ebook img

Longioculus burmensis, N. gen., N. sp. (Orthoptera: Elcanidae) in burmese amber PDF

2007·3.5 MB·
Save to my drive
Quick download
Download
Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.

Preview Longioculus burmensis, N. gen., N. sp. (Orthoptera: Elcanidae) in burmese amber

PROC. ENTOMOL. SOC. WASH. 109(3), 2007, pp. 649-655 LONGIOCULUS BURMENSIS, N. GEN., N. SP. (ORTHOPTERA: ELCANIDAE) IN BURMESE AMBER George Poinar, Jr., Andrej V. Gorochov, and Ron Buckley (GP) Department of Zoology, Oregon State University, Corvallis, OR 97331, U.S.A. (e-mail: [email protected]); (AG) Zoological Institute, Russian Academy of Sciences, S. Petersburg 199034, Russia (e-mail: [email protected]); (RB) 9635 Sumpter Road, Florence, KY 41042-8355, U.S.A. (e-mail: [email protected]) — Abstract. An adult orthopteran in Early Cretaceous Burmese amber is described as a new genus and species, Longiociiliis burmensis Poinar, Gorochov, and Buckley. On the basis ofits tegminal venation, three-segmented tarsi, and large spines on the hind tibia, it is placed in the extinct family Elcanidae. This fossil differs from previously described members ofthe family by its relatively small and slender body, protruding eyes, enlarged scapes and antennal cavities, short pronotum, and unique venational and leg armament characters. Key Words: Orthoptera, Elcanidae, Longioculus, Longioculus burmensis, Burmese amber, Early Cretaceous Adult orthopterans in amber are rare, unpublished research 2002). Palyno- since these insects are usually strong morphs from the amber beds where the enough to free themselves from the resin. fossil originated have been assigned to the A well-preserved Burmese amber orthop- Upper Albian of the Lower Cretaceous teroid previously depicted in Poinar et al. (-100 mya) (Cruickshank and Ko 2003); (2005) is the topic of this paper. The however, since the amber is secondarily specimen has three-segmented tarsi, deposited, the age could be older. a short pronotum, enlarged hind femora, The piece of amber containing the and venational characters that align it specimen is rectangular in shape, mea- mm mm with members of the family Elcanidae suring 13 in length, 10 in width mm (Sharov 1968, Carpenter 1992, Gorochov and 6 in depth. The fossil is well 1995, Gorochov and Rasnitsyn 2002). preserved and complete except for the tips of the antennae and wings, one side Materials and Methods of the apex of the abdomen (including Amber from Burma occurs in lignitic one cercus and the genital apparatus), seams in sandstone-limestone deposits in the left metatibia and metatarsus and the the Hukawng Valley, southwest ofMain- apical portion of the right metatibia. gkhwan in the state of Kachin (26'20'N, Other fossils in the same amber piece are 96'36'E). Nuclear magnetic resonance three small adult beetles, one mite, one (NMR) spectra of amber samples taken adult neinatoceran and several branched from the same locality as the fossils plant hairs. Observations and photo- indicated an araucarian (possibly Agathis) graphs were made with a Nikon SMZ- source of the amber (Lambert and Wu, 10 stereoscopic microscope and Nikon 650 PROCEEDINGS OF THE ENTOMOLOGICAL SOCIETY OF WASHINGTON — — VOLUME NUMBER 109, 3 651 Optiphot optical microscope (with mag- Cretaceous Cratoelcana Martins- Neto nifications up to 650X). (Martins-Neto 1991), by the apices of the branches of tegminal "C" positioned Family Elcanidae Handlirsch, 1906 within a short distance of each other and the most proximal crossvein in the area Longioculus Poinar, Gorochov, and between R+ RS (possibly the basal part of Buckley, new genus — RS) situatednearthebasesofthethirdand Description. Body relatively small fourth branchesofRA. From Cratoelcana, and slender; scapes and antennal cavities with species over20 mm in length, thenew greatly enlarged, occupying entire area genus differs in being much smaller (under between compound eyes; compound eyes 8 mm in length). large, protruding from head; ocelli lack- Type species. Longioculus burmensis, ing; pronotum short, hind tibia with n. sp. dorsal row ofdenticles and row ofmuch larger spines in middle part (and possibly Longioculus burmensis Poinar, Gorochov, in distal part); ventral surface of hind and Buckley, new species basitarsus with row ofrather long spines; (Figs. 1-12) tegmina with both branches of false — costa ("C") meeting within short dis- Description. Characters as listed un- tance of each other on anterior wing der generic description. Alate male; body margin; tegminal area between "C" and brown with transparent wing; length Sc narrow; tegminal crossveins in visible body, 7.14 mm; length pronotum, 2.4 area between R+ RA reduced (most mm; length hind femur, 6.4 mm. proximal crossvein in the area, possibly Head: Narrow; without rostral tuber- basal part of RS, situated between bases cles between antennal cavities; ocelli not of third and fourth branches of RA). observed; antennalcavities incontactwith Etymology. ''Longioculus'" is from each other, with edges prominent; anten- the Latin "oculus" for eye and "longus" nal scapes enlarged; antennal flagellum for long, in reference to the protruding longerthan body(bothantennaecutoffat eyes. The gen—der is masculine. edge of amber piece); filiform; antenno- Diagnosis. On the basis of the nar- meres short, equal or subequal in size; row, large spines on the hind tibiae, the each antennomere bears one to several new genus may belong to the Late spines; genae narrow; clypeus and mouth- Jurassic-Early Cretaceous subfamily Elca- parts more or less normal for Ensifera ninae (= Baisselcaninae). Longioculus is (only lower edge oflabrum exposed). similar in size to the Early Cretaceous Thorax: Pronotum saddle-shaped, with genus Minelcana Gorochov, Jarzembow- anterior margin convex; pronotal dorsum sky, and Coram (Gorochov et al. 2006) with seven circular light blotches with and the smallest species of the Early dark borders located in depressions sym- Cretaceous genus Panorpidium Westwood metrically positioned on each side; hind (Westwood 1854), butcanbedistinguished part ofpronotum convex, not prolonged from both these genera as well as from over abdomen; legs covered with short othergeneraofElcanidae, exceptthe Early hairs; fore- and midfemora with pair of Figs. 1-4. LongioculusburmensisinBurmeseamber. 1, Lateralviewofentirespecimen. Bar = 1.6 mm. 2, Metatarsusshowinglongspine(arrow) and twodenticles(arrowheads). Bar = 88 |im. 3, Dorsalviewof anteriorportion showingprotrudingeyes (arrows) and roundcolored areas on pronotum. Bar = 542 \im. 4, Portion ofantenna showing scattered setae. Bar = 63 (im. 652 PROCEEDINGS OF THE ENTOMOLOGICAL SOCIETY OF WASHINGTON VOLUME NUMBER 109, 3 653 Figs. 10-12. Longioculus bwinensis in Bunnese amber. 10, Venation of tegmina. Dotted portions representreconstructed areas. Bar = 1 mm. 11, Frontalviewshowingprotrudingeyes, prominentantennal cavities and enlarged antennal scapes. Bar = 1 mm. 12, Hind leg showing denticles and spines on dorsal surface ofmetatibia and spines on ventral surface ofbasitarsus. Dotted portions represent reconstructed areas. Bar = 1 mm. rounded apical lobules, lacking denticles; dorsal surface bearing single row ofsmall fore tibia with single apical outer spine; denticles from 25-31 jam in height and mid- and hind tibiae with pair of apical 25-31 i^m in width at base; distance spines; basal portion of hind tibia on between denticles 201-246 jam; denticles Figs. 5-9. Longioculus burmensis in Burmese amber. 5, Frontal view. Bar = 375 )am. 6, Mouthparts. Bar = 700 (im. 7, Metatarsus (arrow points to small spines on first tarsal segment of metatarsus) and mesotarsus (arrowhead). Note rows of large spines opposite small spines on ventral surface of basimetatarsus. Bar = 800 |J,m. 8, Denticles on proximal portion ofmetatibia. Bar = 575 jam. 9. Portion ofabdomen showing remaining cercus. Bar = 800 ^m. PROCEEDINGS OF THE ENTOMOLOGICAL SOCIETY OF WASHINGTON 654 replaced on middle part (and possibly on suggests that the entire distal portion distal part) ofdorsal surface of hind tibia contained a row of large spines, which is by large spines (only one complete spine, typical for elcanids. The depressed col- 265 |Lim long and 63 ^m wide, and one ored areas on the dorsum of the prono- partial second spine visible); distance tum probably served as camouflage. between first andsecondlargetibial spines, 315 jam; all tarsi with first segment longer Discussion than 2nd and 3rd combined; apex of all Fossils of the superfamily Elcanoidea basitarsi with 2 pairs of apical spines; first appeared in the Early Permian and midtarsus very short, less than Va as long extended into the mid-Cretaceous. Mem- as basitarsus; third tarsal segments with bers ofthe grasshopper-appearing family well- developed, simple, slightly curved Elcanidae first appeared in the Early claws; arolium absent; fore- and midbasi- Jurassic and representatives of the sub- tarsi with 2 rows ofshort spines on dorsal family Elcaninae, which ranged from and ventral surfaces; hind basitarsus with Siberiato England and Brazil, wererather two rows of spines, dorsal row composed common in Lower Cretaceous localities of 27 short spines and ventral row with 7 (Martins-Neto 1991; Gorochov 1995; large spines; midtarsus without spines; Gorochov and Rasnitsyn 2002). The tegmina membranous (wings folded); ve- small size of Longioculus may indicate nation as shown in Fig. 10; tegmina how it became entrapped in amber. coloration light (transparent) with dark veins and clear area between first and Acknowledgments second branches ofRA. Abdomen: Short, robust; cercus slen- We thank Jim Davis for supplying the der, pointed, approximately 1/3 length of amber, J. B. Lambert and Y. Wu, De- abdomen; base of cercus with single, partment of Chemistry, Northwestern small, outer sensilla; anal plate, subgeni- University, for their analysis of the tal plate, and genital apparatus missing. amber, and RobertaPoinarforcomments — Material examined. Holotype male on an earlier draft ofthis manuscript. in Burmese amber from the Hukawng Valley, southwest of Maingkhwan in the Literature Cited state of Kachin (26°20'N, 96°36'E), Carpenter, F. M. 1992. Superclass Hexapoda. In northern Myanmar (Burma), deposited Kaesler, R. L. ed. Treatise on Invertebrate in the amber collection of Ron Buckley, Paleontology, Part R, Arthropoda 4, Vol- Florence, Kentucky (accession # ab ume 3. The Geological Society of America 307). The specimen is available for study and The University of Kansas, Boulder and Lawrence. 277 pp. by contacting R. Buckley. — Cruickshank. R. D. and K. Ko. 2002. Geology of Etymology. The specific name "bur- an amber locality in the Hukawng Valley, mensis" indicates the place of origin of northern Myanmar. Journal of Asian Earth the fossil. Sciences 21: 441^55. Comments.—Unfortunately, the left Gorochov, A. V. 1995. System andevolution ofthe hind tibia is missing and only the cseuebdoirndgesroEfnstihfeerZaoo(lOorgtihcoaplterIans)t.ituPtaer,tR1u.ssPiraon- proximal half of the right hind tibia is Academy ofSciences [Trudy Zoologicheskogo present (the remainder is obliterated by Instituta RAN], v. 260: 1-224 (in Russian). a cavity in the amber) but the right Gorochov, A. V. and A. P. Rasnitsyn. 2002. midtarsus is present on the other side of Superorder Gryllidea. Laicharting, 1781 (= the cavity. One complete and a second Orthopteroidea Handlirsch, 1903). pp. 293-303. In Rasnitsyn, A. P. and D. L. J. Quicke, eds. partial spine positioned at the distal end HistoryofInsects.KluwerAcademicPublishers, ofthe remaining portion ofthe hind tibia Dordrecht. VOLUME 109, NUMBER 3 655 Gorochov, A. V., E. A. Jarzembowski, and R. A. Poinar,Jr., G. O.,R. Buckley, andA. Brown. 2005. Coram. 2006. Grasshoppers and crickets (In- The secrets of Burmese amber. Mid Atlantic sects: Orthoptera) from the Lower Cretaceous Paleontology Society 29: 20-29. ofsouthern England. Cretaceous Research 27: Sharov, A. G. 1968. Phylogeny of orthopteroid 641-662. insects. Proceedings of the Paleontological Martins-Neto, R. G. 1991. Sistematica dos En- Institute, Academy of Sciences of the USSR sifera (Insects, Orthopteroida) da Formagao 118: 1-216 (in Russian). Santana, Cretaceo Inferior do nordeste do Westwood, J. D. 1854. Contributions to fossil Brasil. EstudioTechnologicos, Acta Geologica entomology. Quarterly Journal of the Geo- Leopoldensia 32: 3-162. logical Society ofLondon 10: 378-396.

See more

The list of books you might like

Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.