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Two new species of fossil Eomerope (Mecoptera: Eomeropidae) from the Ypresian Okanagan Highlands, far-western North America, and Eocene Holarctic dispersal of the genus

Published online by Cambridge University Press:  09 March 2018

S. Bruce Archibald*
Affiliation:
Department of Biological Sciences, Simon Fraser University, 8888 University Drive, Burnaby, British Columbia, V5A 1S6, Canada Museum of Comparative Zoology, 26 Oxford Street, Cambridge, Massachusetts, 02138, United States of America Royal British Columbia Museum, 65 Belleville Street, Victoria, British Columbia, V8W 9W2, Canada
Alexandr P. Rasnitsyn
Affiliation:
A.A. Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117647, Russia Invertebrate Palaeontology Department, Natural History Museum, Cromwell Road, London, SW7 5BD, United Kingdom
*
1Corresponding author (e-mail: sba48@sfu.ca)

Abstract

Two new species of Eocene Eomerope Cockerell (Mecoptera: Eomeropidae) are described from the Ypresian Okanagan Highlands deposits of British Columbia, Canada: Eomerope simpkinsaenew species from the Allenby Formation near the town of Princeton, and Eomerope eonearcticanew species from the McAbee locality near the towns of Cache Creek and Ashcroft. Eomerope eonearctica is very close to the coeval Eomerope asiatica Ponomarenko from Primorskiy Kray in Pacific-coastal Russia, consistent with Eocene intercontinental dispersal, which is well documented in numerous plant and animal taxa.

Type
Biodiversity & Evolution
Copyright
© Entomological Society of Canada 2018 

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References

Archibald, S.B. 2005. New Dinopanorpidae (Insecta: Mecoptera) from the Eocene Okanagan Highlands (British Columbia, Canada and Washington State, USA). Canadian Journal of Earth Sciences, 42: 119136.Google Scholar
Archibald, S.B., Bossert, W.H., Greenwood, D.R., and Farrell, B.D. 2010. Seasonality, the latitudinal gradient of diversity, and Eocene insects. Paleobiology, 36: 374398.Google Scholar
Archibald, S.B., Cover, S.D., and Moreau, C.S. 2006. Bulldog ants of the Eocene Okanagan Highlands, and the history of the subfamily (Hymenoptera: Formicidae: Myrmeciinae). Annals of the Entomological Society of America, 99: 487523.Google Scholar
Archibald, S.B., Rasnitsyn, A.P., and Akhmetiev, M.A. 2005. The ecology and distribution of Cenozoic Eomeropidae (Mecoptera), and a new species of Eomerope Cockerell from the Early Eocene McAbee locality, British Columbia, Canada. Annals of the Entomological Society of America, 98: 503514.Google Scholar
Beard, K.C. and Dawson, M.R. 1999. Intercontinental dispersal of Holarctic land mammals near the Paleocene/Eocene boundary; paleogeographic, paleoclimatic and biostratigraphic implications. Bulletin de la Société géologique de France, 170: 697706.Google Scholar
Bowen, G.J., Clyde, W.C., Koch, P.L., Ting, S., Alroy, J., Tsubamoto, T., et al. 2002. Mammal dispersal at the Paleocene/Eocene boundary. Science, 295: 20622065.Google Scholar
Brikiatis, L. 2014. The De Geer, Thulean and Beringia routes: key concepts for understanding early Cenozoic biogeography. Journal of Biogeography, 41: 10361054.Google Scholar
Cockerell, T.D.A. 1909. Description of Tertiary insects, VI. American Journal of Science, 27: 381387.CrossRefGoogle Scholar
Cockerell, T.D.A. 1924. Fossil insects in the United States National Museum. Proceedings of the United States National Museum, 64: 1–15.Google Scholar
Dlussky, G.M., Rasnitsyn, A.P., and Perfilieva, K.S. 2015. The ants (Hymenoptera: Formicidae) of Bol’shaya Svetlovodnaya (Late Eocene of Sikhote-Alin, Russian Far East). Caucasian Entomological Bulletin, 11: 131152.Google Scholar
Greenwood, D.R., Archibald, S.B., Mathewes, R.W., and Moss, P.T. 2005. Fossil biotas from the Okanagan Highlands, southern British Columbia and northern Washington State: climates and ecosystems across an Eocene landscape. Canadian Journal of Earth Sciences, 42: 167185.Google Scholar
Manchester, S.R. 1999. Biogeographical relationships of North American Tertiary floras. Annals of the Missouri Botanical Garden, 86: 472522.Google Scholar
Manchester, S.R., Chen, Z.D., LU, A.M., and Uemura, K. 2009. Eastern Asian endemic seed plant genera and their paleogeographic history throughout the Northern Hemisphere. Journal of Systematics and Evolution, 47: 142.Google Scholar
Manchester, S.R. and Tiffney, B.H. 2001. Integration of paleobotanical and neobotanical data in the assessment of phytogeographic history of holarctic angiosperm clades. International Journal of Plant Sciences, 162: S19S27.Google Scholar
Moss, P.T., Greenwood, D.R., and Archibald, S.B. 2005. Regional and local vegetation community dynamics of the Eocene Okanagan Highlands (British Columbia-Washington State) from palynology. Canadian Journal of Earth Sciences, 42: 187204.Google Scholar
Peña, L.E. 1968. Natural history notes on Notiothauma . Discovery (Yale University), 4: 4244.Google Scholar
Penny, N.D. 1975. Evolution of the extant Mecoptera. Journal of the Kansas Entomological Society, 48: 331350.Google Scholar
Ponomarenko, A.G. and Rasnitsyn, A.P. 1974. New Mesozoic and Cenozoic Protomecoptera. Paleontological Journal, 4: 493507.Google Scholar
Popov, V.K. and Grebennikov, A.V. 2001. New data on the age of effusives from the Bogopol Formation in Primorye. Tikhookeanskaya Geologiya, 3: 4754.Google Scholar
Ren, D. and Shih, C.K. 2005. The first discovery of fossil eomeropids from China (Insecta, Mecoptera). Acta Zootaxonomica Sinica, 30: 275280.Google Scholar
Rust, J. and Andersen, N.M. 1999. Giant ants from Paleogene of Denmark with a discussion of the fossil history and early evolution of ants (Hymenoptera: Formicidae). Zoological Journal of the Linnean Society, 125: 331348.Google Scholar
Soszyńska-Maj, A., Krzemiński, W., Kopeć, K., and Coram, R.A. 2016. Phylogenetic relationships within the relict family Eomeropidae (Insecta, Mecoptera) based on the oldest fossil from the Early Jurassic (Sinemurian) of Dorset, southern England. Journal of Systematic Palaeontology, 14: 10251031.Google Scholar
Suan, G., Popescu, S.M., Suc, J.P., Schnyder, J., Fauquette, S., Baudin, F., et al. 2017. Subtropical climate conditions and mangrove growth in Arctic Siberia during the early Eocene. Geology, 45: 539542.Google Scholar
Tiffney, B.H. 2000. Geographic and climatic influences on the Cretaceous and Tertiary history of Euramerican floristic similarity. Acta Universitatis Carolinae Geologica, 44: 516.Google Scholar
Tiffney, B.H. and Manchester, S.R. 2001. The use of geological and paleontological evidence in evaluating plant phylogeographic hypotheses in the Northern Hemisphere Tertiary. International Journal of Plant Sciences, 162: S3S17.Google Scholar
Willmann, R. 1989. Evolution und Phylogenetisches System der Mecoptera (Insecta: Holometabola). Abhandlungen der Senckenbergischen Naturforschenden Gesellschaft, 544: 1153.Google Scholar
Woodburne, M.O. and Swisher, C.C. 1995. Land mammal high-resolution geochronology, intercontinental overland dispersals, sea level, climate, and vicariance. In Geochronology, time scales, and global stratigraphic correlations: unified temporal framework for an historical geology. Edited by W.A. Berggren, D.V. Kent, M.-P. Aubry, and J. Hardenbol. Society for Sedimentary Geology Special Publication 54. Society for Sedimentary Geology, Tulsa, Oklahoma, United States of America. Pp. 335364.Google Scholar
Zhang, J.-X., Shih, C.K., Petrulevičius, J.F., and Ren, D. 2011. A new fossil eomeropid (Insecta, Mecoptera) from the Jiulongshan Formation, Inner Mongolia, China. Zoosystema, 33: 443450.Google Scholar
Zhang, J.-X., Shih, C.K., and Ren, D. 2012. A new fossil eomeropid (Insecta, Mecoptera) from the Yixian Formation, Liaoning, China. Acta Zootaxonomica Sinica, 37: 6871.Google Scholar
Zherikhin, V.V. 1978. Razvitie i smena melovykh i kainozoiskikh faunisticheskikh kompleksov (trakheinye i khelitserovye) [Development and changes in Cretaceous and Cenozoic faunistic complexes (tracheates and chelicerates)]. Trudy Paleontologicheskogo Instituta, 165: 1200.Google Scholar