Introductory post on Mia Tiljander's paper
The study of Lake Korttajärvi in Central Finland was carried out by Mia Tiljander as her academic dissertation on the Holocene sedimentary history of that lake. The dissertation is available in full at the reference provided below.
Confidence in the conclusion that the laminae in Lake Korttajärvi represent varves was provided by a number of analyses, beginning with the nature of deposits that are being made presently:
The varve year begins when a light mineral lamina deposits in the spring. The mineral lamina becomes gradually mixed with organic matter in summer and autumn. At the end of the varve year (winter) black organic matter deposits under the ice cover.
Source: Mia Tiljander, Holocene sedimentary history of annual laminations of Lake Korttajärvi, central Finland, Helsinki 2005. Full paper available at -
http://ethesis.helsinki.fi/julkaisut/mat/geolo/vk/tiljander/holocene.pdf
The seasonal nature of the depositional pattern was verified by mineral- and palaeomagnetic measurements, including natural remanent magnetization, anhysteric remanent magnetization and isothermal remanent magnetization. These analyses were backed-up with stable isotope examination. The Korttajärvi varves were correlated with independent varve cores from Lakes Alimmainen Savijärvi and Nautajärvi, which supported conclusions about the chrononlogy represented by the Korttajärvi varves.
Study of the pattern of sedimentation showed strong correlations with known climatological variations from recent history and from more distant history as well, such that mineral- and organic-rich depositional periods could be identified alternating in intervals of from decades to centuries, correlations that matched similar evidence from other studies. Climate-dependent depositional patterns could be identified for the Medieval Warm period from 980-1250 AD, as well as for periods corresponding to 140-220 AD, 1688-1486 BC and 1846-1704 BC.
Severe climatic conditions were reflected in the sedimentation history for 3061-3037 BC, 1877-1848 BC and 907-875 BC. The latter dates coincide with an abrupt climate cooling that is known to have taken place at about that time in Western Europe. Increased mineral deposition was also noted for the periods 1580-1630 AD and 1650-1710 AD. Disturbances in sedimentation caused by increases in farming activity in the area in the early 18th century could also be identified. Chronologies were verified by carbon and hydrogen isotope studies.
So given this weight of evidence from Lake Korttajärvi varve sequences it is reasonable to conclude that varves are exactly what geologists understand them to be, seasonally deposited annually recurring lamina.
However, various factors can impact upon the count of varve sequences, such as depositional variations (changes in climate, increases in human activity in the locality, changes in the lake itself) and/or periods of disturbance in the varve-forming sequence caused by bioturbation or currents and/or counting errors inherent in the process itself, but these are variations understood and taken into account by geologists. This is why varve chronologies are quoted with error bars, for example the Lake Alimmainen Savijärvi varve record covers 10,295 +/-340 varve years, the Lake Nautajärvi record 9,898 +/-97 varve years, and the Lake Korttajärvi record 9,590 +/-103 varve years.
All data from Tiljander, op. cit.
This brief survey conclusively demonstrates that 'young Earth' chronologies that place the age of Earth at less than 7,000 years are seriously awry.