FINICKY FORAMS: HETEROGENEITIES IN RECRUITMENT ON EXPERIMENTAL SUBSTRATES, ROSS SEA, ANTARCTICA
Here, we show that recruitment of benthic forams differ between experimental arrays composed of two treatments: inorganic calcite (in mesh bags of 0.1mm2 opening) and natural calcite from the Antarctic scallop, Adamussium colbecki (in mesh bags of 1.0 mm2 opening). The arrays were deployed at 9 m (30 ft) by ice divers at the Herbertson Glacier site of McMurdo Sound, Ross Sea, Antarctica. After two years on the seafloor, the arrays were retrieved, and for each mesh bag and substrate, the forams were identified and counted. If foraminiferal propagules were not selective of substrate type, we would expect that similar recruitment would occur on both treatment, but we found that recruitment was significantly higher on natural substrates than unnatural substrates (t-test, P < 0.01). Additionally, variance in recruitment was significantly higher on A. colbecki substrates and mesh bags than those of inorganic calcite (F-test, P < 0.01), indicating patchiness in recruitment. Our findings suggest that foraminiferal propagules are significantly more likely to recruit to natural substrates than to inorganic substrates. Therefore, utilizing natural substrates in taphonomic and paleoecologic studies may provide more accurate data to understand recruitment, community structure and dispersal capabilities of encrusting forams.