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Pulicat Lake : ウィキペディア英語版 | Pulicat Lake
Pulicat Lake (Tamil: ''Pazhaverkaadu Eri'', Telugu: ''Pulicat Sarassu'') is the second largest brackish – water lake or lagoon in India, after Chilika Lake. It straddles the border of Andhra Pradesh and Tamil Nadu states on the Coromandal Coast in South India. The lake encompasses the Pulicat Lake Bird Sanctuary. The barrier island of Sriharikota separates the lake from the Bay of Bengal and is home to the Satish Dhawan Space Centre.〔 ==History== (詳細はPeriplus of the Erythraean Sea listed Podouke (Pulicat) as one of the three ports on the east coast of India. In the 2nd century, Ptolomey's list of ports on this coast included Podouke emporion. In the 13th century, Arabs migrated to the shores of the lake after they were banished from Mecca for refusing to pay tributes to a new calif. Streets with dilapidated masonry houses once occupied by these Arabian Muslims are still found in the area and resident families claim records in Arabic testifying the migration. Portuguese colonized the lake in 16th century followed by the Dutch. The Dutch drifted to the lagoon as their ships got stuck on the shores of Karimanal village on the opposite side of the mouth of the lake. During the Dutch occupation, Pulicat was known by the name ''Pallaicatta''. Fort Geldria dating to 1609, a church, a cemetery with tombs and mausoleums constructed by the Dutch are protected by the Archaeological Survey of India (ASI). The Dutch transacted business with the British East India Company and other countries in the region.〔〔 A scientific study of the palynological characteristics of the lagoon was conducted by taking sedimentary soil samples from four test pits. It shows that the vegetational reconstruction from peat beds at a.m.s.l. and (a.m.s.l.) in the west at Sullurpeta and Kasdredinilem, respectively, is indicative of a palaeoshorelin. The sea level reached its maximum around 6650 plus or minus 110 yrs BP in Sullurpeta, west from the present shoreline. The radiocarbon dates of peat bed at Kasdreddinilem reveals an age of 4608 plus or minus 122 yrs BP, indicating the shift in mangrove line eastwards during the regressive phase.〔
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