Björn Berglund
Professor emeritus
Holocene organic carbon burial rates in the Baltic coast
Författare
Summary, in English
To estimate Holocene changes in organic carbon mass accumulation rates (Corg MARs) in the
southeastern Swedish Baltic Sea, two sediment cores were studied in combination with biogeochemical
modelling. Prior to 11 300 cal. BP, Corg MARs were extremely low, indicating low organic matter production
on the catchment of the Baltic Ice Lake. Following a brief regression, the Ancylus Lake stage occurred
between 11 100 and 9800 cal. BP. Corg MARs increased substantially during this period because of
enhanced washing in of terrestrial organic matter, when boreal forests were initially established. The
prominent marine stage, known as the Littorina transgression between 8500 and 3000 cal. BP, is marked
by a minor increase in Corg MARs. Our modelling reveals a changing terrestrial organic carbon input
between 100 and 1000 g/m2 per yr that accounts for 30–80% of total organic carbon in sediments of the
southeastern Swedish Baltic Sea, with maximum values (c. 20 x 103 g/m2 per yr) occurring during the
Bronze/Iron Age transition at about 3000 cal. BP. Corg MAR in the entire Baltic basin is estimated at
3.01 x 106 t/yr during the pre-industrial Holocene, comparable with other large inland water bodies.
Regardless of the source of carbon, our data indicate that the Baltic basin is an important sedimentary
reservoir for organic carbon storage and thus should be included in accounting for global terrestrial carbon
cycling during the pre-industrial Holocene.
southeastern Swedish Baltic Sea, two sediment cores were studied in combination with biogeochemical
modelling. Prior to 11 300 cal. BP, Corg MARs were extremely low, indicating low organic matter production
on the catchment of the Baltic Ice Lake. Following a brief regression, the Ancylus Lake stage occurred
between 11 100 and 9800 cal. BP. Corg MARs increased substantially during this period because of
enhanced washing in of terrestrial organic matter, when boreal forests were initially established. The
prominent marine stage, known as the Littorina transgression between 8500 and 3000 cal. BP, is marked
by a minor increase in Corg MARs. Our modelling reveals a changing terrestrial organic carbon input
between 100 and 1000 g/m2 per yr that accounts for 30–80% of total organic carbon in sediments of the
southeastern Swedish Baltic Sea, with maximum values (c. 20 x 103 g/m2 per yr) occurring during the
Bronze/Iron Age transition at about 3000 cal. BP. Corg MAR in the entire Baltic basin is estimated at
3.01 x 106 t/yr during the pre-industrial Holocene, comparable with other large inland water bodies.
Regardless of the source of carbon, our data indicate that the Baltic basin is an important sedimentary
reservoir for organic carbon storage and thus should be included in accounting for global terrestrial carbon
cycling during the pre-industrial Holocene.
Avdelning/ar
- Kvartärgeologi
Publiceringsår
2007
Språk
Engelska
Sidor
673-681
Publikation/Tidskrift/Serie
The Holocene
Volym
17
Issue
5
Dokumenttyp
Artikel i tidskrift
Förlag
SAGE Publications
Ämne
- Geology
Nyckelord
- Holocene
- southeastern Sweden
- carbon cycling.
- organic carbon burial rates
- Baltic Sea
- early diagenesis
Status
Published
ISBN/ISSN/Övrigt
- ISSN: 0959-6836