Tagasi otsingusse
Bruck et al., 1985
Beaconites antarcticus in the (?Middle) Late Devonian McAras Brook Formation, Cape George, Nova Scotia
Bruck, P. M., Forbes, W. H., Nance, D., Pickerill, R. K.
DOI | 10.4138/1589 |
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Aasta | 1985 |
Ajakiri | Maritime Sediments and Atlantic Geology |
Köide | 21 |
Number | 1 |
Leheküljed | 87–96 |
Tüüp | artikkel ajakirjas |
Keel | inglise |
Id | 19512 |
Abstrakt
Beaconites antarcticus has recently been recorded in (?Middle-) Late Devonian fluvial siltstones of the McAras Brook Formation, Nova Scotia. Although previously noted in several North American Palaeozoic sequences the trace fossil has not, until now, been documented from Nova Scotia. Herein we note its occurrence and compare it to previously reported examples which occur in similar stratigraphical and environmental settings particularly from the British Isles and Antarctica.
Viimati muudetud: 26.9.2022