Atmospheric Hypoxia Limits Selection for Large Body Size in Insects
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The Engineering of the Giant Dragonflies of the Permian: Revised Body Mass, Power, Air Supply, Thermoregulation and the Role of Air Density Alan E
© 2018. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2018) 221, jeb185405. doi:10.1242/jeb.185405 COMMENTARY The engineering of the giant dragonflies of the Permian: revised body mass, power, air supply, thermoregulation and the role of air density Alan E. R. Cannell ABSTRACT abdomen as well as spiny and surprisingly robust legs. Illustrations An engineering examination of allometric and analogical data on the of M. monyi and a female Meganeurula selysii (Shear and flight of giant Permian insects (Protodonata, Meganeura or griffinflies) Kukalova-Peck, 1990) also indicate creatures with strong mouth indicates that previous estimates of the body mass of these insects parts, well-developed pincers and strong long thick legs. In both are too low and that the largest of these insects (wingspan of 70 cm or drawings, the abdomen is similar in diameter to the thorax, unlike more) would have had a mass of 100–150 g, several times greater the structure of most modern dragonflies, which have much more – – than previously thought. Here, the power needed to generate lift and slender abdomens. This large size and consequently high mass fly at the speeds typical of modern large dragonflies is examined has attracted attention for over a hundred years as there are no extant together with the metabolic rate and subsequent heat generated by insects of this size and their physiology in terms of power generation the thoracic muscles. This evaluation agrees with previous work and thermoregulation is not understood. This Commentary suggesting that the larger specimens would rapidly overheat in the examines the questions of mass, power generation to fly and high ambient temperatures assumed in the Permian. -
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. -
PRISCUM the Newsletter of the Paleontological Society Volume 13, Number 2, Fall 2004
PRISCUM The Newsletter of the Paleontological Society Volume 13, Number 2, Fall 2004 Paleontological PRESIDENT’S Society Officers COLUMN: Inside... President Treasurer’s Report 2 William I. Ausich WE NEED YOU! GSA Information 2 President-Elect by William I. Ausich Reviews of PS- David Bottjer Sponsored Sessions 3 Past-President Why are you a member of The Paleontology Portal 5 Patricia H. Kelley The Paleontological Society? In PS Lecture Program 6 Secretary the not too distance past, the Books for Review 9 Roger D. K. Thomas only way to receive a copy of the Journal of Book Reviews 9 Treasurer Paleontology and Paleobiology was to pay your dues Conference Announce- and belong to the Society. I suppose one could Mark E. Patzkowsky have borrowed a copy from a friend or wander over ments 14 JP Managing Editors to the library. However, this was probably done Ann (Nancy) F. Budd with a heavy burden of guilt. Now, as we move Christopher A. Brochu into the digital age of scientific journal publishing, Jonathan Adrain one can have copies of the Journal of Paleontology and Paleobiology transmitted right to your Paleobiology Editors computer. It actually may arrive faster than the Tomasz Baumiller U.S. mail, you do not have to pay anything, and Robyn Burnham you do not even have to walk over to the library. Philip Gingerich No need for shelf space, no hassle, no dues, no Program Coordinator guilt – isn’t the Web great? The Web is great, but the Society needs dues-paying members in order Mark A. Wilson to continue to publish in paper, digitally, or both. -
Rasnitsynala Sigambrorum Gen. Et Sp. N., a Small Odonatopterid
A peer-reviewed open-access journal ZooKeys 130: 57–66 (2011)Rasnitsynala sigambrorum gen. et sp. n., a small odonatopterid... 57 doi: 10.3897/zookeys.130.1458 RESEARCH ARTICLE www.zookeys.org Launched to accelerate biodiversity research Rasnitsynala sigambrorum gen. et sp. n., a small odonatopterid (“Eomeganisoptera”, “Erasipteridae”) from the early Late Carboniferous of Hagen-Vorhalle (Germany) Wolfgang Zessin1,†, Carsten Brauckmann2,‡, Elke Gröning2,§ 1 Lange Straße 9, 19230 Jasnitz, Germany 2 Clausthal University of Technology, Institute of Geology and Paleontology, Leibnizstraße 10, 38678 Clausthal-Zellerfeld, Germany † urn:lsid:zoobank.org:author:EE854837-A2FB-457C-82F1-60406627EC58 ‡ urn:lsid:zoobank.org:author:A9B536B4-6DEF-48C4-980A-9EB8A9467F8B § urn:lsid:zoobank.org:author:6D085012-9A15-4937-B408-FEFDF39B4907 Corresponding author: Wolfgang Zessin ([email protected]) Academic editor: D. Shcherbakov | Received 2 May 2011 | Accepted 26 August 2011 | Published 24 September 2011 urn:lsid:zoobank.org:pub:708DBB4C-244E-4606-992B-D10129016158 Citation: Zessin W, Brauckmann C, Gröning E (2011) Rasnitsynala sigambrorum gen. et sp. n., a small odonatopterid (“Eomeganisoptera”, “Erasipteridae”) from the early Late Carboniferous of Hagen-Vorhalle (Germany). In: Shcherbakov DE, Engel MS, Sharkey MJ (Eds) Advances in the Systematics of Fossil and Modern Insects: Honouring Alexandr Rasnitsyn. ZooKeys 130: 57–66. doi: 10.3897/zookeys.130.1458 Abstract Besides Erasipteroides valentini (Brauckmann in Brauckmann, Koch & Kemper, 1985), Zessinella siope Brauckmann, 1988, and Namurotypus sippeli Brauckmann & Zessin, 1989, Rasnitsynala sigambrorum gen. et sp. n. is the fourth species of the Odonatoptera from the early Late Carboniferous (Early Penn- sylvanian: Namurian B, Marsdenian) deposits of the important Hagen-Vorhalle Konservat-Lagerstätte in Germany. -
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, -
Libro 34(1).Indb 115 19/12/2007 20:39:30 116 Nel Et Al
ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es /info/estratig/journal.htm Journal of Iberian Geology 34 (1) 2008: 115-122 The Odonatoptera of the Late Permian Lodève Basin (Insecta) Odonatoptera del Pérmico Superior de la Cuenca de Lòdeve (Insecta) A. N. Nel1*, G. Fleck1, R. Garrouste1, G. Gand2 1CNRS UMR 5202, Muséum National d’Histoire Naturelle, CP 50, Entomologie, 45 rue Buffon, F-75005, Paris, France e-mail: [email protected] 2 Laboratoire de Biogéosciences, CNRS, Université de Bourgogne, Centre des Sciences de la Terre; 6, boulevard Gabriel, F-21000 Dijon, France Received: 15/07/06 /Accepted: 27/12/06 Abstract The discovery of numerous and very diverse Odonatoptera in the Red Late Permian Lodève Basin questions its current recons- tructions of a dry to very dry palaeoclimate and palaeoenvironment. It rather suggests the presence of more or less permanent water bodies, surrounded by a diversity of terrestrial biotas. The discovery of large to very large Meganeuridae contradicts the alleged relations between the decrease of body and wing sizes of the insects during the late Permian as a direct consequence of the decrease of the oxygen atmospheric concentrations at that time. Keywords: Insecta, Odonatoptera, Late Permian, Lodève Basin, diversity, palaeoecology, gigatism, oxygen atmospheric concentrations. Resumen El descubrimiento de una numerosa y variada fauna de Odonatoptera en el Pérmico Superior rojo de la cuenca de Lodève pone en cuestión la hipótesis de un paleoclima seco a muy seco para este yacimiento. Sugiere la presencia de masas de agua más o menos permanentes, rodeadas por una importante diversidad de medios terrestres. -
Wielkie Ważki Paleozoiku. Dlaczego Były Tak Wielkie I Dlaczego Nie Ma Obecnie Podobnie Wielkich? the Large Dragonflies of the Palaeozoic
Odonatrix 16_4 (2020) Wielkie ważki paleozoiku. Dlaczego były tak wielkie i dlaczego nie ma obecnie podobnie wielkich? The large dragonflies of the Palaeozoic. Why were they so large and why do similar huge insects not exist nowadays? Edwin SIEREDZIŃSKI autor niezależny, ul. Górna 24, 26-600 Radom, mail: [email protected] Abstract The body sizes of recent insects are rather small; enormous body lengths or wingspans of several dozen cm are rare. For example, the largest contemporary damselfly Megaloprepus caerulatus has a wingspan of 19 cm. But during the Carboniferous and Permian periods, bigger “dragonflies” (griffenflies from the order Meganisoptera) did exist; with wingspans of over 70 cm, the Meganeuridae were the largest ever flying insects. To explain these great sizes, factors such as oxygen concentration and the evolutionary arms race between herbivorous and carnivorous insects have been invoked. However, these explanations do not go far enough, because many other factors have not been taken into consideration, for example, the evolution of higher verte- brates during the late Palaeozoic, and the morphological and physiological limitations of the in- sect body. These aspects will have been crucial to the existence of giant insects such as Meganeura and Meganeuropsis. Most probably, such large dragonflies and damselflies (as well as other insects) are no longer extant because the bodies of higher vertebrates are more efficient. Large insects simply lose out against small and medium-sized vertebrates, as demonstrated by the competition between the New Zealand weta and rodents (kiore and brown rat), and the ex- tinction of Labidura herculeana. Key Words. Palaeozoic, Odonata, dragonflies, size, Meganeura, palaeontology Wstęp Współczesne owady najczęściej kojarzą się ze zwierzętami o relatywnie niewielkich rozmiarach ciała. -
Odonatological Abstract Service
Odonatological Abstract Service published by the INTERNATIONAL DRAGONFLY FUND (IDF) in cooperation with the WORLDWIDE DRAGONFLY ASSOCIATION (WDA) Editors: Dr. Martin Lindeboom, Silberdistelweg 11, D-72113 Ammerbuch, Germany. Tel. ++49 (0)7073 300770; E-mail: [email protected] Dr. Klaus Reinhardt, Dept Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, UK. Tel. ++44 114 222 0105; E-mail: [email protected] Martin Schorr, Schulstr. 7B, D-54314 Zerf, Germany. Tel. ++49 (0)6587 1025; E-mail: [email protected] Published in Rheinfelden, Germany and printed in Trier, Germany. ISSN 1438-0269 1997 than 500 taxa below the family level were inventoried, and each listing includes relative frequency of en- 7574. He, J.-r.; Jiang B.-h.; Chen, T.-s. (1997): The counter, life stages collected, and dominant role in the aquatic insects of Rainbow Lake. Conservation Quar- greenleaf manzanita community. Specific host relation- terly, summer quarterly, June,1997,18: 37-41. (in Chi- ships are included for some predators and parasitoids. nese) [Rainbow Lake is an alpine Lake in Taiwan. The Herbivores, predators, and parasitoids comprised the paper provides brief information on Aeshna petalura majority (80 percent) of identified insects and related and Polycanthagyna erythromelas. (Abstract by Hao- taxa." (Authors) The list of Odonata includes the follow- miao Zhang)] ing taxa: Aeshna palmata, Anax junius, Cordulegaster dorsalis, Libellula sp., Pantala hymenea, Tarnetrum cor- 7575. Liebherr, J.K.; Polhemus, D.A. (1997): R.C.L. rupturn, Lestidae species undet., and Coenagrionidae Perkins: 100 years of Hawaiian entomology. Pacif. Sci. species undet..] Address: http://www.fs.fed.us/psw/pub- 51(4): 343-355, 1 pl. -
The Largest Known Odonate in China: Hsiufua Chaoi Zhang Et Wang, Gen
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Springer - Publisher Connector Article Geology May 2013 Vol.58 No.13: 15791584 doi: 10.1007/s11434-012-5567-3 The largest known odonate in China: Hsiufua chaoi Zhang et Wang, gen. et sp. nov. from the Middle Jurassic of Inner Mongolia ZHANG HaiChun1*, ZHENG DaRan1,2, WANG Bo1, FANG Yan1 & JARZEMBOWSKI Edmund A1 1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China; 2 Graduate University of the Chinese Academy of Sciences, Beijing 100049, China Received June 26, 2012; accepted October 19, 2012; published online November 27, 2012 A new genus and species, Hsiufua chaoi Zhang et Wang, is established based on a forewing from the Middle Jurassic Haifanggou Formation in Inner Mongolia, China and attributed to Campterophlebiidae, Isophlebioidea, Odonata. It is the largest odonate known in China and the fourth in the world in terms of forewing length. The maximum size (based on forewing length) of Odonata is smaller in the Permian than in the Mesozoic which is probably due to competition for prey between Odonata and Pro- todonata in the Permian. The reason that the maximum size of Jurassic odonates is larger than that of their extant relatives is most probably less competition and lower predation pressure from contemporary aerial vertebrates. Hsiufua chaoi Zhang et Wang, new genus and species, largest odonate, Middle Jurassic, China Citation: Zhang H C, Zheng D R, Wang B, et al. The largest known odonate in China: Hsiufua chaoi Zhang et Wang, gen. -
Flight Adaptations in Palaeozoic Palaeoptera (Insecta)
Biol. Rev. (2000), 75, pp. 129–167 Printed in the United Kingdom # Cambridge Philosophical Society 129 Flight adaptations in Palaeozoic Palaeoptera (Insecta) ROBIN J. WOOTTON" and JARMILA KUKALOVA! -PECK# " School of Biological Sciences, University of Exeter, Devon EX44PS, U.K. # Department of Earth Sciences, Carleton University, Ottawa, Ontario, Canada K1S 5B6 (Received 13 January 1999; revised 13 October 1999; accepted 13 October 1999) ABSTRACT The use of available morphological characters in the interpretation of the flight of insects known only as fossils is reviewed, and the principles are then applied to elucidating the flight performance and techniques of Palaeozoic palaeopterous insects. Wing-loadings and pterothorax mass\total mass ratios are estimated and aspect ratios and shape-descriptors are derived for a selection of species, and the functional significance of wing characters discussed. Carboniferous and Permian ephemeropteroids (‘mayflies’) show major differences from modern forms in morphology and presumed flight ability, whereas Palaeozoic odonatoids (‘dragonflies’) show early adaptation to aerial predation on a wide size-range of prey, closely paralleling modern dragonflies and damselflies in shape and wing design but lacking some performance-related structural refinements. The extensive adaptive radiation in form and flight technique in the haustellate orders Palaeodictyoptera, Megasecoptera, Diaphanopterodea and Permothemistida is examined and discussed in the context of Palaeozoic ecology. Key words: Wings, flight, Palaeozoic, -
Evolution of the Insects
CY501-PIND[733-756].qxd 2/17/05 2:10 AM Page 733 Quark07 Quark07:BOOKS:CY501-Grimaldi: 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, 270 Acherontia atropos, 585 -
Insect Evolution
Current Biology Magazine ABInsect evolution Michael S. Engel It goes without saying that insects epitomize diversity, and with over a million documented species they stand out as one of the most remarkable lineages in the 3.5-billion-year history of life on earth (Figure 1). This reality is passé to even the layperson and is taken for granted in the same way none of us think much of our breathing as we go about our day, and yet insects are just as vital to our existence. Insects 5 mm are simultaneously familiar and foreign to us, and while a small fraction are C beloved or reviled, most are simply ignored. These inexorable evolutionary overachievers outnumber us all, their segmented body plan is remarkably labile, they combine a capacity for high rates of speciation with low levels of natural extinction, and their history of successes eclipses those of the 10 cm more familiar ages of dinosaurs and mammals alike. It is their evolution — persisting over vast expanses of geological time and inextricably Figure 5. Animals from the early Ordovician Fezouata formations of Morocco. (A) The marrellomorph arthropod Furca (Natural History Museum of Toulouse, France, MHNT. implicated in the diversifi cation of other PAL.2007.39.80.1). (B) A concretion preserving the giant fi lter feeding anomalocaridid Aegirocassis lineages — that stands as one of the benmoulai (Yale Peabody Museum YPM 237172). (C) Reconstruction of Aegirocassis benmoulai most expansive subjects in biology. © Marianne Collins. (Images reprinted by permission from Macmillan Publishers Ltd: Nature (Van Insects comprise the more diverse Roy et al., 2010 and 2015), copyright 2010 and 2015.) of two classes united together as the arthropod subphylum Hexapoda, the other being the Entognatha, consisting FURTHER READING Ma, X., Hou, X., Edgecombe, G.D., and Strausfeld, N.J.