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Meromictic lake
Permanently stratified lake with layers of water that do not intermix

A meromictic lake is a type of lake with layers of water that do not mix, unlike typical holomictic lakes, which experience annual mixing of surface and deep waters. The term meromictic was introduced by Austrian scientist Ingo Findenegg in 1935, derived from the older term holomictic. The understanding and terminology of meromictic lakes were largely developed with contributions from G. Evelyn Hutchinson in 1937, establishing foundational concepts still used today in limnology.

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Characteristics

Most lakes are holomictic: at least once per year, the surface and the deep waters mix. In monomictic lakes, the mixing occurs once per year; in dimictic lakes, it occurs twice a year (typically spring and autumn), and in polymictic lakes, the mixing occurs several times a year. In meromictic lakes, the layers of water can remain unmixed for years, decades, or centuries.

Meromictic lakes can usually be divided into three sections or layers. The bottom layer is the monimolimnion; the waters in this portion of the lake circulate little, and are generally hypoxic and more saline than the rest of the lake. The top layer is the mixolimnion, and essentially behaves like a holomictic lake. The area in between is the chemocline, or chemolimnion.6

The lack of mixing between layers creates radically different environments for life: the stratification, or stable layering, of lake waters means that the bottom layer receives little oxygen from the atmosphere, hence becomes depleted of oxygen. While the surface layer may have 10 mg/L or more dissolved oxygen in summer, the depths of a meromictic lake can have less than 1 mg/L.7 Very few organisms can live in such an oxygen-poor environment. One exception is purple sulfur bacteria. These bacteria, commonly found at the top of the monimolimnion in such lakes, use sulfur compounds such as sulfides in photosynthesis. These compounds are produced by decomposition of organic sediments in oxygen-poor environments. The monimolimnion is often rich in phosphorus and nitrogen. These factors combine to create an ideal environment for bacterial growth. The mixolimnion can have similar qualities. However, the types of bacteria that can grow at the surface are determined by the amount of light received at the surface.8

A meromictic lake may form because the basin is unusually deep and steep-sided compared to the lake's surface area, or because the lower layer of the lake is highly saline and denser than the upper layers of water.9 However, human influence can lead to cultural meromixis occurring.101112 The increased use of road salt as a deicing strategy, particularly in northern latitude regions, can disturb the natural mixing cycles in lakes by inhibiting mixing.1314 As salt is flushed into aquatic systems at high concentrations in late winter/early spring, it accumulates in the deepest layer of lakes leading to incomplete mixing.

Stratification in meromictic lakes can be either endogenic or ectogenic. Endogenic means the patterns seen in the lake are caused by internal events, such as organic matter accumulating in the sediments and decaying, whereas ectogenic means the patterns seen are caused by external causes, like an intrusion of saltwater settling in the hypolimnion, preventing it from mixing.15

The layers of sediment at the bottom of a meromictic lake remain relatively undisturbed because there is little physical mixing and few living organisms to agitate them. There is also little chemical decomposition. For this reason, cores of the sediment at the bottom of meromictic lakes are important in tracing past changes in climate at the lake, by examining trapped pollen grains and the types of sediments [see Proxy (climate)].

When the layers do mix for whatever reason, the consequences can be devastating for organisms that normally live in the mixolimnion. This layer is usually much smaller in volume than the monimolimnion. When the layers mix, the oxygen concentration at the surface will decrease dramatically. This can result in the death of many organisms, such as fish, that require oxygen.

Occasionally, carbon dioxide, methane, or other dissolved gases can build up relatively undisturbed in the lower layers of a meromictic lake. When the stratification is disturbed, as could happen from an earthquake, a limnic eruption may result. In 1986, a notable event of this type took place at Lake Nyos in Cameroon, causing nearly 1,800 deaths.161718 In the following decades after this disaster, active research and management has been done to mitigate gas buildup in the future through the Nyos Organ Pipes Program (NOPP).19 The NOPP program placed large organ pipes into Lake Nyos, to reach the monimolimnion where harmful dissolved gases built up, that allow for gas release to the atmosphere, effectively degassing the monimolimnion.20 Since 2019, Lake Nyos has successfully been degassed to a nonhazardous concentration of dissolved gas.21 Paralleling Lake Nyos, Lake Kivu is another lake that poses a potentially fatal threat to the community. Some management strategies have suggested taking a different approach, moving gases from the monimolimnion to the mixolimnion, rather than degassing to the atmosphere through organ pipes.22

While it is mainly lakes that are meromictic, the world's largest meromictic basin is the Black Sea. The deep waters below 50 m (160 ft) do not mix with the upper layers that receive oxygen from the atmosphere. As a result, over 90% of the deeper Black Sea volume is anoxic water. The Caspian Sea is anoxic below 100 m (330 ft). The Baltic Sea is persistently stratified, with dense, highly saline water comprising the bottom layer, and large areas of hypoxic sediments (see Baltic Sea hypoxia).

List of meromictic lakes

There are meromictic lakes all over the world. The distribution appears to be clustered, but this may be due to incomplete investigations. Depending on the exact definition of "meromictic", the ratio between meromictic and holomictic lakes worldwide is around 1:1000.23

Africa

Antarctica

Asia

Australia

Europe

North America

See also

Wikimedia Commons has media related to Meromictic lakes. Look up meromictic lake or monimolimnion in Wiktionary, the free dictionary.

References

  1. Wetzel, Robert G. (2001). Limnology: Lake and River Ecosystems (Third ed.). New York: Academic Press. ISBN 978-0-12-744760-5. 978-0-12-744760-5

  2. Lewis, William M. Jr. (1983). "A revised classification of lakes based on mixing" (PDF). Canadian Journal of Fisheries and Aquatic Sciences. 40 (10): 1779–1787. doi:10.1139/f83-207. Archived from the original (PDF) on 6 March 2009. https://web.archive.org/web/20090306140542/http://cires.colorado.edu/limnology/pubs/pdfs/Pub058.pdf

  3. Hakala, Anu (27 February 2004). "Meromixis as a part of lake evolution – observations and a revised classification of true meromictic lakes in Finland" (PDF). Boreal Environment Research. 9: 37–53. ISSN 1239-6095. http://www.borenv.net/BER/pdfs/ber9/ber9-037.pdf

  4. Findenegg, Ingo (1935). "Limnologische Untersuchungen im Kärntner Seengebiete. Ein Beitrag zur Kenntnis des Stoffhaushaltes in Alpenseen". Internationale Revue der Gesamte Hydrobiologie (in German). 32: 369–423. As cited by Hakala (2004).

  5. Hutchinson, G. Evelyn (1937). "A contribution to the limnology of arid regions". Transactions of the Connecticut Academy of Arts and Sciences. 33: 47–132. As cited by Hakala (2004).

  6. Walker, K. F. (March 1974). "The Stability of Meromictic Lakes in Central Washington". Limnology and Oceanography. 19 (2): 209–222. Bibcode:1974LimOc..19..209W. doi:10.4319/lo.1974.19.2.0209. JSTOR 2834407. /wiki/Bibcode_(identifier)

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  15. Wetzel, Robert G. (2001). Limnology: Lake and River Ecosystems (Third ed.). New York: Academic Press. ISBN 978-0-12-744760-5. 978-0-12-744760-5

  16. Krajick, Kevin (28 March 2003). "Africa's Davids and Goliaths". Science. 299 (5615): 2024–2026. doi:10.1126/science.299.5615.2024. ISSN 0036-8075. PMID 12663915. https://www.science.org/doi/10.1126/science.299.5615.2024

  17. Boehrer, Bertram; Saiki, Kazuto; Ohba, Takeshi; Tanyileke, Greg; Rouwet, Dmitri; Kusakabe, Minoru (28 July 2021). "Carbon Dioxide in Lake Nyos, Cameroon, Estimated Quantitatively From Sound Speed Measurements". Frontiers in Earth Science. 9. doi:10.3389/feart.2021.645011. ISSN 2296-6463. https://doi.org/10.3389%2Ffeart.2021.645011

  18. Tassi, Franco; Rouwet, Dmitri (12 February 2014). "An overview of the structure, hazards, and methods of investigation of Nyos-type lakes from the geochemical perspective". Journal of Limnology. 73 (1). doi:10.4081/jlimnol.2014.836. ISSN 1723-8633. http://www.jlimnol.it/index.php/jlimnol/article/view/jlimnol.2014.836

  19. Halbwachs, Michel; Sabroux, Jean-Christophe; Kayser, Gaston (2020). "Final step of the 32-year Lake Nyos degassing adventure: Natural CO2 recharge is to be balanced by discharge through the degassing pipes". Journal of African Earth Sciences. 167: 103575. doi:10.1016/j.jafrearsci.2019.103575. https://doi.org/10.1016%2Fj.jafrearsci.2019.103575

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