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The historical development of three man-made reservoirs in a mining region: A story told by subfossil chironomids
Title The historical development of three man-made reservoirs in a mining region: A story told by subfossil chironomids Author Chamutiová Tímea Co-authors Hamerlík Ladislav Szarłowicz Katarzyna Kyška-Pipík Radovan 1970 - SAVUVOZ - Ústav vied o Zemi SAV SCOPUS ORCID Starek Dušan 1974 - SAVUVOZ - Ústav vied o Zemi SAV SCOPUS ORCID Šporka Ferdinand 1951- SAVZOOL - Ústav zoológie SAV Přidalová Marcela Sochuliaková Lucia Bitušík Peter Source document Journal of Limnology. Vol. 77 (2018), p. 220-229 Language eng - English Country IT - Italy Document kind rozpis článkov z periodík (rbx) Citations LENCIONI, Valeria - CRANSTON, Peter S. - MAKARCHENKO, Eugenyi A. Recent advances in the study of Chironomidae: An overview. In JOURNAL OF LIMNOLOGY. ISSN 1129-5767, 2018, vol. 77, no., pp. 1-6. SZARLOWICZ, Katarzyna - STOBINSKI, Marcin - HAMERLIK, Ladislav - BITUSIK, Peter. Origin and behavior of radionuclides in sediment core: a case study of the sediments collected from man-made reservoirs located in the past mining region in Central Slovakia. In ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH. ISSN 0944-1344, 2019, vol. 26, no. 7, pp. 7115-7122. DE MELO, Dalescka Barbosa - DOLBETH, Marina - PAIVA, Franciely Ferreira - MOLOZZI, Joseline. Extreme drought scenario shapes different patterns of Chironomid coexistence in reservoirs in a semi-arid region. In SCIENCE OF THE TOTAL ENVIRONMENT. ISSN 0048-9697, 2022, vol. 821, no., pp. Dostupné na: https://doi.org/10.1016/j.scitotenv.2022.153053. Category ADMA - Scientific papers in foreign impacted journals registered in Web of Sciences or Scopus Category of document (from 2022) V3 - Vedecký výstup publikačnej činnosti z časopisu Type of document článok Year 2018 Registered in WOS Registered in SCOPUS DOI 10.4081/jlimnol.2018.1798 
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rok CC IF IF Q (best) JCR Av Jour IF Perc SJR SJR Q (best) CiteScore N rok vydania rok metriky IF IF Q (best) SJR SJR Q (best) 2018 2017 1.277 Q3 0.632 Q2
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