1957
DOI: 10.4095/101505
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The arthropod fauna of the Upper Carboniferous rocks of the Maritime Provinces

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Cited by 49 publications
(54 citation statements)
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“…The largest specimens from the Speiser Shale are smaller than Bless & Pollard's (1973) (Bless & Pollard, 1973); Visean and Namurian of Scotland; Westphalian A-D, Britain (Pollard, 1966;Anderson, 1970); Limburg (Bless, 1967); Westphalian A and B, Nova Scotia (Copeland, 1957); and France (Pruvost, 1911). Remarks.…”
Section: Systematic Palaeontologymentioning
confidence: 99%
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“…The largest specimens from the Speiser Shale are smaller than Bless & Pollard's (1973) (Bless & Pollard, 1973); Visean and Namurian of Scotland; Westphalian A-D, Britain (Pollard, 1966;Anderson, 1970); Limburg (Bless, 1967); Westphalian A and B, Nova Scotia (Copeland, 1957); and France (Pruvost, 1911). Remarks.…”
Section: Systematic Palaeontologymentioning
confidence: 99%
“…Anderson (1970, p. 74) (Bless & Pollard, 1973); Westphalian C, Britain (Bless & Pollard, 1973;Anderson, 1970); Westphalian D, Britain (Anderson, 1970); Westphalian A, Nova Scotia (Copeland, 1957); and Pennsylvanian of eastern USA (Scott & Summerson, 1943).…”
Section: Systematic Palaeontologymentioning
confidence: 99%
“…The eocarid Pseudotealliocaris (Fig. 6c) and Anthracophausia fauna of the lower Mabou Group (Copeland 1957) have been interpreted elsewhere to be representatives of a nearshore marine community (Schram 1981). Within the lower Mabou occur also the ostracods Shernonaella (Paraparchites) scotoburdigalensis and Beyrichiopsis sp., which are indicative of a nearshore environment and which are found also in the Dinantian of Scotland (Copeland 1957;.…”
Section: Namurianmentioning
confidence: 99%
“…6c) and Anthracophausia fauna of the lower Mabou Group (Copeland 1957) have been interpreted elsewhere to be representatives of a nearshore marine community (Schram 1981). Within the lower Mabou occur also the ostracods Shernonaella (Paraparchites) scotoburdigalensis and Beyrichiopsis sp., which are indicative of a nearshore environment and which are found also in the Dinantian of Scotland (Copeland 1957;. It is possible, therefore, that maximum transgressions from the retreating Windsor Sea continued for some time to influence the basinal waters of the Maritimes during deposition of the succeeding strata, the Mabou Group.…”
Section: Namurianmentioning
confidence: 99%
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