A NEW GENUS AND SPECIES OF HEPTAGENIIDAE (EPHEMEROPTERA) FROM WESTERN CANADA

1979 ◽  
Vol 111 (7) ◽  
pp. 859-862 ◽  
Author(s):  
D.M. Lehmkuhl

AbstractA new genus and species of Heptageniidae (Ephemeroptera) is based on a series of nymphs and reared female adults from the Saskatchewan River, Saskatchewan. Descriptions of female and nymphal Macdunnoa nipawinia n. gen., n. sp., of the subfamily Heptageniinae, are given along with notes on the biology. The genus has no close North American relatives, but is allied to heptageniid genera from southeast Asia.

2013 ◽  
Vol 50 (3) ◽  
pp. 355-378 ◽  
Author(s):  
Craig S. Scott ◽  
Daniel N. Spivak ◽  
Arthur R. Sweet

Although mammals of Paleocene age are well known from Alberta, their record is largely restricted to one lithological unit, the Paskapoo Formation (a record that includes mammals from the Cochrane area erroneously attributed to the Porcupine Hills Formation). We report here the first occurrence of Paleocene mammals from the Porcupine Hills Formation at exposures near the western edge of the city of Calgary. The assemblage, termed the Bearspaw local fauna, documents a diversity of multituberculate and eutherian mammals, including new species of the pentacodontid Aphronorus bearspawensis sp. nov., the mixodectid Eudaemonema bohachae sp. nov., the hyopsodontid Promioclaenus thnetus sp. nov., and a new genus and species of multituberculate (Alopocosmodon hadrus gen. et sp. nov.) tentatively referred to the Microcosmodontidae. The Bearspaw local fauna also details the first Canadian occurrences of several taxa, including Ptilodus wyomingensis, Aphronorus fraudator, Bryanictis microlestes, Elpidophorus minor, and possibly Goniacodon. Preliminary biostratigraphic analyses suggest that the Bearspaw local fauna is middle Torrejonian (To2) in age, correlating most closely with near-coeval Gidley Quarry of Montana and Rock Bench Quarry of Wyoming. In addition to improving the depauperate record of Torrejonian mammals in western Canada, the new fauna is important in documenting a mammal assemblage from a lithological unit that is thought to have been deposited in semi-arid conditions, rather than the wetter and more humid conditions of the Paskapoo Formation. Further, the Bearspaw localities, along with several other recently discovered localities in the Calgary and Cochrane areas, closely bracket the 27n–26r chron boundary and as such will be important in detailing the Torrejonian–Tiffanian transition in western Canada.


Zootaxa ◽  
2009 ◽  
Vol 2292 (1) ◽  
pp. 25-33
Author(s):  
LAURENCE A. MOUND

A new genus and species of panchaetothripine thripid, Stosicthrips szitas, apparently related to Parthenothrips dracaenae, is described from leaves of a cultivated Grevillea (Proteaceae) in central Queensland and also at Perth, Australia. In another genus, Bhattithrips, a new species B. borealis is described from northern Australia, and the four members of this Australian genus are distinguished in a key. A species described from Southeast Asia, Astrothrips aureolus, is established and probably native to northern Australia, where it damages the leaves of an Hymenocallis cultivar (Amaryllidaceae).


2000 ◽  
Vol 14 (3) ◽  
pp. 363 ◽  
Author(s):  
William A. Shear

A new genus and species, Infulathrix siam, gen. et sp. nov. and a new species, Heterochordeuma petarberoni, sp. nov. are described from southeast Asia, and the previously known members of the Heterochordeumatidae are reviewed. The genusSumatreuma Hoffman is placed in the synonymy of Heterochordeuma Pocock. Heterochordeumatid gonopod structure is not primitive, as previously supposed, but apomorphic within the superfamily Heterochordeumatoidea and the Diplopoda in general. The families of the order Chordeumatida are grouped into four suborders: Chordeumatidea, Heterochordeumatidea, Craspedosomatidea and Striariidea.


1996 ◽  
Vol 70 (6) ◽  
pp. 969-985 ◽  
Author(s):  
Colin D. Sumrall

A new classification is proposed for late Paleozoic Edrioasteroidea (Echinodermata), separating forms with the advanced clavate thecal design from those with the ancestral pyrgate thecal design, and a new Subfamily Discocystinae is erected to receive the clavate agelacrinitid edrioasteroids. Lepidodiscus Meek and Worthen is restricted to the pyrgate type species L. squamosus (Meek and Worthen) and two unnamed species, whereas the clavate L. laudoni (Bassler) is assigned to Clavidiscus, new genus. The clavate Discocystis priesti Strimple and three new species, Hypsiclavus kinsleyi, new genus and species, Hypsiclavus huntsvillensis, new genus and species, and Hypsiclavus guensburgi, new genus and species, are placed in Hypsiclavus, new genus. Bostryclavus, new genus, is erected to receive Echinodiscus sampsoni Miller. A redescription of Discocystis kaskaskiensis (Hall) and a diagnosis of Spiraclavus Sumrall are included for completeness.


1999 ◽  
Vol 73 (3) ◽  
pp. 389-393 ◽  
Author(s):  
Stan P. Dunagan

Eospongilla morrisonensis n. gen. and sp., the oldest-described freshwater sponge (Demospongea: Spongillidae), is found in the Upper Jurassic (?Oxfordian/Kimmeridgian to Tithonian) Morrison Formation, east-central Colorado, U.S.A. Eospongilla morrisonensis occurs within the well-developed lacustrine carbonate succession of the Morrison Formation, and is represented by two micritic body fossils with calcite-replaced megascleres that range in length from 180 to 300 μm and in diameter from 20 to 35 μm. Megascleres are simple oxeas and strongyles and lack apparent ornamentation, possibly due to the diagenetic replacement. The oxeas are straight but the strongyles display a slight curvature. Microscleres are absent; gemmoscleres were not observed.


2006 ◽  
Vol 43 (11) ◽  
pp. 1695-1709 ◽  
Author(s):  
Craig S Scott

A new genus and species of erinaceid lipotyphlan (Mammalia, Insectivora) from the late Paleocene of western Canada is described. Oncocherus krishtalkai gen. et sp. nov. is known from three late Tiffanian localities in central Alberta and southeastern Saskatchewan and is but one of several erinaceomorph and soricomorph taxa known from the Late Paleocene of western Canada. Oncocherus possesses apomorphies that link it to other primitive erinaceids (e.g., enlarged upper and lower fourth premolars, lower molars markedly decreasing in size from m1-m3, talonid basins V-shaped), yet its affinity with any of the recognized erinaceid subfamilies is uncertain. Although Oncocherus is phenetically, and probably phylogenetically, closest to Litolestes Jepsen, the genus is clearly distinguished from Litolestes and other erinaceid taxa by its proportionately larger and more inflated premolars and lower crowned molars, features that were likely adaptations for durophagy. Oncocherus joins a number of endemic mammalian taxa that were apparently confined to more northerly latitudes of the Western Interior of North America during the Late Paleocene.


Sign in / Sign up

Export Citation Format

Share Document