Modernisation of the Hymenoptera: ants, bees, wasps, and sawflies of the early Eocene Okanagan Highlands of western North America

2018 ◽  
Vol 150 (2) ◽  
pp. 205-257 ◽  
Author(s):  
S. B. Archibald ◽  
Alexandr P. Rasnitsyn ◽  
Denis J. Brothers ◽  
Rolf W. Mathewes

AbstractMost major modern families of Hymenoptera were established in the Mesozoic, but the diversifications within ecologically key trophic guilds and lineages that significantly influence the character of modern terrestrial ecosystems – bees (Apiformes), ants (Formicidae), social Vespidae, parasitoids (Ichneumonidae), and phytophagous Tenthredinoidea – were previously known to occur mostly in the middle to late Eocene. We find these changes earlier, seen here in the early Eocene Okanagan Highlands fossil deposits of western North America. Some of these may have occurred even earlier, but have been obscured by taphonomic processes. We provide an overview of the Okanagan Highlands Hymenoptera to family level and in some cases below that, with a minimum of 25 named families and at least 30 when those tentatively assigned or distinct at family level, but not named are included. Some are poorly known as fossils (Trigonalidae, Siricidae, Peradeniidae, Monomachidae), and some represent the oldest confirmed occurrences (Trigonalidae, Pompilidae, Sphecidaesensu stricto, Peradeniidae, Monomachidae, and possibly Halictidae). Some taxa previously thought to be relictual or extinct by the end of the Cretaceous (Angarosphecidae, Archaeoscoliinae, some Diapriidae) are present and sometimes abundant in the early Eocene. Living relatives of some taxa are now present in different climate regimes or on different continents.

Zootaxa ◽  
2021 ◽  
Vol 4980 (1) ◽  
pp. 142-156
Author(s):  
VLADIMIR N. MAKARKIN ◽  
S. BRUCE ARCHIBALD ◽  
ROLF W. MATHEWES

The osmylid subfamily Protosmylinae is revised based on our emended diagnosis: Petrushevskia Martynova, 1958 and Mesosmylidus Jepson et al., 2012 are excluded (both considered Osmylidae incertae sedis), and Sogjuta Martynova, 1958 is transferred to it from the Mesosmylininae. The late Eocene genus Protosmylus Krüger, 1913 is considered a junior synonym of Osmylidia Cockerell, 1908 based on a distinct apomorphy (deeply forked MA in the hind wing), syn. nov. Three new species of Osmylidia from the early Eocene of North America are described: O. donnae sp. nov. from Quilchena, O. glastrai sp. nov. from Republic, Washington, USA, and an unnamed species of Osmylidia is reported from Driftwood Canyon Provincial Park, British Columbia (all localities of the Okanagan Highlands series), and O. taliae sp. nov. from the Green River Formation of Colorado, USA. 


2019 ◽  
Vol 56 (8) ◽  
pp. 803-813
Author(s):  
Gerald Mayr ◽  
S. Bruce Archibald ◽  
Gary W. Kaiser ◽  
Rolf W. Mathewes

We survey the known avian fossils from Ypresian (early Eocene) fossil sites of the North American Okanagan Highlands, mainly in British Columbia (Canada). All specimens represent taxa that were previously unknown from the Eocene of far-western North America. Wings from the McAbee site are tentatively referred to the Gaviiformes and would constitute the earliest fossil record of this group of birds. A postcranial skeleton from Driftwood Canyon is tentatively assigned to the Songziidae, a taxon originally established for fossils from the Ypresian of China. Two skeletons from Driftwood Canyon and the McAbee site are tentatively referred to Coliiformes and Zygodactylidae, respectively, whereas three further fossils from McAbee, Blakeburn, and Republic (Washington, USA) are too poorly preserved for even a tentative assignment. The specimens from the Okanagan Highlands inhabited relatively high paleoaltitudes with microthermal climates (except Quilchena: lower mesothermal) and mild winters, whereas most other Ypresian fossil birds are from much warmer lowland paleoenvironments with upper mesothermal to megathermal climates. The putative occurrence of a gaviiform bird is particularly noteworthy because diving birds are unknown from other lacustrine Ypresian fossil sites of the Northern Hemisphere. The bones of the putative zygodactylid show a sulphurous colouration, and we hypothesize that this highly unusual preservation may be due to the metabolic activity of sulphide-oxidizing bacteria.


Zootaxa ◽  
2021 ◽  
Vol 4951 (1) ◽  
pp. 41-79
Author(s):  
S. BRUCE ARCHIBALD ◽  
VLADIMIR N. MAKARKIN

Four new species of Raphidiidae are described from the early Eocene of western North America: Megaraphidia antiquissima sp. nov. from McAbee, M. ootsa sp. nov. from Driftwood Canyon, M. hopkinsi sp. nov. from the Allenby Formation (all from British Columbia, Canada), M. klondika sp. nov. from Republic (Washington, United States of America). Archiinocellia Handlirsch, 1910, Archiinocellia oligoneura Handlirsch, 1910 from Horsefly River (British Columbia, Canada), and A. protomaculata (Engel, 2011), comb. nov., from the Green River Formation (Colorado, United States of America) are redescribed. Archiinocellia is assigned to Raphidiidae, sit. nov. The apparent absence of sclerotized gonocoxites 9 in the Archiinocellia protomaculata male is probably plesiomorphic at the family level. As some modern snakeflies do not require a cold interval to complete their development and Eocene Inocelliidae and Raphidiidae lived in regions of warm winters (especially A. protomaculata), adaptation to cold winters in many modern snakeflies is a post-Eocene phenomenon. Eocene Raphidiidae of Europe (Priabonian) differ greatly from those of North America (Ypresian and Priabonian). This pattern might reflect dispersal in either direction or ranges established prior to continental separation. Eocene Inocelliidae of Europe (Priabonian), however, are more similar to those of North America (Ypresian and Lutetian). 


2013 ◽  
Vol 87 (1) ◽  
pp. 123-146 ◽  
Author(s):  
Vladimir N. Makarkin ◽  
S. Bruce Archibald

The early Eocene green lacewings (Neuroptera, Chrysopidae) of the Okanagan Highlands deposits of McAbee, and Driftwood Canyon, British Columbia (Canada) and Republic, Washington (U.S.A.) are treated in detail for the first time. At least six genera are present, one unnamed, three new, with at least 10 new species, six named:Protochrysa fuscobasalisn. sp. (McAbee) (Limaiinae, the youngest known record of the subfamily),Okanaganochrysa coltsunaen. gen. n. sp. (McAbee),Adamsochrysa asperan. gen. n. sp. (McAbee),A. wilsonin. gen. n. sp. (Republic),Archaeochrysa profractan. sp. (McAbee), andPseudochrysopa harveyin. gen. n. sp. (Driftwood Canyon) (all Nothochrysinae, the latter provisionally). The four unnamed species include one assigned toPseudochrysopa, two likely belonging toAdamsochrysa, and one of an unknown nothochrysine genus. Microtholi are detected on the abdominal sclerites ofAdamsochrysa wilsoni, and the spermatheca and spermathecal duct in the abdomen ofPseudochrysopa harveyi, the first reported occurrences of these preserved in fossil Chrysopidae. Structures were detected on the apical wing margins of some species that appear similar to trichosors, which are unknown in Chrysopidae, but are present in some other neuropteran families. This is the richest described assemblage of the family anywhere in the fossil record. Okanagan chrysopids were also morphologically and presumably ecologically diverse, including large species with rich venation and well as those with simplified venation and the smallest known fossil species. This is the oldest reported occurrence of the family in North America.


2019 ◽  
Vol 151 (6) ◽  
pp. 783-816
Author(s):  
S. Bruce Archibald ◽  
Robert A. Cannings

AbstractWe describe the first dragonflies (Odonata: Anisoptera) from the early Eocene Okanagan Highlands of far-western North America from nine fossils. Six are assigned to five species in four new, named genera of Aeshnidae: Antiquiala snyderaenew genus and species, Idemlinea versatilisnew genus and species, Ypshna brownleeinew genus and species, Ypshna latipennatanew genus and species, and Eoshna thompsonensisnew genus and species; we treat one as Aeshnidae genus A, species A; one is assigned to Gomphidae: Auroradraco eosnew genus and species; and we treat a ninth, fragmentary fossil of unknown family affinity as Anisoptera indeterminate genus A, species A, which represents a seventh genus and eighth species. The dominance of Aeshnidae is consistent with other Paleocene and Eocene fossil localities. Auroradraco eos is the only fossil Gomphidae in the roughly 66-million-year gap between occurrences in mid-Cretaceous Burmese amber and the early Oligocene of France. Ypshna appears close to Parabaissaeshna ejerslevense from the early Eocene Fur Formation of Denmark; this is not surprising given Holarctic intercontinental connections at this time and a growing list of insect taxa shared between the Okanagan Highlands and the Fur Formation.


Zootaxa ◽  
2021 ◽  
Vol 4966 (3) ◽  
pp. 392-400
Author(s):  
S. BRUCE ARCHIBALD ◽  
ROBERT A. CANNINGS

We describe Republica weatbrooki, a new genus and species of damselfly (Odonata, Zygoptera, Euphaeidae, Eodichromatinae) from the early Eocene (Ypresian) fossil locality at Republic, Washington, U.S.A. Its single specimen is the sole damselfly known from the Okanagan Highlands series of localities in far-western North America. 


1997 ◽  
Vol 71 (6) ◽  
pp. 1109-1124 ◽  
Author(s):  
Li Guo-Qing ◽  
Mark V. H. Wilson ◽  
Lance Grande

Review of recently collected material of Eohiodon from North America suggests that there are two valid species, E. rosei (Hussakof) and E. woodroffi Wilson. Eohiodon falcatus Grande is identical to E. woodruffi in known skeletal features and nearly all meristic features and is treated as a junior synonym of the latter. The fossil genus Eohiodon Cavender differs from Hiodon Lesueur, which is known from both fossil and extant species, in numerous meristic and osteological features. The caudal skeleton in Eohiodon is nearly identical to that in Hiodon.The traditionally accepted Notopteroidei, containing Lycopteridae, Hiodontidae, and Notopteridae, is a polypheletic group. The Asian fossil family Lycopteridae is not more closely related to Hiodontidae than it is to other taxa in the Osteoglossomorpha, but is sister to all other Osteoglossomorpha. The Hiodontiformes sensu stricto, including only the family Hiodontidae, is the sister-group of the Osteoglossiformes. This family is not more closely related to notopterids than to other taxa in Osteoglossiformes. The Notopteridae are most closely related to the Mormyroidea; together they and the fossil family Ostariostomidae constitute the sister-group of the Osteoglossoidei.Fossil records of Hiodontiformes sensu stricto and Notopteroidei indicate a widespread pre-Neogene biogeographic range of these freshwater teleosts, suggesting that extinction must have been involved in the Cenozoic evolution of these two osteoglossomorph sublineages.


Geology ◽  
1991 ◽  
Vol 19 (12) ◽  
pp. 1189 ◽  
Author(s):  
Scott L. Wing ◽  
Thomas M. Bown ◽  
John D. Obradovich

2009 ◽  
Vol 141 (3) ◽  
pp. 246-308 ◽  
Author(s):  
Valerie M. Behan-Pelletier ◽  
Barbara Eamer

AbstractThe oribatid mite genusCeratozetesBerlese is represented in America north of Mexico by 21 previously described species known from forest, grassland, subarctic and arctic soils and litter, and canopy habitats. The closely related genusCeratozetoidesShaldybina is represented in America north of Mexico only byC. cisalpinus(Berlese). Three new species ofCeratozetesfrom North America are described:C. biporosussp. nov.from forest habitats of southeastern North America,C. cyclopeasp. nov.from montane habitats in western North America, andC. pseudomediocrissp. nov.from forest habitats of western North America. A detailed revised diagnosis is given forCeratozetes,Ceratozetoides, all previously described species ofCeratozetes(C. angustus(Banks),C. borealisBehan-Pelletier,C. cuspidatusJacot,C. enodis(Ewing),C. fjellbergiBehan-Pelletier,C. gracilisMichael,C. kutchinBehan-Pelletier,C. longispinusJacot,C. mediocris(Berlese),C. oresbiosBehan-Pelletier,C. pacificusBehan-Pelletier,C. parvulusSellnick,C. spitsbergensisThor,C. subaquila(Ewing),C. subinconspicuus(Berlese),C. thienemanniWillmann,C. virginicus(Banks), andC. watertonensisBehan-Pelletier), andCeratozetoides cisalpinus.Ceratozetes figuratus(Ewing) andC. zeteki(Ewing) are considered junior subjective synonyms ofC. enodis(Ewing)syn. nov., andC. inupiaqBehan-Pelletier is transferred to Mycobatidae asCyrtozetes inupiaq(Behan-Pelletier)comb. nov. New distribution records are given forCeratozetoides cisalpinusandCeratozetes angustus,C. borealis,C. cuspidatus,C. gracilis,C. mediocris,C. longispinus,C. oresbios,C. pacificus,C. parvulus,C. thienemanni,C. virginicus, andC. watertonensis.A diagnostic key is provided to adults of theCeratozetesandCeratozetoidesspecies now known for America north of Mexico. An analysis of the systematic relationships of 23 of these species based on adult characters indicates thatCeratozetes, excludingCeratozetoides, is paraphyletic. The clade that includesCeratozetoides cisalpinusand 15 species ofCeratozetesincludes most species for which immatures are known. One sister clade includesCeratozetes cyclopea,C. enodis, andC. fjellbergiand another includesC. kutchin, C. parvulus, andC. thienemanni.The decision whether or not these 6 species should be retained inCeratozetessensu strictoawaits discovery of their immatures and molecular analysis.


Sign in / Sign up

Export Citation Format

Share Document