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Abstract
Peesey Swamp on southern Yorke Peninsula, southern Australia, is a north-northwesterly south-southeasterly trending lowland depression, approximately 24 km long and 4 to 10 km wide. The richly fossiliferous mollusc and foraminiferal faunal assemblages of the last interglacial Glanville Formation in Peesey Swamp indicate that the paleoenvironment was a low- to medium-energy, sheltered sandflat to shallow-water seaway during the Last Interglacial Maximum (Marine Isotope Substage [MIS] 5e; 128–116 ka). The presence of the fossil bivalve molluscs Katelysia rhytiphora, Chlamys (Equichlamys) bifrons and Fulvia tenuicostata, in life position, indicate that the paleowater depth was ≤4 m in Peesey Swamp. The seaway cut across southern Yorke Peninsula, establishing a marine connection between southern Spencer Gulf and Investigator Strait during deposition of these taxa. Amino acid racemisation dating of the fossil marine molluscs Katelysia sp. and Fulvia tenuicostata confir ....

Kangaroo Island , Investigator Strait , South Australia , Yorke Peninsula , Western Australia , Fleurieu Peninsula , Spencer Gulf , Glanville Formation , Peesey Swamp , Last Interglacial Maximum , Marine Isotope Substage , Leeuwin Current , கங்காரு தீவு , புலனாய்வாளர் சங்கடமான , தெற்கு ஆஸ்திரேலியா , யார்க் தீபகற்பம் , மேற்கு ஆஸ்திரேலியா , ப்லேுரிஎஉ தீபகற்பம் , ஸ்பென்சர் வளைகுடா , கிளான்வில்லே உருவாக்கம் , லீவின் தற்போதைய ,