Last Ice Age millennial scale climate changes recorded in Huon Peninsula corals.

• Main Authors: Yokoyama, Yusuke, Esat, Tezer M, Lambeck, Kurt, Fifield, L Keith
• Format: Article in Journal/Newspaper
• Language: English
• Published: Radiocarbon 2000
• Subjects: Huon Peninsula;Papua;Heinrich events;Dansgaard Oeschger cycles;Papua New Guinea;terraces;reefs;sea level changes;Th U;climate change;Atlantic Ocean;North Atlantic;calibration;atmosphere;Australasia;last glacial maximum;Pleistocene;upper Pleistocene;Cenozoic;Quaternary;C 14;carbon;isotopes;radioactive isotopes;absolute age; Huon; North Atlantic; North atlantic Thermohaline circulation
• Online Access: https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/3830

Uranium series and radiocarbon ages were measured in corals from the uplifted coral terraces of Huon Peninsula (HP), Papua New Guinea, to provide a calibration for the (super 14) C time scale beyond 30 ka (kilo annum). Improved analytical procedures, and quantitative criteria for sample selection, helped discriminate diagenetically altered samples. The base-line of the calibration curve follows the trend of increasing divergence from calendar ages, as established by previous studies. Superimposed on this trend, four well-defined peaks of excess atmospheric radiocarbon were found ranging in magnitude from 100% to 700%, relative to current levels. They are related to episodes of sea-level rise and reef growth at HP. These peaks appear to be synchronous with Heinrich Events and concentrations of ice-rafted debris found in North Atlantic deep-sea cores. Relative timing of sea-level rise and atmospheric (super 14) C excess imply the following sequence of events: An initial sea-level high is followed by a large increase in atmospheric (super 14) C as the sea-level subsides. Over about 1800 years, the atmospheric radiocarbon drops to below present ambient levels. This cycle bears a close resemblance to ice-calving episodes of Dansgaard-Oeschger and Bond cycles and the slow-down or complete interruption of the North Atlantic thermohaline circulation. The increases in the atmospheric (super 14) C levels are attributed to the cessation of the North Atlantic circulation.