272 D17. Paleontology, Paleoecology/Taphonomy (Posters)
Tuesday, 24 October 2017
9:00 AM - 6:30 PM
Halls 4EF
RELATIVELY FAST GROWTH AND MODERATE LONGEVITY FOR THE ANTARCTIC SCALLOP, ADAMUSSIUM COLBECKI, LIVING IN THE COLDEST WATERS ON EARTH
Paper number: 272-41
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Sally WalkerUniversity of Georgia, Athens, GA
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Roger MannCollege of William and Mary, Gloucester Point, VA
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A.S. ChuteNational Oceanic and Atmospheric Association, Woods Hole, MA
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Mathew LongCollege of William and Mary, Gloucester Point, VA
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Samuel S. BowserNew York State Department of Health, Albany, NY
Abstract
We estimated growth and lifespan for A. colbecki from two sites that differ by sea ice cover in western McMurdo Sound, Antarctica: Explorers Cove (EC) and Bay of Sails (BOS). EC has multi-annual sea ice, which may affect nutrient availability, and sea ice melts out yearly at BOS. Both have similar austral summer temperatures (-1.97 oC). We predict that EC scallops would have longer lifespans and slower growth than BOS scallops, but if temperature affects growth then BOS and EC should be similar. Adult A. colbecki (72 – 92 mm) were collected at ~ 18 m water depth, 14 top and bottom valves of which were randomly selected from each site. Using a scallop fisheries method, distinct yearly annuli were counted for longevity estimates. Growth increments from umbo to each successive annulus were measured and used in Ford Walford plots, the slope from which yields K values for each valve that were also pooled by site and valve type. Data were compared using ANOVA and 95% CIs.
Results indicate that A. colbecki lives at least two decades at EC and BOS (13–19 yrs) and is not a century old as previously reported for EC. It also grows relatively fast for a polar bivalve (pooled Ks: 0.15–0.20) unlike previous reports from EC (Ks = 0.09–0.12); there is also much individual variation (K range: 0.11–0.23). Our estimates align with A. colbecki living in seasonally warmer Antarctic regions (Terra Nova Bay: 0.11 > K > 0.19; Antarctic Peninsula K = 0.24). Importantly, age and K estimates were not statistically different by site or valve type suggesting that persistent sea ice may not affect their growth.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-306175
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