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GeoRef Categories
Era and Period
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Book Series
Date
Availability
EXCEPTIONALLY PRESERVED LATE ALBIAN (CRETACEOUS) ARCELLACEANS (THECAMOEBIANS) FROM THE DAKOTA FORMATION NEAR LINCOLN, NEBRASKA, USA Available to Purchase
A new sea-level curve from Nova Scotia: evidence for a rapid acceleration of sea-level rise in the late mid-Holocene Free
Foraminifera in Winyah Bay and North Inlet marshes, South Carolina; relationship to local pollution sources Available to Purchase
Morphological variations of benthic foraminiferal tests in response to changes in ecological parameters; a review Free
Holocene and latest Wisconsinan benthic foraminiferal assemblages and paleocirculation history, lower Scotian slope and rise Available to Purchase
Recent Arctic shelf foraminifera; seasonally ice covered vs. perennially ice covered areas Available to Purchase
Fragile abyssal foraminifera (including new Komokiacea) from the Nares abyssal plain Available to Purchase
Holocene sea levels, paleoceanography, and late glacial ice configuration near the Northumberland Strait, Maritime Provinces: Reply Free
Larger agglutinated foraminifera; comparison of assemblages from central North Pacific and western North Atlantic (Nares Abyssal Plain) Available to Purchase
Can smaller benthic foraminifera be ignored in paleoenvironmental analyses? Available to Purchase
A case study of protozoan intraclonal variability; taxonomic implications Available to Purchase
Empirical method for measuring seasonality in deep-sea cores Available to Purchase
Distribution of recent benthonic foraminifera near Sable Island, Nova Scotia Free
Arcellaceans ("thecamoebians") in small lakes of New Brunswick and Nova Scotia; modern distribution and Holocene stratigraphic changes Available to Purchase
Designation of types, for one genus and nine species of arcellaceans (thecamoebians), with additional original reference material for four other species Available to Purchase
Holocene rise of relative sea level at Sable Island, Nova Scotia, Canada Available to Purchase
HOLOCENE ARCELLACEA (THECAMOEBIANS) FROM EASTERN CANADA Available to Purchase
ABSTRACT A previous geological study of bottom and core samples of fossilized Holocene freshwater thecamoebians, involving the study of thousands of specimens belonging almost entirely to the superfamily Arcellacea, has prompted us to revise some of the rather confused taxonomy of several common genera. The Arcellacea present numerous cases of morphological test intergradation between main phenetic clusters. This has led specialists to propose classifications that recognize almost every rare morphotype as a distinct taxon (species or “variety”). We believe that such intergradation, which is at the basis of the confusion in these genera, is mainly due to the rarity of sexual events. We discuss the rationale and practical criteria for recognizing “species” among such uniparental or almost uniparental organisms. Apart from the problem of intergradation in fossil thecamoebians, taxonomic difficulties also arise from the absence of basic diagnostic characteristics (such as pseudopodia and others). We discuss how the importance of pseudopodial types in thecamoebian microclassification may have been exaggerated. More difficulties stem from the fact that in the past many arcellacean species and varieties have been defined according to the nature of their xenosomes (foreign agglutinated particles). While the shape of idiosomes (test particles secreted by the organism) may be a valid taxonomic characteristic, in most cases the nature of the xenosomes depends on the availability of inorganic particles and not on genome-based selectivity. The discussion of these problems leads us to define arcellacean species as wide phenetic clusters in which specimens are linked to each other through intergradation. In most cases the intergradational series were selected from large contiguous populations. We have organized accordingly the taxonomy of fourteen species (some of which can themselves be linked to each other by scarcer intermediate specimens) instead of the several dozens of species in which the same organisms were divided by earlier authors. The fourteen species (in five genera) are: Difflugia protaeiformis Lamarck, D. bacillariarum Perty, D. bidens Pénard, D. corona Wallich, D. fragosa Hempel, D. globulus (Ehrenberg), D. oblonga Ehrenberg, D. urceolata Carter, D. tricuspis Carter, Lagenodifflugia vas (Leidy), Pontigulasia compressa (Carter), Heleopera sphagni (Leidy), Centropyxis aculeata (Ehrenberg), and C. constricta (Ehrenberg). These species are redescribed, discussed, and their fossilized forms illustrated. The literature indicates that these species are cosmopolitan and usually form a large percentage of the lacustrine faunae everywhere. Hence the taxonomy presented here is potentially applicable universally.