The empty tests of dead foraminifera behave as sedimentary particles and are subject to transport, although their diﬀerent shapes and eﬀectively low density means that their hydraulic equivalence is greater than that of spherical quartz grains (see Haake, 1962). Their estimated traction velocities range from c. 4 cm s-1 to c. 13 cm s-1 (Snyder et al., 1999). The presence of calcareous foraminiferal tests in a fossil sedimentary deposit would normally be taken as an indication of deposition in a marine environment. However, it has long been known that wind can transport...
Research Article| November 01, 2009
Wind transport of foraminiferal tests into subaerial dunes: an example from western Ireland
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JOHN W. MURRAY; Wind transport of foraminiferal tests into subaerial dunes: an example from western Ireland. Journal of Micropalaeontology ; 28 (2): 185–187. doi: https://doi.org/10.1144/jm.28.2.185
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