Issue Date
1995-01-01Keywords
North Seaglacial features
fjords
Kattegat
Skagerrak
Denmark
modern
shore features
Atlantic Ocean
North Atlantic
sea water
marine environment
isotope ratios
Holocene
Europe
Western Europe
Scandinavia
Cenozoic
Quaternary
C 14
carbon
dates
isotopes
radioactive isotopes
shells
Invertebrata
Mollusca
C 13 C 12
stable isotopes
absolute age
Metadata
Show full item recordCitation
Heier-Nielsen, S., Heinemeier, J., Nielsen, H. L., & Rud, N. (1995). Recent reservoir ages for Danish fjords and marine waters. Radiocarbon, 37(3), 875-882.Journal
RadiocarbonDescription
From the 15th International Radiocarbon Conference held in Glasgow, Scotland, August 15-19, 1994.Additional Links
http://radiocarbon.webhost.uits.arizona.edu/Abstract
AMS 14C dates were measured for 28 mollusk shells collected live in Danish waters over the period AD 1885 to 1945. Fourteen samples were from fjords and 14 were marine samples from the Danish Skagerrak-Kattegat coastal area and from the Belts. Reservoir ages were calculated for all samples on the basis of the tree-ring calibration curve. For the marine samples, which cover the period AD 1885-1916, we found a weighted-average reservoir age of 377 +/16 yr. The marine Delta-R values (the difference between the measured 14C age and the age deduced from marine, mixed-layer model calculation of Stuiver, Pearson and Braziunas (1986)) were found to be uniform within the experimental uncertainty with a weighted average of Delta-R = 13 +/16yr. Based on the observed scatter, the standard deviation is 21 yr. This result shows that it is justified to use the marine calibration curve with standard parameters (Delta-R = 0) when 14C-dating marine samples from the Danish area. Our value is consistent with the result Delta-R = -33 +/27 yr previously found for the Norwegian and Swedish Skagerrak-Kattegat coasts. In contrast, reservoir ages for Danish fjords were found to vary from 400 to >900 yr, far beyond experimental uncertainty. We ascribe this to varying content of dissolved, old soil carbonate (hard-water effect). Therefore, dating of samples from such fjord environments is expected to be uncertain by several hundred years.Type
Proceedingstext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200014958