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High abundances of the nuisance raphidophyte Gonyostomum semen in brown water lakes are associated with high concentrations of iron
Linnéuniversitetet, Fakulteten för Hälso- och livsvetenskap (FHL), Institutionen för biologi och miljö (BOM). Uppsala University. (Ctr Ecol & Evolut Microbial Model Syst EEMiS)ORCID-id: 0000-0002-3853-1662
Swedish University of Agricultural Sciences.
Uppsala University.
Swedish University of Agricultural Sciences.
Vise andre og tillknytning
2018 (engelsk)Inngår i: Scientific Reports, ISSN 2045-2322, E-ISSN 2045-2322, Vol. 8, artikkel-id 13463Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Algal blooms occur frequently in lakes and oceans and the causes and consequences of those are often studied. In this study, we focus on a less well known type of algal bloom by the freshwater raphidophyte Gonyostomum semen. This species' abundance and occurrence is increasing, especially in brown water lakes, the most abundant lake type in the boreal zone. The aim of the study was to investigate which environmental factors are associated with G. semen by statistical evaluation of field data of 95 Swedish lakes over five years. Although we found G. semen to be associated with dark waters it was, contrary to our expectations, mainly high concentrations of iron, and only to a lesser extent high TOC (total organic carbon) concentrations, that were associated with blooms of G. semen. In addition, high phosphorus concentrations and low pH also appear to facilitate G. semen blooms. We suggest that browning of lakes caused by increased iron concentrations may decrease net heterotrophy by fostering heavy algal blooms, i.e. the opposite to commonly assumed effects of increased DOM (dissolved organic matter).

sted, utgiver, år, opplag, sider
Nature Publishing Group, 2018. Vol. 8, artikkel-id 13463
HSV kategori
Forskningsprogram
Ekologi, Akvatisk ekologi
Identifikatorer
URN: urn:nbn:se:lnu:diva-78098DOI: 10.1038/s41598-018-31892-7ISI: 000444022800067PubMedID: 30194445Scopus ID: 2-s2.0-85052985359OAI: oai:DiVA.org:lnu-78098DiVA, id: diva2:1252424
Tilgjengelig fra: 2018-10-01 Laget: 2018-10-01 Sist oppdatert: 2019-08-29bibliografisk kontrollert

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