Data from a 3 m sediment core collected west of Pidgeon Island in the Windmill Islands, Antarctica

• 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), CUNNINGHAM, LAURA KAY (collaborator), CUNNINGHAM, LAURA KAY (hasPrincipalInvestigator), CUNNINGHAM, LAURA KAY (author), MCMINN, ANDREW (hasPrincipalInvestigator), RIDDLE, MARTIN J. (hasPrincipalInvestigator), Riddle, M.J., McMinn, A. and Cunningham, L.K. (originator)
• Format: Dataset
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: biota; oceans; EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PROTISTS > DIATOMS; PLANTS > MICROALGAE > BIOSPHERE > ECOSYSTEMS > MARINE ECOSYSTEMS > BENTHIC; COASTAL; ECOLOGICAL DYNAMICS > COMMUNITY DYNAMICS > COMMUNITY STRUCTURE; AGE; BENTHIC %; BENTHIC INDEX; CORRECTED AGE; DEPTH; MARINE; PLANKTONIC %; RADIOCARBON AGE; SEDIMENTS; SITE; SPECIES; TEMPORAL; SEDIMENT CORERS; FIELD SURVEYS; AMD/AU; CEOS; AMD; CONTINENT > ANTARCTICA > Windmill Islands; GEOGRAPHIC REGION > POLAR; Antarc*; Antarctica; Pidgeon Island
• Online Access: https://researchdata.edu.au/data-3-m-islands-antarctica/2821572

Progress Code: completed Statement: Dates given in temporal coverage are approximate only. The year is accurate. A sediment core was collected from the western side of Pidgeon Island, (66.3216 S, 110.445 E) at a water depth of 82.0 m. This sediment core (PG 1411-2) was recovered using a release-controlled piston corer, with a length of 3 m, using the coring technique described in Melles et al., (1994). The total core length was 240 cm. This core was stored in the dark, at 0 degrees C until required. Samples were taken for diatom analyses and radiocarbon (14C) dating. Prior to sub-sampling the core was split in half, along its length. One half was used for sampling, the other kept intact and stored at IASOS (University of Tasmania). To reduce potential contamination, resulting from the disturbance of sediments during the core-splitting procedure, a thin layer of sediment was removed from the exposed surface immediately prior to sampling. In order to obtain samples for diatom analysis, a toothpick was inserted into the core segment, and used to gouge a small amount of sediment from the middle of the core. Samples for diatom analyses were initially collected every 5 mm, however, sampling frequency progressively decreased down the core. Samples for radiocarbon data consisted of at least 1 cm 3 of sediment, collected from the middle of the core. These samples were collected from between 0-1 cm, 12-13 cm, 59-60 cm, 77-78 cm, 117-118 cm, and 229-230 cm depth. Diatom data are presented as raw counts, benthic abundances, the ratio of benthic to plankton species, and as the benthic index. Calculated ages (in years) are also given for all samples. The sedimentological core log is given as a powerpoint presentation. This work was completed as part of ASAC project 1130 (ASAC_1130) and project 2201 (ASAC_2201). Public summary from project 1130: Algal mats grow on sea floor in most shallow marine environments. They are thought to contribute more than half of the total primary production in many of these areas, making them ...