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SCAR BULLETIN, No. 151, October 2003

Antarctic Specially Protected Area No 143
Marine Plain, Mule Peninsula, Vestfold Hills, Princess Elizabeth Land

1. Description of Values to be Protected

Marine Plain is representative of a major Antarctic terrestrial ice-free ecosystem with outstanding fossil fauna and rare geological features. It is of exceptional ongoing scientific interest and has been subject to several detailed geological, palaeontological, geomorphological and glaciological studies.
The Area has yielded an outstanding vertebrate fossil fauna including Australodelphis mirus, the first higher vertebrate named from the Oligocene-Pleistocene interval on land in Antarctica, and the first cetacean fossil from the polar margin of circum-Antarctic Southern Ocean that postdates the break-up of Gondwana. Marine Plain has also revealed four other species of cetaceans; a species of fish; and a diverse invertebrate fauna comprising molluscs, gastropods, marine diatoms, and the first Pliocene decapod crustacean from Antarctica.
Marine Plain contains a roughly horizontal section of ca 8 m thick Pliocene marine sediments known as the Sørsdal Formation, which is exposed or underlies Holocene sediments, up to about 1 m thick. A diatom biostratigraphy placed the Sørsdal Formation in the Fragilariopsis barronii Zone, Early Pliocene (ca 4.5-4.1 Ma).
The Vestfold Hills have an ice-free area of approximately 413 km2, and are characterised by their low altitude, typically less that 180 m. The hills have been subject to intermittent glaciation and glacial striae show the direction of past ice movements.
Marine Plain provides the largest periglacial thermokarst in East Antarctica
The meromictic and saline Burton Lake, together with several smaller lakes and ponds in the ASPA, provide important examples in the spectrum of hypersaline to fresh water lake types in the Vestfold Hills and present the opportunity for important research.

2. Aims and Objectives

3. Management Activities

4. Period of Designation

Designated for an indefinite period.

5. Maps

Map A: Vestfold Hills, East Antarctica, showing the locations of Marine Plain ASPA;
Map B: The region immediately surrounding Marine Plain ASPA.
Map C: Geological map of Marine Plain ASPA.
Map D: Sørsdal Formation sketch map
Map E: Sketch of Surface Geology

6. Description of the Area

6(i). Geographical Co-Ordinates, Boundary Markers and Natural Features

Marine Plain ASPA (23.4 km2, 68°37’50.2" S, 78°07’55.2" E) opens into an arm of Crooked Fjord on the southern side of Mule Peninsula. The Vestfold Hills are a largely ice-free oasis of approximately 512 km2 of bedrock, glacial debris, lakes, and ponds, at the eastern side of Prydz Bay, Princess Elizabeth Land.
The three major lithologies forming the Vestfold Hills are (in order of age) Chelnock Paragneiss, Mossel Gneiss and Crooked Lake Gneiss. This is repeated in units from east-northeast to west-southwest. Intruded into these, are groups of mafic dykes in a rough north-south orientation (Map C). The dykes are a major feature of the Vestfold Hills.
The Precambrian rock is overlain in low-lying areas (approximately 10–17 m above sea level) by ca 8 m of early Pliocene (ca 4.5-3.5 Ma) diatomite with limestone lenses in the upper half. The limestone contains molluscs, especially bivalves including Chlamys tuftsensis Turner. Holocene (ca 6.49 ka) glacial debris disconformably covers the marine deposit (0.5-1 m), extending over an area of 8-10 km2. A layer of lenticular sandstone separates the Pliocene and Holocene units.
Burton Lake is a major feature of the western side of the Area. There is a number of unnamed ponds and small lakes within the Area. Burton Lake has a maximum depth of 18 m. Burton Lake, is ice-covered for 10–11 months of the year and is seasonally connected to Crooked Fjord by a tidal channel approximately 20 m wide and up to 2 m deep. The lake is isolated from Crooked Fjord for about 6-7 months of the year by ice.
The lake contains a range of photosynthetic bacteria, psychrophilic bacteria, one novel species of bacterium is Psychroserpens burtonensis, which has not been cultured from or recorded in any other environment, 41 diatom species, four metazoan species, many holotrichia, at least two species of nematode, a large marine amphipod and tardigrades. One species of fish, Pagothenia borchgrevinki, has been observed in the lake on one occasion.
Mosses and lichens occur in the vicinity of small ephemeral watercourses. The northern end of Burton Lake provides a rich lichen site, while the northern end of Poseidon Lake is rich in mosses.
Several vertebrates occur sporadically during the summer months. Wilson’s storm petrels (Oceanites oceanicus), Snow petrels (Pagodroma nivea) and South polar skuas (Catharacta maccormicki) nest in the Area. Weddell seals (Leptonychotes weddellii) and Southern Elephant seals (Mirounga leonina) along with Adélie penguins (Pygoscelis adeliae) and Emperor penguins (Aptenodytes forsteri) also occur in small groups.
The Vestfold Hills area has a polar maritime climate that is cold, dry and windy.

6(ii). Special Zones within the Area

None.

6(iii). Location of Structures Within and Adjacent to the Site

There are two refuges located nearby: Marine Plain Refuge with an adjacent helicopter landing site; and Watts Hut.
A variety of evidence of research activity remains at Marine Plain. Boundary markers are to be installed at boundary turning points.

6(iv). Location of Other Protected Areas in the Vicinity

Two Historic Sites and Monuments lay in the Vestfold Hills, at least 25 km north of Marine Plain: HSM No. 72 and HSM No. 6.

7. Permit Conditions

Entry into the Area is prohibited except in accordance with a Permit issued by an appropriate national authority.

7(i). Access to and Movement within or over the Area

7(ii). Activities which are, or may be conducted, within the Area, including restrictions on time and place

7(iii). Installation, modification or removal of structures

Any structures erected or installed within the Area are to be specified in a Permit. Permanent structures or installations are prohibited.

7(iv). Location of field camps

Parties should not camp in the Area but use the Marine Plain Refuge (68°36’54”S, 78°6’30”E).

7(v). Restrictions on materials and organisms which may be brought into the Area

7(vi). Taking of or harmful interference with native flora and fauna

The taking of or harmful interference with native flora or fauna is prohibited, except by Permit.

7(vii). Collection and removal of anything not brought into the Area by the Permit Holder

7(viii). Disposal of waste

All wastes, including all human wastes, shall be removed from the ASPA.

7(ix). Measures that may be necessary to ensure that the aims and objectives of the Plan of Management can continue to be met

7(x). Requirements for reports

Parties should ensure that the principal Permit Holder for each Permit issued submits to the appropriate national authority a report on activities undertaken.