Wenlock Palaeoscenidiidae and Entactiniidae (Radiolaria) from the Cape Phillips Formation of the Canadian Arctic Archipelago

1986 ◽  
Vol 32 (2) ◽  
pp. 129 ◽  
Author(s):  
Q. H. Goodbody
Keyword(s):  
Canadian Arctic ◽  
Canadian Arctic Archipelago ◽  
Cape Phillips Formation

scholarly journals Silurian ostracoderms from Washington Land (North Greenland), with comments on cyathaspid structure, systematics and phyletic position

1986 ◽  
Vol 132 ◽  
pp. 89-123
Author(s):  
S.E Bendix-Almgreen
Keyword(s):  
Canadian Arctic ◽  
Stability Control ◽  
Canadian Arctic Archipelago ◽  
Marine Deposits ◽  
Type Section ◽  
Cape Phillips Formation ◽  
North Greenland

The few detached dermal elements recorded here document a new ostracoderm fauna comprising undeterminable species of one anaspid, two cyathaspids and a heterostracan which might have its closest relatives among the pteraspids. This fauna is derived from marine deposits of ultimate Wenlock or possibly Early Ludlow age at the top of the Lafayette Bugt Formation in its type section, in Washington Land, western North Greenland. It is probably equivalent to one of the undescribed faunas known from the Monograptus testis - M. nilssoni sequence of the Cape Phillips Formation in the Canadian Arctic Archipelago. Comparative material from Norway and Spitsbergen is considered in this study which prompted general comments on cyathaspid squamation, vestigial fin structure, cyathaspid systematics, their phyletic position relative to the pteraspids, system of stability control in swimming, their habitats and diets.

A new Silurian Astylospongid sponge from Baillie-Hamilton Island, Canadian Arctic Archipelago

1978 ◽  
Vol 15 (1) ◽  
pp. 157-162 ◽  
Author(s):  
J. Keith Rigby ◽  
Alfred C. Lenz
Keyword(s):  
Canadian Arctic ◽  
Canadian Arctic Archipelago ◽  
Arctic Canada ◽  
Uniform Size ◽  
Cape Phillips Formation

The new sponge, Astylospongiella megale, is described from rocks of the Ludlovian Neodiversograptus nilssoni Zone of the Cape Phillips Formation from southern Baillie-Hamilton Island, Arctic Canada. The genus is included in Astylospongiidae because its skeletal net is composed of sphaeroclones, which in this species, are of relatively uniform size throughout the sponge. The new sponge also has irregularly placed radiating canals which are subparallel to the upper surface, and which are cross-connected by upward fanning canals that are approximately normal to the sponge surface and the radiating canals.

Morphology and classification of some Early Silurian monograptids (Graptoloidea) from the Cape Phillips Formation, Canadian Arctic Islands

1997 ◽  
Vol 34 (8) ◽  
pp. 1128-1149 ◽  
Author(s):  
Jeff J. Lukasik ◽  
Michael J. Melchin
Keyword(s):  
Canadian Arctic ◽  
Canadian Arctic Archipelago ◽  
Dorsal Wall ◽  
Wall Structures ◽  
Morphological Criteria ◽  
Cape Phillips Formation ◽  
Upward Growth ◽  
Definition Of ◽  
Simultaneous Evolution

Exquisitely preserved early to mid-Llandovery monograptids have been chemically isolated from calcareous concretions sampled from the Cape Phillips Formation, central Canadian Arctic Archipelago. They provide morphological information critical in refining the definition of four of the earliest known monograptid genera, and in the elucidation of their phylogenetic dispersal through the Llandovery monograptid radiation. These primitive monograptid genera are defined primarily on the basis of derived thecal form. The specific, derived thecal and thecal apertural character states used in generic diagnoses are as follows: species of Atavograptus possess simple, geniculate to slightly sigmoidal thecae with a large dorsoventral overlap; species of Pribylograptus possess thecae bearing lateral apertural lappets that may occur with Atavograptus-style thecae proximally; species of Coronograptus possess flared thecal apertures at least part way along the rhabdosome; species of Lagarograptus have conspicuous, tongue-like, ventral apertural processes developed as ventral apertural margin outgrowths. Species of all of these genera may possess hoods that are genicular in origin, with the exception of those of Lagarograptus inexpeditus, which are dorsal wall structures. These earliest monograptid genera possess a pattern Mr astogeny, characterized by the outward, then upward growth of theca 1 from a sicular resorption porus (pattern Mr, different from younger monograptids that possess a primary porus developed during sicular astogeny (pattern Mp)). Through analysis of their defining morphological criteria in conjunction with sicular dimensions and thecal uniformity, each of these early monograptid genera is considered to be monophyletic, arising from the primitive Atavograptus stock. Atavograptus thecal morphology provided a simple template for the derivation of thecal form leading to the nearly simultaneous evolution of Pribylograptus, Coronograptus, and Lagarograptus in the lower Rhuddanian. Fourteen species belonging to four genera are described, including six new species.

Silurian (Wenlockian) trilobites from Baillie-Hamilton Island, Canadian Arctic Archipelago

1977 ◽  
Vol 14 (2) ◽  
pp. 285-317 ◽  
Author(s):  
D. G. Perry ◽  
B. D. E. Chatterton
Keyword(s):  
New Species ◽  
Northwest Territories ◽  
New Taxa ◽  
Canadian Arctic ◽  
Canadian Arctic Archipelago ◽  
Cape Phillips Formation ◽  
Mackenzie Mountains

Wenlockian trilobites representing at least 15 genera are reported from carbonate strata within the Cape Phillips Formation, Baillie-Hamilton Island. The collections are stratigraphically bounded by the graptolite Zones of Cyrtograptus murchisoni and Monograptus testis. The fauna is generically dominated by lichids, odontopleurids, and cheirurids. Scutelluids, phacopids, dalmanitids, and harpids are notable for their absence. At the familial level the fauna corresponds to one recently discovered from similar age beds of the Mackenzie Mountains, Northwest Territories. The limited quantity and fragmental nature of much of the silicified fauna precludes erection of many new taxa, although four new species described are: Sphaerexochus dimorphus, Dicranogmus skinneri, Hemiarges rohri, and Hemiarges mikulici. Dimorphic pygidia are interpreted as probable sexual dimorphs in Sphaerexochus dimorphus n. sp.

Llandovery graptolite biostratigraphy and paleobiogeography, Cape Phillips Formation, Canadian Arctic Islands

1989 ◽  
Vol 26 (9) ◽  
pp. 1726-1746 ◽  
Author(s):  
Michael J. Melchin
Keyword(s):  
North America ◽  
Canadian Arctic ◽  
The Arctic ◽  
Canadian Cordillera ◽  
Canadian Arctic Archipelago ◽  
The South ◽  
Cape Phillips Formation ◽  
Shallow Basin

Llandovery graptolites have been collected from 11 sections in the Cape Phillips Formation of the Canadian Arctic Archipelago: Melville, Bathurst, Truro, Cornwallis, Devon, and Ellesmere islands. The Cape Phillips Formation appears to have been deposited in a distinct subbasin, here termed the Cape Phillips Basin, under deep-shelf to shallow-basin conditions intermediate in position between the Arctic Platform to the south and east and the deeper Hazen Trough to the northwest.A total of 170 graptolite species and a further 25 subspecies have been identified. Their stratigraphic distribution allows the recognition of 11 graptolite zones: the acuminatus, atavus, acinaces, cyphus, curtus, convolutus, minor, turriculatus, crispus, griestoniensis, and sakmaricus zones. The curtus Zone can be subdivided into the pectinatus and orbitus subzones. The zones can be correlated with graptolite sequences worldwide.The Canadian Arctic faunas show strong affinities with those of Siberia, China, and the northern Canadian Cordillera. It may be possible to recognize a circum-equatorial faunal province in northern North America, Siberia, and China based on the occurrence of distinctive forms including Agetograptus and "Paramonoclimacis" in the middle Llandovery and certain Cyrtograptus species (especially C. sakmaricus) in the upper Llandovery.

Wenlock (Silurian) graptolites, Cape Phillips Formation, Canadian Arctic Islands

1991 ◽  
Vol 82 (3) ◽  
pp. 211-237 ◽  
Author(s):  
A. C. Lenz ◽  
M. J. Melchin
Keyword(s):  
New Species ◽  
Canadian Arctic ◽  
Canadian Arctic Archipelago ◽  
Important Species ◽  
Cape Phillips Formation ◽  
Total Fauna

Twenty six of the more important species of monograptids (s.l.), retiolitids and Cyrtograptus (from a total fauna of 52 species) are described from Wenlock strata of the Cape Phillips Formation, Canadian Arctic Archipelago. Of this fauna, eight new species or subspecies, Monograptus firmus festinolatus, M. instrenuus, M. opimus, M. testis incomptus, Cyrtograptus falcatus, C. hamatus brevis, C. kolobus and C. pseudomancki, are described and illustrated.Wenlock biostratigraphic zones comprise the Cyrtograptus centrifugus-C. insectus Zone (earliest Wenlock), M. instrenuus-C. kolobus Zone, tentatively divisible into lower and upper subzones, C. perneri-M. opimus Zone possibly divisible into lower and upper subzones, C. lundgreni-M. testis Zone divisible into a lower M. testis incomptus Subzone and an upper M. testis testis Subzone, and the Pristiograptus ludensis Zone (latest Wenlock).

Silurian (Wenlock) calymenid trilobites from the Cape Phillips Formation, Central Canadian Arctic

1997 ◽  
Vol 71 (4) ◽  
pp. 657-682 ◽  
Author(s):  
Jonathan M. Adrain ◽  
Gregory D. Edgecombe
Keyword(s):  
New Species ◽  
New Taxa ◽  
Type Species ◽  
New Genus ◽  
Canadian Arctic ◽  
Canadian Arctic Archipelago ◽  
Cape Phillips Formation ◽  
Common Components

Calymenid trilobites are common components of diverse Silurian silicified faunas recovered from the Cape Phillips Formation of the Cape Phillips Basin, central Canadian Arctic Archipelago. Calymenids are represented in the Wenlock of the northern Laurentian region by only two genera, Diacalymene Kegel, 1927, and Arcticalymene new genus (type species A. viciousi new species). Calymenid diversity in any given fauna is never higher than two species, although these species may be numerically abundant. Arcticalymene became extinct during the Homerian, at which point calymenids disappeared forever from the northern Laurentian record.Other new taxa are Arcticalymene cooki new species, A. jonesi new species, A. matlocki new species, and A. rotteni new species. Material representing at least two more species of the new genus is reported in open nomenclature. Diacalymene gabrielsi Siveter and Chatterton, 1996, is recorded from the Cape Phillips Basin.

Ludlow (Silurian) lithistid and hexactinellid sponges, Cape Phillips Formation, Canadian Arctic

1991 ◽  
Vol 28 (12) ◽  
pp. 2042-2061 ◽  
Author(s):  
Tim A. de Freitas
Keyword(s):  
Canadian Arctic ◽  
Evolutionary Trends ◽  
The Family ◽  
Cape Phillips Formation ◽  
Canal Systems ◽  
Structural Simplicity ◽  
Lithistid Sponge ◽  
Hexactinellid Sponges

Abundant hexactinellid and lithistid sponges occur in Ludlow (Silurian) platform slope strata of the Cape Phillips Formation, Canadian Arctic Islands. The following are new: in the Anthaspidellidae Miller, 1889, rhodesispongia simplex n.gen and sp., Climacospongia snowblindella n.sp., and Climacospongia undulata n.sp.; in the Sphaerocladina Schrammen, 1910, Caryospongia tuberosa n.sp.; in the Hexactinellida Schmidt, 1870 Malumispongium? cornwallisi n.sp., of the monospecific superfamily Malumispongium Rigby, 1967. Other previously described sponges recognized in the study assemblage include Hindia sphaeroidalis Duncan, 1879 and Caryospongia juglans Rauff, 1894. These occur in association with abundant Archaeoscyphia sp. in thin, laterally extensive lithistid sponge biostromes which throve on platform slope sediments during the Late Silurian. Based on the dominant dendroclone forms in the skeletons of these and other genera, Anthaspidellidae can be divided informally into two groups: (i) the polyclonids, possessing complex skeletons built of variable dendroclones types, including I-, X-, and Y-shape dendroclones, and accessory spicules, including rhizoclones, chiastoclones, and monactines; and (ii) the monoclonids, possessing simpler parenchymal canal systems and skeletons constructed mainly of I-shaped (amphiarborescent) dendroclones and lacking accessory spicules. The classification, based chiefly on skeletal architecture, suggests two main evolutionary trends in the family. The monoclonids generally maintained structural simplicity, inherited from the probable ancestral monactinellid, whereas the polyclonids evolved a varied and complex skeletal architecture that was more successful.

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