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Titel Paleoenvironmental reconstruction using nitrogen and carbon contents and isotopes in lake sediments of Tiefer See, NE Germany
VerfasserIn Birgit Plessen, Ulrike Kienel, Nadine Dräger, Achim Brauer
Konferenz EGU General Assembly 2016
Medientyp Artikel
Sprache en
Digitales Dokument PDF
Erschienen In: GRA - Volume 18 (2016)
Datensatznummer 250127173
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2016-7016.pdf
 
Zusammenfassung
Lake Tiefer See (Mecklenburg/Germany) is a seasonally stratified lake formed in a north-south directed subglacial channel system with a maximum depth of 63 m. In order to understand the lake productivity and nitrogen cycle depending on natural variability and anthropogenic forcing, we compared the recent input and productivity, monitored in sediment traps in the hypo-, meta- and epilimnion since 2012 with the sedimentary record of the last 400 years. Light stable isotopes of nitrogen and carbon are interpreted to reflect human impact by extensive land use, manure, sewage input, and atmospheric nitrogen compounds. The sediment trap material clearly shows high $\delta ^{15}$N (+7 to +14\permil\ ), and low $\delta ^{13}$C$_{org}$ (-28 to -33\permil\ ) values, whereas surface soil and terrestrial plant materials are characterised by lower $\delta ^{15}$N (+3 to +6\permil\ ), and higher $\delta ^{13}$C$_{org}$ (-28 to -25\permil\ ) values. Recent high $\delta ^{15}$N$_{NO$_3$} values of up to +15\permil\ in the epilimnion water together with low $\delta ^{18}$O $