Late Holocene precipitation record from Windmill Island lakes

• Other Authors: AADC (owner), AADC, DATA OFFICER (distributor), AADC, DATA OFFICER (custodian), AU/AADC > Australian Antarctic Data Centre, Australia (hasAssociationWith), Australian Antarctic Data Centre (publisher), Australian Antarctic Division (sponsor), MCMINN, ANDREW (collaborator), MCMINN, ANDREW (hasPrincipalInvestigator), MCMINN, ANDREW (author), McMinn, A. (originator)
• Format: Dataset
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: climatologyMeteorologyAtmosphere; geoscientificInformation; oceans; EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS; BIOLOGICAL CLASSIFICATION > PROTISTS > DIATOMS; PLANTS > MICROALGAE > CATCHMENT; CODE; ELEVATION; FLORA; ICE DEPTH; LAKE; LAKE AREA; LAKE DEPTH; LATITUDE; LOCATION; LONGITUDE; NITRATE; NITRITE; PH; PHOSPHATE; SALINITY; SILICON; SPECIES; WATER SAMPLE; AMD/AU; CEOS; AMD; CONTINENT > ANTARCTICA > Windmill Islands; GEOGRAPHIC REGION > POLAR; Antarc*; Antarctic; Antarctica; Beall Island; Holl Island; ice core
• Online Access: https://researchdata.edu.au/late-holocene-precipitation-island-lakes/2816754

Progress Code: completed Statement: All data were collected with confidence. Antarctic lake cores record a history of precipitation in the preservation of climate sensitive microbial communities. Comprehensive integration of our precipitation records with other climate proxies such as ice core temperature records and historical climate data are dependent upon accurate dating of this lake sediment. Fourteen lakes and ponds of the Windmill Islands were sampled in 1998 for diatoms and in 1999 for water chemistry. The waterbodies included in this study fall into one of 3 broad categories: saline lake (greater than 5m deep; greater than, or equal to, 3 parts per thousand - salinity), saline pond (less than 5m deep; greater than, or equal to, 3 parts per thousand - salinity) or freshwater pond (less than 5m deep; less than 3 parts per thousand - salinity). Saline Lakes Beall Lake, the largest lake on Beall Island, is situated in a rocky catchment with evidence of breeding penguin pairs nearby. Outflow into the small lake on the northwestern point of Beall Lake occurs at elevated lake levels. Holl Lake, the largest lake on Holl Island, is contained by ridges to the NE and SW with an obvious outflow to the SE. At the time of sampling (20 Dec 1998), penguin feathers were observed in the sediment. In 2001 large numbers of penguins were observed behind the NE ridge in addition to the numerous skuas nesting on most nearby peaks. Lake A is the westernmost lake on Browning Peninsula. This large closed saline lake has a very thick ice cover (~2.5 m) and very little evidence of birdlife. Lake M is the easternmost lake sampled on Browning Peninsula. This large closed saline lake had a very thick ice cover (3.0 m) at the time of sampling. Saline Ponds Lake Warrington is the largest waterbody on Warrington Island. Found in the centre of Warrington Island, this small shallow (1.9 m) saline pond was almost completely frozen (ice cover of 1.6 m), with ca. 0.3 m of water below the ice at the time of sampling. The lake catchment is ...