| A hole in the nematosphere: tardigrades and rotifers dominate the cryoconite hole environment, whereas nematodes are missing K Zawierucha, DL Porazinska, GF Ficetola, R Ambrosini, G Baccolo, ... Journal of Zoology 313 (1), 18-36, 2021 | 41 | 2021 |
| Integrative approach reveals new species of water bears (Pilatobius, Grevenius, and Acutuncus) from Arctic cryoconite holes, with the discovery of hidden lineages of Hypsibius K Zawierucha, J Buda, TN Jaromerska, K Janko, P Gąsiorek Zoologischer Anzeiger 289, 141-165, 2020 | 18 | 2020 |
| Stable isotopic composition of top consumers in Arctic cryoconite holes: revealing different position in supraglacial trophic network T Jaroměřská, J Trubač, K Zawierucha, L Vondrovicová, M Devetter, ... Biogeosciences Discussions 2020, 1-18, 2020 | 11 | 2020 |
| Cryophilic Tardigrada have disjunct and bipolar distribution and establish long-term stable, low-density demes K Zawierucha, EŠ Kašparová, S McInnes, J Buda, R Ambrosini, ... Polar Biology 46 (10), 1011-1027, 2023 | 4 | 2023 |
| Spatial distribution and stable isotopic composition of invertebrates uncover differences between habitats on the glacier surface in the Alps TN Jaroměřská, R Ambrosini, M Mazurkiewicz, A Franzetti, P Klimaszyk, ... Limnology 24 (2), 83-93, 2023 | 3 | 2023 |
| Spatio-temporal changes in cryoconite community, isotopic, and elemental composition over the ablation season of an alpine glacier T Novotná Jaroměřská, R Ambrosini, D Richter, M Pietryka, P Niedzielski, ... Biogeosciences Discussions 2022, 1-37, 2022 | | 2022 |
| Separation and Elemental Composition of Tardigrades and Rotifers from Cryoconite in Svalbard T Jaroměřská Univerzita Karlova, Přírodovědecká fakulta, 2019 | | 2019 |
| Stoichiometric patterns in cold oligotrophic aquatic systems T Jaroměřská Univerzita Karlova, Přírodovědecká fakulta, 2016 | | 2016 |
| Elemental composition of Tardigrada and Rotifera in cryoconite sediment in Svalbard T Jaroměřská, J Žárský Proceedings: Students in Polar and Alpine Research Conference 2017 20-22 …, 0 | | |
