Varve

A varve is an annual layer of sediment or sedimentary rock.

The word 'varve' derives from the Swedish word varv whose meanings and connotations include 'revolution', 'in layers', and 'circle'. The term first appeared as Hvarfig lera (varved clay) on the first map produced by the Geological Survey of Sweden in 1862.^[1] Initially, "varve" referred to each of the separate components comprising a single annual layer in glacial lake sediments, but at the 1910 Geological Congress, the Swedish geologist Gerard De Geer (1858–1943) proposed a new formal definition, where varve means the whole of any annual sedimentary layer.^[2] More recently introduced terms such as 'annually laminated' are synonymous with varve.

Of the many

An annual layer can be highly visible because the particles washed into the layer in the spring when there is greater flow strength are much coarser than those deposited later in the year. This forms a pair of layers—one coarse and one fine—for each annual cycle. Varves form only in

Although the term varve was not introduced until the late nineteenth century, the concept of an annual rhythm of deposition is at least two centuries old. In the 1840s, Edward Hitchcock suspected laminated sediment in North America could be seasonal, and in 1884 Warren Upham postulated that light-dark laminated couplets represented a single year's deposition. Despite these earlier forays, the chief pioneer and populariser of varve research was Gerard De Geer. While working for the Geological Survey of Sweden, De Geer noticed a close visual similarity between the laminated sediments he was mapping, and tree-rings. This prompted him to suggest the coarse-fine couplets frequently found in the sediments of glacial lakes were annual layers.

The first varve chronology was constructed by De Geer in Stockholm in the late 19th century. Further work soon followed, and a network of sites along the east coast of Sweden was established. The varved sediments exposed in these sites had formed in glaciolacustrine and glacimarine conditions in the Baltic basin as the last ice sheet retreated northwards. By 1914, De Geer had discovered that it was possible to compare varve sequences across long distances by matching variations in varve thickness, and distinct marker laminae. However, this discovery led De Geer and many of his co-workers into making incorrect correlations, which they called 'teleconnections', between continents, a process criticised by other varve pioneers like Ernst Antevs.

In 1924, the Geochronological Institute, a special laboratory dedicated to varve research was established. De Geer and his co-workers and students made trips to other countries and continents to investigate varved sediments. Ernst Antevs studied sites from Long Island, U.S.A. to Lake Timiskaming and Hudson Bay, Canada, and created a North American varve chronology. Carl Caldenius visited Patagonia and Tierra del Fuego, and Erik Norin visited central Asia. By this stage, other geologists were investigating varve sequences, including Matti Sauramo who constructed a varve chronology of the last deglaciation in Finland.

1940 saw the publication of a now classic scientific paper by De Geer, the Geochronologia Suecica, in which he presented the Swedish Time Scale, a floating varve chronology for ice recession from

In 2008, although varves were considered likely to give similar information to dendrochronology, they were considered "too uncertain" for use on a long-term timescale.^[3] However, by 2012, “missing” varves in the Lake Suigetsu sequence were identified in the Lake Suigetsu 2006 Project by overlapping multiple cores and improved varve counting techniques, extending the timescale to 52,800 years.^[4][5]

Formation

Varves form in a variety of

The classic varve archetype is a light / dark coloured couplet deposited in a glacial lake. The light layer usually comprises a coarser laminaset, a group of conformable laminae, consisting of silt and fine sand deposited under higher energy conditions when meltwater introduces sediment load into the lake water. During winter months, when meltwater and associated suspended sediment input is reduced, and often when the lake surface freezes, fine clay-size sediment is deposited forming a dark coloured laminaset.

In addition to seasonal variation of sedimentary processes and deposition, varve formation requires the absence of

A well-known marine example of varved sediments are those found in the Santa Barbara basin, off California.^[6] Another long record of varved sediments is the palaeo-lacustrine record of the Piànico–Sèllere Basin (southern Alps).^[7] Here, the detrital layer part of each varve was used as a proxy for 771 palaeofloods which occurred over a period of 9.3 thousand years during an interglacial period in the Pleistocene.^[8][9]

See also

• Dendrochronology – Method of dating based on the analysis of patterns of tree rings
• Dendroclimatology – Science of determining past climates from trees
• Rhythmite – Layers of sediment or sedimentary rock laid down with periodicity and regularity

References

Further reading

• De Geer, G. (1940), Geochronologia Sueccia Principles. Kungl. Svenska Vetenskapsakademiens Handlingar, Tredje Serien. Band 18 No.6.
• Lowe, J.J. and Walker, M.J.C. (1984), Reconstructing Quaternary Environments. Longman Scientific and Technical.
• Sauramo, M. (1923), Studies on the Quaternary varve sediments in southern Finland. Comm. Geol. Finlande Bulletin 60.
• Wohlfarth, B. (1996), The chronology of the Last Termination: A review of radiocarbon-dated, high-resolution terrestrial stratigraphies. Quaternary Science Reviews 15 pp. 267–284.

The Wikibook Historical Geology has a page on the topic of: Varves

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