2005
DOI: 10.1007/s00248-004-0270-9
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High Heterotrophic Bacterial Production in Acidic, Iron-Rich Mining Lakes

Abstract: The acidic mining lakes of Eastern Germany are characterized by their extremely low pH and high iron concentrations. Low concentrations of CO2 in the epilimnion due to the low pH and reduced light transmission due to dissolved ferric iron potentially limit phytoplankton primary production (PP), whereas dissolved organic carbon (DOC) may promote heterotrophic production of bacteria (HP). We, therefore, tested whether HP exceeds PP in three lakes differing in pH and iron concentration (mean pH 2.3-3.0, 23-500 mg… Show more

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Cited by 48 publications
(30 citation statements)
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“…The hydrochemical composition is remarkably similar in the study lakes; pH ranges from 2.3-2.8. Physico-chemical and biological features of these AML have been reported by Nixdorf et al (2003), Kamjunke et al (2005), Gaedke and Kamjunke (2006), Weithoff et al (2010), and Moser and Weisse (2011b). The AML at Langau (LG in the following) and the AML111 in Lusatia (ML111 in the following) are older than the adjacent AML130 (ML130 in the following); the latter is also the largest of the three study lakes (Table 1).…”
Section: Methodssupporting
confidence: 52%
“…The hydrochemical composition is remarkably similar in the study lakes; pH ranges from 2.3-2.8. Physico-chemical and biological features of these AML have been reported by Nixdorf et al (2003), Kamjunke et al (2005), Gaedke and Kamjunke (2006), Weithoff et al (2010), and Moser and Weisse (2011b). The AML at Langau (LG in the following) and the AML111 in Lusatia (ML111 in the following) are older than the adjacent AML130 (ML130 in the following); the latter is also the largest of the three study lakes (Table 1).…”
Section: Methodssupporting
confidence: 52%
“…During the last few decades, numerous studies have permitted to describe the biogeochemical functioning of these acid mining pit lakes and to currently consider bioremediation strategies (e.g. Peine et al, 2000;Knöller et al, 2004;Meier et al, 2004;Kamjunke et al, 2005;Blodau, 2006;Koschorreck et al, 2007;Geller et al, 2009). The acidity of lake water is a result of the weathering of pyriteand marcasite-enriched surrounding dumps through the production of SO different factors controlling microbial oxidizing and reductive processes within top sediments are thus crucial for the dynamics of acidity generation and consumption, and as a consequence, for the long-term development of acidic mining lakes and their watersheds (Blodau, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…The formation of low‐molecular‐weight organic acids by photolysis of recalcitrant DOC (Brinkmann et al. 2003, Kamjunke et al. 2005) stimulates the activity of bacteria and algae (Wetzel et al.…”
mentioning
confidence: 99%
“…Cd. acidophila and planktonic bacteria from an acidic environment were isolated from mining lake 111 (Germany; pH 2.6; see Kamjunke et al. 2005).…”
mentioning
confidence: 99%