To link to full-text access for this article, visit this link: http://dx.doi.org/10.1016/j.dsr.2010.07.010 Byline: Andrea Burke (a), Laura F. Robinson (b), Ann P. McNichol (c), William J. Jenkins (b), Kathryn M. Scanlon (d), Dana S. Gerlach (c) Keywords: Deep-sea corals; Age survey; Radiocarbon dating; Biogeography Abstract: We have developed a rapid 'reconnaissance' method of preparing graphite for.sup.14C/.sup.12C analysis. Carbonate ([approximately equal to]15mg) is combusted using an elemental analyzer and the resulting CO.sub.2 is converted to graphite using a sealed tube zinc reduction method. Over 85% (n=45 replicates on twenty-one individual corals) of reconnaissance ages measured on corals ranging in age from 500 to 33,000 radiocarbon years (Ryr) are within two standard deviations of ages generated using standard hydrolysis methods on the same corals, and all reconnaissance ages are within 300Ryr of the standard hydrolysis ages. Replicate measurements on three individual aragonitic corals yielded ages of 1076[+ or -]35Ryr (standard deviation; n=5), 10,739[+ or -]47Ryr (n=8), and 40,146[+ or -]3500Ryr (n=9). No systematic biases were found using different cleaning methods or variable sample sizes. Analysis of.sup.13C/.sup.12C was made concurrently with the.sup.14C/.sup.12C measurement to correct for natural fractionation and for fractionation during sample processing and analysis. This technique provides a new, rapid method for making accurate, percent-level.sup.14C/.sup.12C analyses that may be used to establish the rates and chronology of earth system processes where survey-type modes of age estimation are desirable. For example, applications may include creation of sediment core-top maps, preliminary age models for sediment cores, and growth rate studies of marine organisms such as corals or mollusks. We applied the reconnaissance method to more than 100 solitary deep-sea corals collected in the Drake Passage in the Southern Ocean to investigate their temporal and spatial distribution. The corals used in this study are part of a larger sample set, and the subset that was dated was chosen based on species as opposed to preservation state, so as to exclude obvious temporal biases. Similar to studies in other regions, the distribution of deep-sea corals is not constant through time across the Drake Passage. Most of the corals from the Burdwood Bank (continental shelf of Argentina) have ages ranging between 0 and 2500 calendar years, whereas most of the corals from the Sars Seamount in the Drake Passage have ages between 10,000 and 12,500 calendar years. Such differences may be caused in part by sampling biases, but may also be caused by changes in larval transport, nutrient supply, or other environmental pressures. Author Affiliation: (a) MIT/WHOI Joint Program, Department of Marine Geology and Geophysics, Woods Hole Oceanographic Institution, 360 Woods Hole Road, MS#24, Woods Hole, MA 02543, USA (b) Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, 360 Woods Hole Road, MS#25, Woods Hole, MA 02543, USA (c) Department of Marine Geology and Geophysics, Woods Hole Oceanographic Institution, 360 Woods Hole Road, MS#8, Woods Hole, MA 02543, USA (d) US Geological Survey, 384 Woods Hole Road, Woods Hole, MA 02543, USA Article History: Received 9 February 2010; Revised 15 July 2010; Accepted 21 July 2010 Article Note: (footnote) [star] Reference to any specific commercial product by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof.