Inland sea (geology)

Short description: Shallow sea within continental land areas

An inland sea (also known as an epeiric sea or an epicontinental sea) is a continental body of water which is very large in area and is either completely surrounded by dry land or connected to an ocean by a river, strait or "arm of the sea". An inland sea will generally have higher salinity than a freshwater lake, but usually lower salinity than seawater.

## Contents

* 1 Definition
* 2 Modern inland seas
* 3 Former epicontinental seas in Earth's history
* 4 See also
* 5 Notes
* 6 References
* 7 External links

## Definition

What constitutes an "inland sea" is complex and somewhat necessarily vague.[1] The United States Hydrographic Office defined it as "a body of water nearly or completely surrounded by land, especially if very large or composed of salt water".[2]

Geologic engineers Heinrich Ries and Thomas L. Watson say an inland sea is merely a very large lake.[1] Rydén, Migula, and Andersson[3] and Deborah Sandler of the Environmental Law Institute add that an inland sea is "more or less" cut off from the ocean.[4][3] It may be semi-enclosed,[3] or connected to the ocean by a strait or "arm of the sea".[4] An inland sea is distinguishable from a bay in that a bay is directly connected to the ocean.[4]

The term "epeiric sea" was coined by Joseph Barrell in 1917. He defined an epeiric sea as a shallow body of water whose bottom is within the wave base (e.g., where bottom sediments are no longer stirred by the wave above).[5] An epeiric sea as one with limited connection to an ocean,[6][7][3] and shallow.[3][lower-alpha 1] An inland sea is only an epeiric sea when a continental interior is flooded by marine transgression due to sea level rise or epeirogenic movement.[5][8]

An epicontinental sea is synonymous with an epeiric sea.[8] The term "epicontinental sea" may also refer to the waters above a continental shelf. This is a legal, not geological, term.[9] Epeiric, epicontinental, and inland seas occur on a continent, not adjacent to it.[3]

The law of the sea does not apply to inland seas.[10]

## Modern inland seas

This 1827 map of Australia depicts a 'Great River' and a 'Supposed Sea' that both proved nonexistent.

In modern times, continents stand high, eustatic sea levels are low, and there are few inland seas.

* The Marmara Sea located in modern-day Turkey is surrounded by land all around, except where it connects the two Turkish Straits, the Bosphorus and the Dardanelles.
* The Baltic Sea is a brackish inland sea, arguably the largest body of brackish water in the world. Other possibilities include the White Sea and the northern half of the Black Sea (its deep southern basin is a closed-off relic of the now-vanished Tethys Sea).[11] The origin of the Baltic Sea basin is not clear as there are differing views on the role of erosion and tectonics.[12]
* Hudson Bay, including James Bay at its southern end, reaches within the North American continent from Baffin Island, Nunavut in the north to Quebec, Ontario and Manitoba in the south. The bay shares some similarities with the Gulf of Bothnia in Fennoscandia; it lies in the middle of a shield and it was the centre of an ice sheet during the Quaternary glaciations. However, the origin of both depressions is unrelated to glacier erosion.[13]
* The Seto Inland Sea in Japan is not a true inland sea but rather a body of water separating Honshū, Shikoku, and Kyūshū, three of the four main islands of Japan.
* The Caspian Sea is a very large, inland body of water at least hundreds of miles from the nearest part of the World Ocean (such as the Persian Gulf) and has some characteristics of the sea, like being composed of at least a good portion of saltwater. However, it is also considered the largest lake in the world.
* The Great Lakes, despite being completely fresh water, have historically been referred to as inland seas due to possessing sea-like characteristics.[14][15]

Modern examples might also include the recently (less than 10,000 years ago) reflooded Persian Gulf, and the South China Sea that presently covers the Sunda Shelf.[lower-alpha 2]

## Former epicontinental seas in Earth's history

At various times in the geologic past, inland seas covered central areas of continents during periods of high sea level that result in marine transgressions. Inland seas have been greater in extent and more common than at present.

* During the Oligocene and Early Miocene large swathes of Patagonia were subject to a marine transgression. The transgression might have temporarily linked the Pacific and Atlantic oceans, as inferred from the findings of marine invertebrate fossils of both Atlantic and Pacific affinity in La Cascada Formation.[16][17] Connection would have occurred through narrow epicontinental seaways that formed channels in a dissected topography.[16][18]
* A vast inland sea, the Western Interior Seaway, extended from the Gulf of Mexico deep into present-day Canada during the Cretaceous.
* At the same time, much of the low plains of modern-day northern France and northern Germany were inundated by an inland sea, where the chalk was deposited that gave the Cretaceous Period its name.
* The Amazon, originally emptying into the Pacific, as South America rifted from Africa, found its exit blocked by the rise of the Andes about 15 million years ago. A great inland sea developed, at times draining north through what is now Venezuela before finding its present eastward outlet into the South Atlantic. Gradually this inland sea became a vast freshwater lake and wetlands where sediment flattened its profiles and the marine inhabitants adapted to life in freshwater. Over 20 species of stingray, most closely related to those found in the Pacific Ocean, can be found today in the freshwaters of the Amazon, which is also home to a freshwater dolphin. In 2005, fossilized remains of a giant crocodilian, estimated to have been 46 ft (14 m) in length, were discovered in the northern rainforest of Amazonian Peru.[19]
* In Australia, the Eromanga Sea existed during the Cretaceous Period. It covered large swaths of the eastern half of the continent.[20][lower-alpha 3]

## See also

* Earth:Endorheic basin - Closed drainage basin that has no outflow
* Earth:Mediterranean sea (oceanography) - Mostly enclosed sea with limited exchange with outer oceans

## Notes

1. ↑ Geologist Richard A. Matzner defines shallow as usually under 250 metres (820 ft) in depth.[6] Rydén, Migula, and Andersson do not define shallow, but cite examples of inland seas with a depth of 100 metres (330 ft) or less.[3]
2. ↑ The Lord Howe Rise that covers much of the sunken "continent" of Zealandia and the largely submerged Mascarene Plateau that includes the Granitic Group islands of the Seychelles could not be considered "inland".
3. ↑ Also in Australia the promise of an inland sea is often said to have been one of the prime motives of inland exploration during the 1820s and 1830s. Although this theory was championed by the explorer Charles Sturt, it enjoyed little support among the other explorers, most of whom were more inclined to believe in the existence of a Great River which discharged into the ocean in the north-west corner of the continent.[21]

## References

1. ↑ 1.0 1.1 Ries, Heinrich; Watson, Thomas L. (1947). Elements of Engineering Geology. New York: J. Wiley & Sons. p. 286. ISBN 9785877732124. OCLC 486745. https://books.google.com/books?id=F8MOAwAAQBAJ.
2. ↑ United States Hydrographic Office (1956). Navigation Dictionary. Washington, D.C.: Supintendent of Documents. p. 189. OCLC 3040490. https://books.google.com/books?id=RNKMJykFRCkC.
3. ↑ 3.0 3.1 3.2 3.3 3.4 3.5 3.6 Rydén, Lars; Migula, Pawel; Andersson, Magnus (2003). Environmental Science: Understanding, Protecting, and Managing the Environment in the Baltic Sea Region. Uppsala: Baltic University Press. p. 123. ISBN 9789197001700. https://books.google.com/books?id=VIopLSQyI5MC.
4. ↑ 4.0 4.1 4.2 Sandler, Deborah (1994). Protecting the Gulf of Aqaba: A Regional Environmental Challenge. Washington, D.C.: Environmental Law Institute. p. 45. ISBN 9780911937466. https://books.google.com/books?id=EeSqklMsgSwC.
5. ↑ 5.0 5.1 Pratt, Brian R.; Holmden, Chris (2007). Dynamics of Epeiric Seas. St. John's, Newfoundland and Labrador, Canada: Geological Association of Canada. p. 1. ISBN 9781897095348.
6. ↑ 6.0 6.1 Matzner, Richard A., ed (2020). Dictionary of Geophysics, Astrophysics, and Astronomy. Boca Raton: CRC Press. p. 156. ISBN 9780367455279. https://books.google.com/books?id=v4bLBQAAQBAJ.
7. ↑ Morris, Christopher, ed (1992). Academic Press Dictionary of Science and Technology. San Diego: Academic Press. p. 757. ISBN 9780122004001. https://books.google.com/books?id=nauWlPTBcjIC.
8. ↑ 8.0 8.1 Monkhouse, Francis J. (2008). A Dictionary of Geography. New Brunswick, N.J.: Aldine Transaction. p. 124. ISBN 9780202361314. https://books.google.com/books?id=4lYPEAAAQBAJ.
9. ↑ Zaklin, Ralph (1974). The Changing Law of the Sea: Western Hemisphere Perspectives. Leiden, Netherlands: Sijthoff. p. 109. ISBN 9789028600843. https://books.google.com/books?id=j5CkK_2TPf4C.
10. ↑ Galletti, Florence (2015). "Transformations in International Law of the Sea: Governance of the Space or Resource". Governance of Seas and Oceans. London: Wiley. p. 31. ISBN 9781848217805. https://books.google.com/books?id=9WPhCgAAQBAJ.
11. ↑ "Baltic Sea Portal". http://www.fimr.fi/en/tietoa/yleiskuvaus/en_GB/yleiskuvaus/.
12. ↑ Šliaupa, Salius; Hoth, Peer (2011). "Geological Evolution and Resources of the Baltic Sea Area from the Precambrian to the Quaternary". The Baltic Sea Basin. Springer. ISBN 978-3-642-17219-9.
13. ↑ Lidmar-Bergström, Karna (1997). "A long-term perspective on glacial erosion". Earth Surface Processes and Landforms 22 (3): 297–306. doi:10.1002/(SICI)1096-9837(199703)22:3<297::AID-ESP758>3.0.CO;2-R. Bibcode: 1997ESPL...22..297L.
14. ↑ Rao, Yerubandi R.; Schwab, David J. (2007-01-01). "Transport and Mixing Between the Coastal and Offshore Waters in the Great Lakes: a Review" (in en). Journal of Great Lakes Research 33 (1): 202–218. doi:10.3394/0380-1330(2007)33[202:TAMBTC2.0.CO;2]. ISSN 0380-1330. https://www.sciencedirect.com/science/article/pii/S0380133007700485.
15. ↑ "Great Lakes and Inland Seas | U.S. Geological Survey". https://www.usgs.gov/science/science-explorer/ocean/great-lakes-and-inland-seas.
16. ↑ 16.0 16.1 "Geochronologic and paleontologic evidence for a Pacific–Atlantic connection during the late Oligocene–early Miocene in the Patagonian Andes (43–44°S)". Journal of South American Earth Sciences 55: 1–18. 2014. doi:10.1016/j.jsames.2014.06.008. Bibcode: 2014JSAES..55....1E.
17. ↑ "Cenozoic Strombidae, Aporrhaidae, and Struthiolariidae (Gastropoda, Stromboidea) from Chile: their significance to biogeography of faunas and climate of the south-east Pacific". Journal of Paleontology 79: 1120–1130. 2005. doi:10.1666/0022-3360(2005)079[1120:csaasg2.0.co;2].
18. ↑ "Neogene uplift of central eastern Patagonia: Dynamic response to active spreading ridge subduction?". Tectonics 28. 2009.
19. ↑ "Peru finds giant crocodile fossil in Amazon". Daily Times. 12 September 2005. http://www.dailytimes.com.pk/default.asp?page=story_12-9-2005_pg6_6.
20. ↑ Clode, Danielle (August 2015). Prehistoric marine life in Australia's inland sea. Museum Victoria. ISBN 978-1-921833-16-8. OCLC 895759221. http://worldcat.org/oclc/895759221.
21. ↑ Cathcart, Michael (2009). The Water Dreamers: How Water and Silence Shaped Australia. Melbourne: Text Publishing. chapter 7. ISBN 9781921520648.

## External links

* Geology Project - Inland Sea Movement Through Time

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