期刊
SEDIMENTARY GEOLOGY
卷 147, 期 3-4, 页码 437-443出版社
ELSEVIER SCIENCE BV
DOI: 10.1016/S0037-0738(01)00099-9
关键词
Bahamas; Bermuda; Sangamonian; aeolian dunes; nearshore sedimentation; global change
类别
We respond to Hearty et al.'s objections to Our interpretation of upper Pleistocene coastal landforms from Bermuda and the Bahamas as aeolian duties rather than, wave-induced deposits. Their remarks concern the origin of fine-scale laminae and fenestral pores observed in these landforms, the apparent lack of steeply dipping foresets, the inference that carbonate coastal dunes can migrate, the vicinity of wave-deposited boulders that we did not mention, and finally, the palaeoclimatic reconstruction we derived from our interpretation. Although, we do not exclude-and never did-that occasional storm-generated,waves washed up and over these dunes and created some scours, we maintain that these controversial deposits have an aeolian origin. (C) 2002 Elsevier Science B.V. All rights reserved.
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