TY - JOUR
T1 - A hole in the nematosphere
T2 - tardigrades and rotifers dominate the cryoconite hole environment, whereas nematodes are missing
AU - Zawierucha, K.
AU - Porazinska, D. L.
AU - Ficetola, G. F.
AU - Ambrosini, R.
AU - Baccolo, G.
AU - Buda, J.
AU - Ceballos, J. L.
AU - Devetter, M.
AU - Dial, R.
AU - Franzetti, A.
AU - Fuglewicz, U.
AU - Gielly, L.
AU - Łokas, E.
AU - Janko, K.
AU - Novotna Jaromerska, T.
AU - Kościński, A.
AU - Kozłowska, A.
AU - Ono, M.
AU - Parnikoza, I.
AU - Pittino, F.
AU - Poniecka, E.
AU - Sommers, P.
AU - Schmidt, S. K.
AU - Shain, D.
AU - Sikorska, S.
AU - Uetake, J.
AU - Takeuchi, N.
N1 - Funding Information:
The authors would like to thank two anonymous reviewers for their valuable comments and corrections. Studies on Arctic glaciers were supported by the National Science Centre under Grant No. NCN 2013/11/N/NZ8/00597 awarded to K.Z. Samples from the Bl?isen and Midtdalsbreen glaciers were collected within the Grant [ETANGO] awarded by INTERACT Transnational Access to K.Z. GFF was funded by the European Research Council under the European Community's Horizon 2020 Programme, Grant Agreement no. 772284 (IceCommunities). NT was supported by the funds from JSPS KAKENHI (19H01143 and 20K21840), and from the Arctic Challenge for Sustainability II (ArCS II), Program Grant Number JPMXD1420318865. Work on glaciers from the McMurdo Dry Valleys of Antarctica was supported by the National Science Foundation Award #1443578 to S.K.S. Fieldwork on Marr Ice Piedmont was realized according to kindly assistance of National scientific foundation (USA) and Palmer station crew. All of the samples were properly collected under the permission of local organizations or governments. The samples from the Ecology Glacier used in the paper were collected and transported based on the logistic support of Henryk Arctowski Polish Antarctic Station. The sampling on Ecology Glacier were initiated by the seminar, ?The role of cryoconite in the functioning of glacial systems? supported by the Centre for Polar Studies (the Leading National Research Centre in Earth Sciences for 2014?2018 No. 03/KNOW2/2014). K.Z. is grateful to Ela Wiejaczka for her support in gaining permission and access to samples from Africa, Joseph Cook for collection of samples in the dark zone of Greenland Ice Sheet, E.?. thanks ?ukasz Paw?owski for collection of samples from Werenskiold Glacier, and T.J. thanks Mat?j Pokorn? (Department of Ecology, Charles University) for collection of samples from Blancmange Glacier. Swedish samples were kindly provided to E.P. by Alexandre Anesio.
PY - 2021/1
Y1 - 2021/1
N2 - The worldwide distribution of microinvertebrates on glaciers, the coldest biome, is poorly known. Owing to their tolerance to hostile conditions, small size and dispersal abilities, nematodes, tardigrades and rotifers are considered cosmopolitan and together inhabit various ecosystems. In this study, we investigated their global distribution in cryoconite holes – a type of freshwater reservoir forming directly in the glacial ice that creates biodiversity hotspots on glaciers. We analysed cryoconite samples (using classical microscopic observations and environmental DNA metabarcoding) from 42 glaciers located around the world (the Arctic, Subarctic, Scandinavia, the Alps, the Caucasus, Siberia, Central Asia, Africa, South America and Antarctica), as well as using literature data. Samples from Antarctic, Karakoram and the Alps were analysed using next-generation sequencing (NGS) and classical observations under microscopes, while all other samples were analysed by microscope alone. Three general outcomes were found: (1) tardigrades and rotifers represented the most common invertebrates in cryoconite holes; (2) tardigrades and rotifers often coexisted together, with one or the other dominating, but the dominant taxon varied by region or by glacier; (3) nematodes – the most abundant, hyperdiverse and widespread metazoans on Earth, including in environments surrounding and seeding glacial surfaces – were consistently absent from cryoconite holes. Despite the general similarity of environmental conditions in cryoconite holes, the distribution of tardigrades and rotifers differed among glaciers, but not in any predictable way, suggesting that their distribution mostly depended on the random dispersal, extreme changes of supraglacial zone or competition. Although nematodes have been found in supraglacial habitats, cryoconite hole environments seem not to provide the necessary conditions for their growth and reproduction. Lack of physiological adaptations to permanently low temperatures (~0°C) and competition for different food resources in the cryoconite hole environment may explain the absence of nematodes in cryoconite holes.
AB - The worldwide distribution of microinvertebrates on glaciers, the coldest biome, is poorly known. Owing to their tolerance to hostile conditions, small size and dispersal abilities, nematodes, tardigrades and rotifers are considered cosmopolitan and together inhabit various ecosystems. In this study, we investigated their global distribution in cryoconite holes – a type of freshwater reservoir forming directly in the glacial ice that creates biodiversity hotspots on glaciers. We analysed cryoconite samples (using classical microscopic observations and environmental DNA metabarcoding) from 42 glaciers located around the world (the Arctic, Subarctic, Scandinavia, the Alps, the Caucasus, Siberia, Central Asia, Africa, South America and Antarctica), as well as using literature data. Samples from Antarctic, Karakoram and the Alps were analysed using next-generation sequencing (NGS) and classical observations under microscopes, while all other samples were analysed by microscope alone. Three general outcomes were found: (1) tardigrades and rotifers represented the most common invertebrates in cryoconite holes; (2) tardigrades and rotifers often coexisted together, with one or the other dominating, but the dominant taxon varied by region or by glacier; (3) nematodes – the most abundant, hyperdiverse and widespread metazoans on Earth, including in environments surrounding and seeding glacial surfaces – were consistently absent from cryoconite holes. Despite the general similarity of environmental conditions in cryoconite holes, the distribution of tardigrades and rotifers differed among glaciers, but not in any predictable way, suggesting that their distribution mostly depended on the random dispersal, extreme changes of supraglacial zone or competition. Although nematodes have been found in supraglacial habitats, cryoconite hole environments seem not to provide the necessary conditions for their growth and reproduction. Lack of physiological adaptations to permanently low temperatures (~0°C) and competition for different food resources in the cryoconite hole environment may explain the absence of nematodes in cryoconite holes.
KW - Nematoda
KW - Rotifera
KW - Tardigrada
KW - distribution
KW - ecological selection
KW - extremophiles
KW - glaciers
KW - psychrophiles
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U2 - 10.1111/jzo.12832
DO - 10.1111/jzo.12832
M3 - Article
AN - SCOPUS:85091000696
VL - 313
SP - 18
EP - 36
JO - Journal of Zoology
JF - Journal of Zoology
SN - 0952-8369
IS - 1
ER -