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"In order to build up a calendar time scale (i.e., varve chronology) for the Suigetsu (SG) core, a total of 85 subsamples were taken in a section of SG extending from 10.43 to 30.34 m below the top sediment, each ca.25 cm in length, including a 1.5 cm overlap with neighbouring subsamples.One of the products of the continuing cycles of the seasons can be found on the bottoms of some lakes.Each spring, tiny plants bloom in Lake Suigetsu, a small body of water in Japan.When these one-cell algae die, they drift down, shrouding the lake floor with a thin, white layer.
Continuous lines show the German oak and pine chronologies fixed by comparison with the varve chronology of Lake Suigetsu.
In order to reconstruct a more precise and longer varve chronology for the laminated sediments from Lake Suigetsu, we have reassessed the varve chronology in the whole section during the deglaciation as well as the Glacial up to a depth of 30.45 m.
The uncertainty in the varve chronology comes from two sources: core sampling and varve counting. Since the varve ages from below 18 m (corresponding to ca.
At the extremes there is a range from 10,447 to 11,700 year B. And evidence that properly conducted C14 radiometric dating can approach reasonable accuracy, possibly within better than 10 percent.
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