertebrates along an Antarctic stream. Polar Biology. 2018;41(10):1911–1921. doi:10.1007/s00300-018-2331-4.