Phytoplankton of the extremely acidic mining lakes of Lusatia (Germany) with pH <=3
Most of the flooded, open-cast lignite mining lakes of Lusatia (Germany) impacted by the oxidation of iron sulphides (pyrite and marcasite) are extremely acidic. Of 32 lakes regularly studied from 1995 to 1998, 14 have a pH
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Veröffentlicht in: | Hydrobiologia 2000-08, Vol.433 (1-3), p.123 |
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creator | Lessmann, Dieter Fyson, Andrew Nixdorf, Brigitte |
description | Most of the flooded, open-cast lignite mining lakes of Lusatia (Germany) impacted by the oxidation of iron sulphides (pyrite and marcasite) are extremely acidic. Of 32 lakes regularly studied from 1995 to 1998, 14 have a pH |
doi_str_mv | 10.1023/A:1004018722898 |
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Of 32 lakes regularly studied from 1995 to 1998, 14 have a pH <3 (median pH 2.3-2.9). These lakes are typically buffered by high concentrations of Fe (III) and have high conductivity (1000-5000 μS cm^sup -1^). Concentrations of dissolved inorganic carbon (DIC) and phosphorus are typically extremely low. These factors result in a very different environment for algae than found in neutral and acid-rain impacted lakes. The planktonic algal flora is generally dominated by flagellates belonging to genera of Chlorophyta (Chlamydomonas), Heterokontophyta of the class Chrysophyceae (Ochromonas, Chromulina), Cryptophyta (Cyathomonas) and Euglenophyta (Lepocinclis, Euglena mutabilis). Near-spherical non-motile Chlorophyta (Nanochlorum sp.), Heterokontophyta of the class Bacillariophyceae (Eunotia exigua, Nitzschia), Dinophyta (Gymnodinium, Peridinium umbonatum), other Chlorophyta (Scourfieldia cordiformis) and Cryptophyta (Rhodomonas minuta) are also found.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 0018-8158</identifier><identifier>EISSN: 1573-5117</identifier><identifier>DOI: 10.1023/A:1004018722898</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Acid mine drainage ; Acid rain ; Algae ; Dissolved inorganic carbon ; Flora ; Lakes ; Lignite ; Limnology ; Phytoplankton ; Plankton ; Pyrite ; Taxonomy</subject><ispartof>Hydrobiologia, 2000-08, Vol.433 (1-3), p.123</ispartof><rights>Kluwer Academic Publishers 2000</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c226t-fd95f213efdcaa50de9211981c832ffa10c6e75013628246843e0c212b65c3a13</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Lessmann, Dieter</creatorcontrib><creatorcontrib>Fyson, Andrew</creatorcontrib><creatorcontrib>Nixdorf, Brigitte</creatorcontrib><title>Phytoplankton of the extremely acidic mining lakes of Lusatia (Germany) with pH <=3</title><title>Hydrobiologia</title><description>Most of the flooded, open-cast lignite mining lakes of Lusatia (Germany) impacted by the oxidation of iron sulphides (pyrite and marcasite) are extremely acidic. Of 32 lakes regularly studied from 1995 to 1998, 14 have a pH <3 (median pH 2.3-2.9). These lakes are typically buffered by high concentrations of Fe (III) and have high conductivity (1000-5000 μS cm^sup -1^). Concentrations of dissolved inorganic carbon (DIC) and phosphorus are typically extremely low. These factors result in a very different environment for algae than found in neutral and acid-rain impacted lakes. The planktonic algal flora is generally dominated by flagellates belonging to genera of Chlorophyta (Chlamydomonas), Heterokontophyta of the class Chrysophyceae (Ochromonas, Chromulina), Cryptophyta (Cyathomonas) and Euglenophyta (Lepocinclis, Euglena mutabilis). Near-spherical non-motile Chlorophyta (Nanochlorum sp.), Heterokontophyta of the class Bacillariophyceae (Eunotia exigua, Nitzschia), Dinophyta (Gymnodinium, Peridinium umbonatum), other Chlorophyta (Scourfieldia cordiformis) and Cryptophyta (Rhodomonas minuta) are also found.[PUBLICATION ABSTRACT]</description><subject>Acid mine drainage</subject><subject>Acid rain</subject><subject>Algae</subject><subject>Dissolved inorganic carbon</subject><subject>Flora</subject><subject>Lakes</subject><subject>Lignite</subject><subject>Limnology</subject><subject>Phytoplankton</subject><subject>Plankton</subject><subject>Pyrite</subject><subject>Taxonomy</subject><issn>0018-8158</issn><issn>1573-5117</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNotjT1PwzAURS0EEqEws1pMMATee44TB8FQVdAiRQIJmCvj2CRtvkgclfx7imC6wzk6l7FzhGsEEjfzWwSIAFVCpFJ1wAKUiQglYnLIAtiDUKFUx-xkGDYAkKQEAXt9KSbfdpVutr5teOu4Lyy33763ta0mrk2Zl4bXZVM2n7zSWzv8Stk4aF9qfrm0fa2b6YrvSl_wbsXv7sUpO3K6GuzZ_87Y--PD22IVZs_Lp8U8Cw1R7EOXp9IRCutyo7WE3KaEmCo0SpBzGsHENpGAIiZFUawiYcEQ0kcsjdAoZuzir9v17ddoB7_etGPf7C_XijCKUxUl4gd8qlAR</recordid><startdate>20000801</startdate><enddate>20000801</enddate><creator>Lessmann, Dieter</creator><creator>Fyson, Andrew</creator><creator>Nixdorf, Brigitte</creator><general>Springer Nature B.V</general><scope>3V.</scope><scope>7QG</scope><scope>7QH</scope><scope>7SN</scope><scope>7SS</scope><scope>7U7</scope><scope>7UA</scope><scope>88A</scope><scope>8AO</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H95</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>LK8</scope><scope>M7N</scope><scope>M7P</scope><scope>P64</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>RC3</scope></search><sort><creationdate>20000801</creationdate><title>Phytoplankton of the extremely acidic mining lakes of Lusatia (Germany) with pH <=3</title><author>Lessmann, Dieter ; 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Of 32 lakes regularly studied from 1995 to 1998, 14 have a pH <3 (median pH 2.3-2.9). These lakes are typically buffered by high concentrations of Fe (III) and have high conductivity (1000-5000 μS cm^sup -1^). Concentrations of dissolved inorganic carbon (DIC) and phosphorus are typically extremely low. These factors result in a very different environment for algae than found in neutral and acid-rain impacted lakes. The planktonic algal flora is generally dominated by flagellates belonging to genera of Chlorophyta (Chlamydomonas), Heterokontophyta of the class Chrysophyceae (Ochromonas, Chromulina), Cryptophyta (Cyathomonas) and Euglenophyta (Lepocinclis, Euglena mutabilis). 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subjects | Acid mine drainage Acid rain Algae Dissolved inorganic carbon Flora Lakes Lignite Limnology Phytoplankton Plankton Pyrite Taxonomy |
title | Phytoplankton of the extremely acidic mining lakes of Lusatia (Germany) with pH <=3 |
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