Lower Permian Insects from Oklahoma Part 2. Orders Ephemeroptera and Palaeodictyoptera* by Frank M
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New Insects from the Earliest Permian of Carrizo Arroyo (New Mexico, USA) Bridging the Gap Between the Carboniferous and Permian Entomofaunas
Insect Systematics & Evolution 48 (2017) 493–511 brill.com/ise New insects from the earliest Permian of Carrizo Arroyo (New Mexico, USA) bridging the gap between the Carboniferous and Permian entomofaunas Jakub Prokopa,* and Jarmila Kukalová-Peckb aDepartment of Zoology, Faculty of Science, Charles University, Viničná 7, CZ-128 43 Praha 2, Czech Republic bEntomology, Canadian Museum of Nature, Ottawa, ON, Canada K1P 6P4 *Corresponding author, e-mail: [email protected] Version of Record, published online 7 April 2017; published in print 1 November 2017 Abstract New insects are described from the early Asselian of the Bursum Formation in Carrizo Arroyo, NM, USA. Carrizoneura carpenteri gen. et sp. nov. (Syntonopteridae) demonstrates traits in hindwing venation to Lithoneura and Syntonoptera, both known from the Moscovian of Illinois. Carrizoneura represents the latest unambiguous record of Syntonopteridae. Martynovia insignis represents the earliest evidence of Mar- tynoviidae. Carrizodiaphanoptera permiana gen. et sp. nov. extends range of Diaphanopteridae previously restricted to Gzhelian. The re-examination of the type speciesDiaphanoptera munieri reveals basally coa- lesced vein MA with stem of R and RP resulting in family diagnosis emendation. Arroyohymen splendens gen. et sp. nov. (Protohymenidae) displays features in venation similar to taxa known from early and late Permian from the USA and Russia. A new palaeodictyopteran wing attributable to Carrizopteryx cf. arroyo (Calvertiellidae) provides data on fore wing venation previously unknown. Thus, all these new discoveries show close relationship between late Pennsylvanian and early Permian entomofaunas. Keywords Ephemeropterida; Diaphanopterodea; Megasecoptera; Palaeodictyoptera; gen. et sp. nov; early Asselian; wing venation Introduction The fossil record of insects from continental deposits near the Carboniferous-Permian boundary is important for correlating insect evolution with changes in climate and in plant ecosystems. -
1 General Introduction
1 General Introduction If the karate-ka (student) shall walk the true path, first he will cast aside all preference. Tatsuo Shimabuku, Grand Master of Isshin-ryu Karate 1.1 The Importance of Insects ~30% of the plants we grow for food and materials. Because of their great numbers and diversity, insects Insects transmit some of these pathogens. While have a considerable impact on human life and indus- weeds can often reduce pest attack, they can also try, particularly away from cities and in the tropics. harbour the pest’s enemies or provide alternative On the positive side they form a large and irreplace- resources for the pest itself. Then in storage, insects, able part of the ecosystem, especially as pollinators mites, rodents and fungi cause a further 30% loss. of fruit and vegetable crops and, of course, many Apart from such biotic damage, severe physical con- wild plants (Section 8.2.1). They also have a place ditions such as drought, storms and flooding cause in soil formation (Section 8.2.4) and are being used additional losses. For example, under ideal field increasingly in ‘greener’ methods of pest control. conditions new wheat varieties (e.g. Agnote and Biological control using insects as predators and Humber) would give yields of ~16 tonnes/ha, but parasites of pest insects has been developed in the produce typically about half this under good hus- West for over a century, and much longer in China. bandry. Pre-harvest destruction due only to insects More recently integrated pest management (IPM) is 10–13% (Pimentel et al., 1984; Thacker, 2002). -
Frank Morton Carpenter (1902-1994): Academic Biography and List of Publications
FRANK MORTON CARPENTER (1902-1994): ACADEMIC BIOGRAPHY AND LIST OF PUBLICATIONS BY DAVID G. FURTH 18 Hamilton Rd., Arlington, MA 02174 The present paper is meant to accompany the preceding one by Elizabeth Brosius, Assistant Editor at the University of Kansas, Paleontological Institute, who was extremely instrumental in aid- ing Prof. Frank Carpenter to finish his Treatise on Invertebrate Paleontology volumes on fossil insects. The Brosius paper is a brief profile taken from her personal interaction with Prof. Carpen- ter as well as numerous interviews about him with his friends, stu- dents, and colleagues. The present paper is intended to be more of an account of Prof. Carpenter's academic background and accom- plishments with the addition of some personal and academic accounts of the author's interaction with Frank Carpenter. Frank Morton Carpenter was born in Boston on 6 September 1902. When he was three years old his family (father Edwin A. and mother Maude Wall) moved from Boston to Revere and at age six his family moved to Melrose where he began to attend Lincoln School the following year. His father worked for the American Express Company but had a strong interest in natural history and taught his elder son (Edwin, four years older than Frank) about the constellations. Edwin later graduated from Harvard, studied astronomy, and became Director of the Astronomical Laboratory at the University of Arizona in Tucson. When Frank Carpenter was a sixth grader at Lincoln School his father encouraged his interest in butterflies and moths. In ninth grade Frank Carpenter began taking out books about insects from the Melrose Public Library. -
THE ORIGIN and EVOLUTION of HYMENOPTEROUS INSECTS [P
THE ORIGIN AND EVOLUTION OF HYMENOPTEROUS INSECTS [p. 24] Chapter 3 EVOLUTION OF THE INFRACLASS SCARABAEONES A. P. Rasnitzyn* Dragonflies [order Odonata] and mayflies [order Ephemeroptera], which have retained a primitive thorax structure (absence of a cryptosternum) but are specialized in other respects, occupy the most isolated position in the infraclass. They are similar to each other in a number of characters, but the nature of the latter does not allow drawing a conclusion about any close relationship of the two orders. Indeed, the primitiveness of the structure of the thorax common to both of them, like any symplesiomorphy, is not evidence of a common origin. The adaptations of the larvae of mayflies and dragonflies to an aquatic way of life are different, and they show, rather, an independent transition to development in water. The loss of the ability to fold the wings as well is connected with different processes in them: in mayflies, with the ephemerality of the imago, the function of which is essentially limited to nuptial flight and oviposition; and in dragonflies, with the metamorphosis of the adult insect to an active aerial predator. It is highly probable that mayflies and dragonflies are independent evolutionary branches. The belonging of dragonflies and mayflies to a common trunk of Scarabaeones, that is, the isolation of them from Protoptera as part of a single trunk with the remaining members of the infraclass (except Protoptera), is confirmed by the metamorphosis of the style of the ninth segment in mayfly males into part of the copulatory organ [endophallus], and in dragonfly females into a sheath of the ovipositor. -
Evolution of the Insects David Grimaldi and Michael S
Cambridge University Press 0521821495 - Evolution of the Insects David Grimaldi and Michael S. Engel Index More information INDEX 12S rDNA, 32, 228, 269 Aenetus, 557 91; general, 57; inclusions, 57; menageries 16S rDNA, 32, 60, 237, 249, 269 Aenigmatiinae, 536 in, 56; Mexican, 55; parasitism in, 57; 18S rDNA, 32, 60, 61, 158, 228, 274, 275, 285, Aenne, 489 preservation in, 58; resinite, 55; sub-fossil 304, 307, 335, 360, 366, 369, 395, 399, 402, Aeolothripidae, 284, 285, 286 resin, 57; symbioses in, 303; taphonomy, 468, 475 Aeshnoidea, 187 57 28S rDNA, 32, 158, 278, 402, 468, 475, 522, 526 African rock crawlers (see Ambermantis wozniaki, 259 Mantophasmatodea) Amblycera, 274, 278 A Afroclinocera, 630 Amblyoponini, 446, 490 aardvark, 638 Agaonidae, 573, 616: fossil, 423 Amblypygida, 99, 104, 105: in amber, 104 abdomen: function, 131; structure, 131–136 Agaoninae, 423 Amborella trichopoda, 613, 620 Abies, 410 Agassiz, Alexander, 26 Ameghinoia, 450, 632 Abrocomophagidae, 274 Agathiphaga, 560 Ameletopsidae, 628 Acacia, 283 Agathiphagidae, 561, 562, 567, 630 American Museum of Natural History, 26, 87, acalyptrate Diptera: ecological diversity, 540; Agathis, 76 91 taxonomy, 540 Agelaia, 439 Amesiginae, 630 Acanthocnemidae, 391 ages, using fossils, 37–39; using DNA, 38–40 ametaboly, 331 Acari, 99, 105–107: diversity, 101, fossils, 53, Ageniellini, 435 amino acids: racemization, 61 105–107; in-Cretaceous amber, 105, 106 Aglaspidida, 99 ammonites, 63, 642 Aceraceae, 413 Aglia, 582 Amorphoscelidae, 254, 257 Acerentomoidea, 113 Agrias, 600 Amphientomidae, -
Diversification of Insects Since the Devonian
www.nature.com/scientificreports OPEN Diversifcation of insects since the Devonian: a new approach based on morphological disparity of Received: 18 September 2017 Accepted: 12 February 2018 mouthparts Published: xx xx xxxx Patricia Nel1,2, Sylvain Bertrand2 & André Nel1 The majority of the analyses of the evolutionary history of the megadiverse class Insecta are based on the documented taxonomic palaeobiodiversity. A diferent approach, poorly investigated, is to focus on morphological disparity, linked to changes in the organisms’ functioning. Here we establish a hierarchy of the great geological epochs based on a new method using Wagner parsimony and a ‘presence/ absence of a morphological type of mouthpart of Hexapoda’ dataset. We showed the absence of major rupture in the evolution of the mouthparts, but six epochs during which numerous innovations and few extinctions happened, i.e., Late Carboniferous, Middle and Late Triassic, ‘Callovian-Oxfordian’, ‘Early’ Cretaceous, and ‘Albian-Cenomanian’. The three crises Permian-Triassic, Triassic-Jurassic, and Cretaceous-Cenozoic had no strong, visible impact on mouthparts types. We particularly emphasize the origination of mouthparts linked to nectarivory during the Cretaceous Terrestrial Revolution. We also underline the origination of mouthparts linked to phytophagy during the Middle and the Late Triassic, correlated to the diversifcation of the gymnosperms, especially in relation to the complex ‘fowers’ producing nectar of the Bennettitales and Gnetales. During their ca. 410 Ma history, hexapods have evolved morphologically to adapt in a continuously changing world, thereby resulting in a unique mega-biodiversity1. Age-old questions2–4 about insects’ macroevolution now- adays receive renewed interest thanks to the remarkable recent improvements in data and methods that allow incorporating full data, phylogenomic trees besides fossil record5–9. -
PALAEODICTYOPTERA, MEGASECOPTERA and DIAPHANOPTERODEA (PALEOPTERA)* by JARMILA KUKALOVA-Peck Department of Geology, Carleton University Ottawa, Ontario, Canada
PTERALIA OF THE PALEOZOIC INSECT ORDERS PALAEODICTYOPTERA, MEGASECOPTERA AND DIAPHANOPTERODEA (PALEOPTERA)* BY JARMILA KUKALOVA-PEcK Department of Geology, Carleton University Ottawa, Ontario, Canada For an understanding of insect evolution the structure of the wing base is of major significance. However, the fossil record o pteralia in extinct orders is extremely scanty. This paper is concerned with the wing bases of certain Paleozoic Paleoptera, namely, Palaeodictyop- tera, Megasecoptera and Diaphanopterodea rom the Upper Carboni- ferous (Namurian) of Czechoslovakia, the Upper Carboniferous (Stephanian) of France, and the Lower Permian of Czechoslovakia and Kansas. Independently of the Neoptera, the Diaphanopterodea acquired the ability to flex the wings backwards over the abdomen. In this respect, the order is of special interest, and an attempt is made here to compare the pteralia o the Diaphanopterodea with those of extant Ephemeroptera. Our present knowledge of the wing base in Paleozoic Paleoptera is restricted to the axillary plate o several palaeodictyopteran adults (Kukalova, 96o, 969-7o), and palaeodictyopteran nymphs (Woot- ton, 972; Sharov, 97I) [See figures , 2 and 4]. Recently, the wing base has been described in the Diaphanopterodea, Family E1- moidae (Kukalova-Peck, 974) (/]g. 8). In the present paper, the axillary plates in Martynoviidae and Asthenohymenidae o the Order Diaphanopterodea are included, and for the first time the axillary sclerites in Megasecoptera are described. The interpretation and terminology of the pteralia in extinct Pale- optera are necessarily dependent upon the detailed functional mor- phology of extant Ephemeroptera and Odonata. At the same time, the wing base structures found in extinct orders provide an evolu- tionary view and might be helpful in unraveling the enigmatic archi- *This research has been aided in part by a Publication Grant from Carleton University and in part by a National Science Foundation Grant, GB 39720, F. -
The Occurrence and Diversity of Coal Measure Insects
Journal of the Geological Sociev, London, Vol. 144, 1987, pp. 5W-511, 3 figs. Printed in Northern Ireland The occurrence and diversity of Coal Measure insects E. A. JARZEMBOWSKI Booth Museum of Natural Hktory, Dyke Road, Brighton BN1 5AA, UK Abslrnd Insects are generally considered to be rare in the Upper Carboniferous Coal Measures. However, recent work in the Westphalian D of SW England suggests that many have been overlooked in the past. This is because wings, which are the most characteristic insect fossils, may be mistaken for detached ‘fern’ pinnules, which are much more common. The resemblance may be functional convergence rather than leaf-mimicry. The earliest members of the class Insecta in the strict sense occur in the Upper Carboniferous. Eleven major divisions or orders are represented in the Coal Measures of which only four are still living. Primitively wingless insects (Archaeognatha) are present, relatives of familiar living insects such as the silverfish. There are numerous winged insects, some ofwhich could fold their wings (Neoptera) and others which could not (Palaeoptera). Palaeopterous insects were more diverse than today. They include three extinct orders (Palaeodictyoptera, Megasecoptera, Diaphanopterodea) which were probably plant suckers like present clay bugs. Other extinct palaeopterous insects (order Protodonata) were probably aerial predators like modem dragonflies, and included some of the largest insects of all time (‘giant dragonflies’). By far the most common neopterous insects were cockroaches (Blattodea) which outnumber all other insects in theUpper Carboniferous. This abundance is perhaps less surprising when one considers the general picture of the coal forests as warm, humid, and rich in organic matter. -
A New Interpretation of Dragonfly Wing Venation Based Upon Early Upper
A new interpretation of dragonfly wing venation based upon Early Upper Carboniferous fossils from Argentina (Insecta: Odonatoidea) and basic character states in pterygote wings EDGARF. RIEK 19 DufJL Street, Ainslie, Conberrcl, A .C.T.,2602, Austrcllia AND JARMILAKUKALOVA-PECK' Department of Geology, Carleton Universih, Ottc~wcl,Ont.. Cnnndo K IS 5B6 Received May 4. 1983 RIEK,E. F., and J. KUKALOVA-PECK.1984. A new interpretation of dragontly wing venation based upon Early Upper Carboniferous fossils from Argentina (Insecta: Odonatoidea) and basic character states in pterygote wings. Can. J. Zool. 62: 1150- 1166. The oldest known odonatoid wings are described from the Namurian of Argentina: Eugeropteron lunatum Riek n.g. et sp. and Geropteron arcuatum Riek n.g. and sp. (Meganisoptera: Meganeurina: Eugeropteridae n, fam.). The wings are gener- alized and support a reinterpretation of the venation of living Odonata as being fully homologous to that of other pterygotes and closely related to Ephemeropteroidea, but different from Neoptera. Therefore, Paleoptera is a valid phylogenetic unit, and Odonatoidea and Ephemeropteroidea are sister groups. RIEK.E. F.. et J. KUKALOVA-PECK.1984. A new interpretation of dragonfly wing venation based upon Early Upper Carboniferous fossils from Argentina (Insecta: Odonatoidea) and basic character states in pterygote wings. Can. J. Zool. 62: 1 150- 1 166. On trouvera ici la description des plus vieilles ailes odonatoi'des jamais rencontrees: il s'agit d'ailes d'Eugeropteron lunatum n. gen. et n. sp. et de Geropteron arcuatum n. gen. et n. sp. Riek (Meganisoptera: Meganeurina: Eugeropteridae n. fam.) provenant du Namurien d'Argentine. Les ailes suivent le plan de base et donnent lieu a une reinterpretation de la nervation des Odonates rkcentes selon laquelle les ailes des Odonates recentes seraient entierement homologues des ailes d'autres ptkrygotes, trks rapprochees des ailes d'Ephemeropteroidea, mais differentes des ailes de Neoptera. -
Fossil Insects Form of a Serpent; Which Then Pene- Trated Into the Earth, and Weaving a Frank M
the pioneer entomology by William Kirby and William Spcnce. "Were a naturalist to announce to the world," they write, "the discovery of an animal which first existed in the Fossil Insects form of a serpent; which then pene- trated into the earth, and weaving a Frank M. Carpenter shroud of pure silk of the finest texture, contracted itself within this covering into a body without external mouth or limbs, and resembling, more than any- Written in the rocks of Colorado, thing else, an Egyptian mummy; and Kansas, Oklahoma, and many other which, lastly after remaining in this places is the story of insects in the ages state without food and without mo- before man appeared on earth. tion . should at the end of that pe- The insects were trapped, caught in riod burst its silken cerements, struggle mud or sticky resin, and thereby left a through its earthly covering and start permanent record—as did dinosaur, into day a winged bird—what think mollusk, and plants—that broadens you would be the sensation excited by our knowledge of their evolution. this strange piece of intelligence ? After About 12,000 species of fossil insects the first doubts of 'its truth were dis- have been described. Countless thou- pelled, what astonishment would suc- sands of specimens have been collected. ceed! Amongst the learned, what sur- Fossil insects are not found in as mises!—what investigations! Even the many deposits or localities as most most torpid would flock to the sight of other invertebrates. Like other organ- such a prodigy." isms, insects are preserved as fossils by a sequence of events that results in EDWIN WAY TEALE is a past presi- their burial in a suitable medium. -
What Serial Homologs Can Tell Us About the Origin
F1000Research 2017, 6(F1000 Faculty Rev):268 Last updated: 17 JUL 2019 REVIEW What serial homologs can tell us about the origin of insect wings [version 1; peer review: 2 approved] Yoshinori Tomoyasu 1*, Takahiro Ohde2,3*, Courtney Clark-Hachtel1* 1Department of Biology, Miami University, Pearson Hall, 700E High Street, Oxford, OH 45056, USA 2Division of Evolutionary Developmental Biology, National Institute for Basic Biology, 38 Nishigonaka Myodaiji, Okazaki 444-8585, Japan 3Department of Basic Biology, School of Life Science, SOKENDAI (The Graduate University for Advanced Studies), 38 Nishigonaka Myodaiji, Okazaki 444-8585, Japan * Equal contributors First published: 14 Mar 2017, 6(F1000 Faculty Rev):268 ( Open Peer Review v1 https://doi.org/10.12688/f1000research.10285.1) Latest published: 14 Mar 2017, 6(F1000 Faculty Rev):268 ( https://doi.org/10.12688/f1000research.10285.1) Reviewer Status Abstract Invited Reviewers Although the insect wing is a textbook example of morphological novelty, 1 2 the origin of insect wings remains a mystery and is regarded as a chief conundrum in biology. Centuries of debates have culminated into two version 1 prominent hypotheses: the tergal origin hypothesis and the pleural origin published hypothesis. However, between these two hypotheses, there is little 14 Mar 2017 consensus in regard to the origin tissue of the wing as well as the evolutionary route from the origin tissue to the functional flight device. Recent evolutionary developmental (evo-devo) studies have shed new light F1000 Faculty Reviews are written by members of on the origin of insect wings. A key concept in these studies is “serial the prestigious F1000 Faculty. -
INSECT WING from ROAD GAP Donald R
71 INSECT WING FROM ROAD GAP Donald R. Chesnut Kentucky Geological Survey James R. Jennings Eastern Kentucky University In the course of collecting fossil plants within the insects and had two pairs of wings which could not be lower part of the Whitesburg coal zone at Road Gap, folded back across the abdomen when resting. Kentucky, a fossil insect wing was found. Insect wings Some of the generically diagnostic features are not are quite rare and few are known from the Lower discernible on our specimen, but the venation that is Pennsylvanian. This is the first Pennsylvanian insect preserved is different from any of the three species of wing reported from Kentucky. the family described from North America (Carpenter The lower part of the Whitesburg coal zone (Breathitt and Richardson, 19711. These species are Homaloneura Formation, Morrowan, Westphalian B) at this stop is dabasinskasi, Mcluckiepteron luciae, and Spilaptera composed of several thin coal beds within a series of americana, all from the Francis Creek Shale (Middle channel-fill shales, siltstones. and sandstones (see Plate Pennsylvanian) in Illinois. This specimen is thus the 4; in pocket). The two lowermost coals were cut-out by oldest known representative of the family in North subsequent channel erosion at the eastern end of the America and may belong to an undescribed genus (a roadcut. A third coal occurs within the channel-fill sedi- more detailed report is planned). ments and dips down into the channel. A coarsening- Of the three described species of the family, Car- upward (in part) sequence overlying the third coal con- penter and Richardson 119711 report only one, sists of silty shale and siltstone, grading (in part) into Homaloneura dabasinskasi, which has preserved mouth sandstone.