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Fig. Ap. 2.1. Denton Tending His Fairy Shrimp Collection
Fig. Ap. 2.1. Denton tending his fairy shrimp collection. 176 Appendix 1 Hatching and Rearing Back in the bowels of this book we noted that However, salts may leach from soils to ultimately if one takes dry soil samples from a pool basin, make the water salty, a situation which commonly preferably at its deepest point, one can then "just turns off hatching. Tap water is usually unsatis- add water and stir". In a day or two nauplii ap- factory, either because it has high TDS, or because pear if their cysts are present. O.K., so they won't it contains chlorine or chloramine, disinfectants always appear, but you get the idea. which may inhibit hatching or kill emerging If your desire is to hatch and rear fairy nauplii. shrimps the hi-tech way, you should get some As you have read time and again in Chapter 5, guidance from Brendonck et al. (1990) and temperature is an important environmental cue for Maeda-Martinez et al. (1995c). If you merely coaxing larvae from their dormant state. You can want to see what an anostracan is like, buy some guess what temperatures might need to be ap- Artemia cysts at the local aquarium shop and fol- proximated given the sample's origin. Try incu- low directions on the container. Should you wish bation at about 3-5°C if it came from the moun- to find out what's in your favorite pool, or gather tains or high desert. If from California grass- together sufficient animals for a study of behavior lands, 10° is a good level at which to start. -
Phylogenetic Analysis of Anostracans (Branchiopoda: Anostraca) Inferred from Nuclear 18S Ribosomal DNA (18S Rdna) Sequences
MOLECULAR PHYLOGENETICS AND EVOLUTION Molecular Phylogenetics and Evolution 25 (2002) 535–544 www.academicpress.com Phylogenetic analysis of anostracans (Branchiopoda: Anostraca) inferred from nuclear 18S ribosomal DNA (18S rDNA) sequences Peter H.H. Weekers,a,* Gopal Murugan,a,1 Jacques R. Vanfleteren,a Denton Belk,b and Henri J. Dumonta a Department of Biology, Ghent University, Ledeganckstraat 35, B-9000 Ghent, Belgium b Biology Department, Our Lady of the Lake University of San Antonio, San Antonio, TX 78207, USA Received 20 February 2001; received in revised form 18 June 2002 Abstract The nuclear small subunit ribosomal DNA (18S rDNA) of 27 anostracans (Branchiopoda: Anostraca) belonging to 14 genera and eight out of nine traditionally recognized families has been sequenced and used for phylogenetic analysis. The 18S rDNA phylogeny shows that the anostracans are monophyletic. The taxa under examination form two clades of subordinal level and eight clades of family level. Two families the Polyartemiidae and Linderiellidae are suppressed and merged with the Chirocephalidae, of which together they form a subfamily. In contrast, the Parartemiinae are removed from the Branchipodidae, raised to family level (Parartemiidae) and cluster as a sister group to the Artemiidae in a clade defined here as the Artemiina (new suborder). A number of morphological traits support this new suborder. The Branchipodidae are separated into two families, the Branchipodidae and Ta- nymastigidae (new family). The relationship between Dendrocephalus and Thamnocephalus requires further study and needs the addition of Branchinella sequences to decide whether the Thamnocephalidae are monophyletic. Surprisingly, Polyartemiella hazeni and Polyartemia forcipata (‘‘Family’’ Polyartemiidae), with 17 and 19 thoracic segments and pairs of trunk limb as opposed to all other anostracans with only 11 pairs, do not cluster but are separated by Linderiella santarosae (‘‘Family’’ Linderiellidae), which has 11 pairs of trunk limbs. -
Ordinal-Level Phylogenomics of the Arthropod Class
Ordinal-Level Phylogenomics of the Arthropod Class Diplopoda (Millipedes) Based on an Analysis of 221 Nuclear Protein-Coding Loci Generated Using Next- Generation Sequence Analyses Michael S. Brewer1,2*, Jason E. Bond3 1 Department of Environmental Science, Policy, and Management, University of California Berkeley, Berkeley, California, United States of America, 2 Department of Biology, East Carolina University, Greenville, North Carolina, United States of America, 3 Department of Biological Sciences and Auburn University Museum of Natural History, Auburn University, Auburn, Alabama, United States of America Abstract Background: The ancient and diverse, yet understudied arthropod class Diplopoda, the millipedes, has a muddled taxonomic history. Despite having a cosmopolitan distribution and a number of unique and interesting characteristics, the group has received relatively little attention; interest in millipede systematics is low compared to taxa of comparable diversity. The existing classification of the group comprises 16 orders. Past attempts to reconstruct millipede phylogenies have suffered from a paucity of characters and included too few taxa to confidently resolve relationships and make formal nomenclatural changes. Herein, we reconstruct an ordinal-level phylogeny for the class Diplopoda using the largest character set ever assembled for the group. Methods: Transcriptomic sequences were obtained from exemplar taxa representing much of the diversity of millipede orders using second-generation (i.e., next-generation or high-throughput) sequencing. These data were subject to rigorous orthology selection and phylogenetic dataset optimization and then used to reconstruct phylogenies employing Bayesian inference and maximum likelihood optimality criteria. Ancestral reconstructions of sperm transfer appendage development (gonopods), presence of lateral defense secretion pores (ozopores), and presence of spinnerets were considered. -
Keys to the Australian Clam Shrimps (Crustacea: Branchiopoda: Laevicaudata, Spinicaudata, Cyclestherida)
Museum Victoria Science Reports 20: 1-25 (2018) ISSN 1833-0290 https://museumsvictoria.com.au/collections-research/journals/museum-victoria-science-reports/ https://doi.org/10.24199/j.mvsr.2018.20 Keys to the Australian clam shrimps (Crustacea: Branchiopoda: Laevicaudata, Spinicaudata, Cyclestherida) Brian V. Timms Honorary Research Associate, Australian Museum, 1 William Street, Sydney 2001; and Centre for Ecosystem Science, School of Biology, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052 Brian V. Timms. 2018. Keys to the Australian clam shrimps (Crustacea: Branchiopoda: Laevicau- data, Spinicaudata, Cyclestherida). Museum Victoria Science Reports 20: 1-25. Abstract The morphology and systematics of clam shrimps is described followed by a key to genera. Each genus is treated, including diagnostic features, list of species with distributions, and references provided to papers with keys or if these are not available preliminary keys to species within that genus are included. Keywords gnammas, freshwater, crustaceans, morphology Figure 1: Limnadopsis birchii – Worlds largest clam shrimp. Keys to the Australian clam shrimps Introduction Australia has a diverse clam shrimp fauna with about 78 species in nine genera recognised in 2017 (Rogers et al., 2012; Timms, 2012, 2013; Schwentner et al., 2012a,b, 2013a,b, 2015b,a; Timms & Schwentner, 2017; Tippelt & Schwent- ner, 2018) . This is an explosion from 26 species in 2008 (Richter & Timms, 2005; Brendonck et al., 2008) when Australia‘s proportion of the world fauna was about 15%; now it is about 30%. It is anticipated another five species will be described before 2020. There have been two periods of active re- search on Australian clam shrimps, the first Figure 2: Number of known species of Aus- from 1855 to 1927 with a peak around the turn tralian clam shrimps over time. -
Artemia Franciscana C
1 Artemia franciscana C. Drewes (updated, 2002) http://www.zool.iastate.edu/~c_drewes/ http://www.zool.iastate.edu/~c_drewes/Artemph.jpg Taxonomy Phylum: Arthropoda Subphylum): Crustacea Class: Branchiopoda (includes fairy shrimp, brine shrimp, daphnia, clam shrimp, tadpole shrimp) Order: Anostraca (brine shrimp and fairy shrimp) Genus and species: Artemia franciscana (= the North American version of Artemia salina) [Note: The species commonly referred to as “Artemia salina” in much research and educational literature appears, in fact, to consist of several closely related species or subspecies. One of these, Artemia franciscana, is the main North American species.] Reproduction Typically, sexes are separate and adults are sexually dimorphic. Males have large graspers (modified second antennae) which easily distinguish them from females. In some species and populations of Artemia (for example, Europe), males may be rare and females reproduce by parthenogenesis. During mating, males deposit sperm in the female ovisac where eggs are fertilized and covered with a shell. Eggs are then deposited and stored in a brood sac near the posterior end of the thorax (Figure 1M). Once fertilized, eggs quickly undergo cleavage and development through the gastrula stage (Figure 1A-E). After one or a few days, eggs are then released by the female (oviposition). Multiple batches of eggs may be released at intervals of every few days by the same female. Two types of eggs may be laid -- (1) thin-shelled “summer eggs” that continue developing and hatch quickly, or (2) thick-shelled, brown “winter eggs” in which development is arrested at about early gastrula stage. Such “winter eggs,” in their dried and encysted form, survive in a metabolically inactive state (termed anabiosis) for up to 10 or more years while still retaining the ability to survive severe environmental conditions. -
First Observation of Triops (Crustacea: Branchiopoda: Notostraca) in the Natural Park of the Serra D’Irta (Peníscola, El Baix Maestrat)
Vol.NEMUS 3 2013 101 First observation of Triops (Crustacea: Branchiopoda: Notostraca) in the Natural Park of the Serra d’Irta (Peníscola, el Baix Maestrat). Enric Forner i Valls1 & James Edward Brewster First record of the tadpole shrimp Triops sp. in the Natural Park of the serra d’Irta (Peníscola, el Baix Maestrat). Key words: Notostraca, Triops, living fossil, temporary pond, biodiversity conservation, serra d’Irta, Peníscola, Ibe- rian Peninsula. Primera observació de Triops (Crustacea: Branchiopoda: Notostraca) al Parc Natural de la Serra d’Irta (Peníscola, el Baix Maestrat). Es documenta per primera vegada la presència de Triops sp. (família Triopidae) al Parc Natural de la serra d’Irta (Peníscola, el Baix Maestrat). Mots clau: Notostraca, Triops, fòssil vivent, ambients aquàtics temporanis, conservació de la biodivesitat, serra d’Irta, Peníscola, península ibèrica. Introduction The order Notostraca, branquiòpodes crustaceans con- reproduction (Machado et al., 1999; Boix et al., 2002; sists of a large current distribution in North America, Zierold et al. 2007) while in Northern Europe there is Eurasia, Africa and Australia, perhaps this is because asexual, hermaphroditism and parthenogenesis. of its old origin (Ombretta et al., 2005). The genus Triops has never been documented until now in the Nat- Triops Schrank 1803 has been quoted from the Trias- ural Park of the Serra d’Irta or in the Baix Maestrat. The sic (Guthörl, 1934; Trusheim, 1938; Tröger et al., 1984; records are from Ulldecona (Boix, 2002), Ares del Mae- Wallossek, 1993; Kelber, 1998, 1999) or the late Permian stre (Zierold et al. 2007) and the Ebro Delta (Alonso, (Gand et al., 1997). -
The Brain of the Remipedia (Crustacea) and an Alternative Hypothesis on Their Phylogenetic Relationships
The brain of the Remipedia (Crustacea) and an alternative hypothesis on their phylogenetic relationships Martin Fanenbruck*†, Steffen Harzsch†‡§, and Johann Wolfgang Wa¨ gele* *Fakulta¨t Biologie, Ruhr-Universita¨t Bochum, Lehrstuhl fu¨r Spezielle Zoologie, 44780 Bochum, Germany; and ‡Sektion Biosystematische Dokumentation and Abteilung Neurobiologie, Universita¨t Ulm, D-89081 Ulm, Germany Edited by May R. Berenbaum, University of Illinois at Urbana–Champaign, Urbana, IL, and approved December 16, 2003 (received for review September 26, 2003) Remipedia are rare and ancient mandibulate arthropods inhabiting ical study and reconstruction of the brain anatomy of Godzil- almost inaccessible submerged cave systems. Their phylogenetic liognomus frondosus Yager, 1989, (Remipedia, Godzilliidae) position is still enigmatic and the subject of extremely controver- from the Grand Bahama Island (12) followed by a discussion of sial debates. To contribute arguments to this discussion, we ana- ecological and phylogenetic implications. lyzed the brain of Godzilliognomus frondosus Yager, 1989 (Remi- pedia, Godzilliidae) and provide a detailed 3D reconstruction of its Methods anatomy. This reconstruction yielded the surprising finding that in The cephalothorax of a formalin-fixed Godzilliognomus frondo- comparison with the brain of other crustaceans such as represen- sus Yager, 1989, (Remipedia, Godzilliidae) specimen was em- tatives of the Branchiopoda and Maxillopoda the brain of G. bedded in Unicryl (British Biocell International, Cardiff, U.K.). frondosus is highly organized and well differentiated. It is matched Slices of 2.5 m were sectioned by using a Reichert-Jung in complexity only by the brain of ‘‘higher’’ crustaceans (Malacos- 2050-supercut. After toluidine-blue staining, digital images were traca) and Hexapoda. -
Updated Checklist and Distribution of Large Branchiopods (Branchiopoda: Anostraca, Notostraca, Spinicaudata) in Tunisia
Biogeographia – The Journal of Integrative Biogeography 31 (2016): 27–53 Updated checklist and distribution of large branchiopods (Branchiopoda: Anostraca, Notostraca, Spinicaudata) in Tunisia FEDERICO MARRONE1,*, MICHAEL KORN2, FABIO STOCH3, LUIGI NASELLI- FLORES1, SOUAD TURKI4 1 Dept. STEBICEF, University of Palermo, via Archirafi, 18, I-90123 Palermo, Italy 2 Limnological Institute, University of Konstanz, Mainaustr. 252, D-78464 Konstanz & DNA-Laboratory, Museum of Zoology, Senckenberg Natural History Collections Dresden, Königsbrücker Landstrasse 159, D- 01109 Dresden, Germany 3 Dept. of Life, Health & Environmental Sciences, University of L’Aquila, Via Vetoio, I-67100 Coppito, L'Aquila, Italy 4 Institut National des Sciences et Technologies de la Mer, Rue du 02 mars 1934, 28, T-2025 Salammbô, Tunisia * e-mail corresponding author: [email protected] Keywords: Branchinectella media, fauna of Maghreb, freshwater crustaceans, Mediterranean temporary ponds, regional biodiversity. SUMMARY Temporary ponds are the most peculiar and representative water bodies in the arid and semi-arid regions of the world, where they often represent diversity hotspots that greatly contribute to the regional biodiversity. Being indissolubly linked to these ecosystems, the so-called “large branchiopods” are unanimously considered flagship taxa of these habitats. Nonetheless, updated and detailed information on large branchiopod faunas is still missing in many countries or regions. Based on an extensive bibliographical review and field samplings, we provide an updated and commented checklist of large branchiopods in Tunisia, one of the less investigated countries of the Maghreb as far as inland water crustaceans are concerned. We carried out a field survey from 2004 to 2012, thereby collecting 262 crustacean samples from a total of 177 temporary water bodies scattered throughout the country. -
Branchiopoda: Cladocera) in Cenozoic Volcanogenic Lakes in Germany, with Discussion of Their Indicator Value
Palaeontologia Electronica palaeo-electronica.org Findings of Daphnia (Ctenodaphnia) Dybowski et Grochowski (Branchiopoda: Cladocera) in Cenozoic volcanogenic lakes in Germany, with discussion of their indicator value Alexey A. Kotov and Torsten Wappler ABSTRACT The goal of this paper is to describe fossil representatives of the Daphniidae Straus, 1820 (Eucrustacea: Cladocera) from German Cenozoic Maar lakes and lacus- trine sediments and discuss an indicator value of their ephippia for palaeoecological reconstructions. All females and ephippia (modified moulting exuvia of females con- taining resting eggs) from the late Early/early Middle Miocene Randeck Maar (about 17-15 m.y.a., mammal zone MN5) and ephippia from the Late Oligocene lacustrian locality Rott (23-24 m.y.a., mammal zome MP30) belong to Daphnia (Ctenodaphnia) Dybowski et Grochowski, 1895. We conclude that these cladocerans were very com- mon in European Eocene-Miocene water bodies. In case of German volcanogenic Maars, numerous ephippia of Daphnia (Ctenodaphnia), including their clusters, in a fossil layer could indicate shallow water conditions and seasonality in such water body. Alexey A. Kotov. A.N. Severtsov Institute of Ecology and Evolution, Leninsky Prospect 33, Moscow 119071, Russia. [email protected] Torsten Wappler. Steinmann Institute, Section Palaeontology, University of Bonn, Nussallee 8, 53115 Bonn, Germany. [email protected] Keywords: Eucrustacea, Cladocera, Tertiary, ephippia, Rott, Randeck Maar Submission: 17 February, 2015 Acceptance: 15 July 2015 INTRODUCTION ments, which are more likely to preserve trans- ported and time-averaged fossil assemblages Ancient Maar lakes and lacustrine sediments (Spicer, 1991; Wappler et al., 2009). Nevertheless, are of outstanding importance for the reconstruc- many of those Maar lakes are famous Cenozoic tion of continental palaeoecosystems with high-res- “fossillagerstätten” with well-preserved fossils of olution unique data for palaeoecological and different ages: from Eocene, e.g., Messel (Lutz, palaeoclimatological research. -
Malacostracan Phylogeny and Evolution
ERIK DAHL Department of Zoology, Lund, Sweden MALACOSTRACAN PHYLOGENY AND EVOLUTION ABSTRACT Malacostracan ancestors were benthic-epibenthic. Evolution of ambulatory stenopodia prob- ably preceded specialization of natatory pleopods. This division of labor was the prere- quisite for the evolution of trunk tagmosis. It is concluded that the ancestral malacostracan was probably more of a pre-eumalacostracan than a phyllocarid type, and that the phyllo- carids constitute an early branch adapted for benthic life. The same is the case with the hoplocarids, here regarded as a separate subclass with eumalacostracan rather than phyllo- carid affinities, although that question remains open. The systematic concept Eumalaco- straca is here reserved for the subclass comprising the three caridoid superorders, Syncarida, Eucarida and Peracarida. The central caridoid apomorphy, proving the unity of caridoids, is the jumping escape reflex system, manifested in various aspects of caridoid morphology. The morphological evidence indicates that the Syncarida are close to a caridoid stem-group, and that the Eumalacostraca sensu stricto were derived from pre-syncarid ancestors. Ad- vanced hemipelagic-pelagic caridoids probably evolved independently within the Eucarida and Peracarida. 1 INTRODUCTION The differentiation of the major crustacean taxa must have taken place very early, pro- bably at least partly in the Precambrian (cf. Bergstrom 1980). Fronrthe Cambrian we have proof of the presence of branchiopods (Simonetta & Delle Cave 1980, Briggs 1976), ostra- -
Dating the Origin of the Major Lineages of Branchiopoda
Available online at www.sciencedirect.com ScienceDirect Palaeoworld 25 (2016) 303–317 Dating the origin of the major lineages of Branchiopoda a,∗ b a,∗ Xiao-Yan Sun , Xuhua Xia , Qun Yang a LPS, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China b Department of Biology, University of Ottawa, Ontario K1N 6N5, Canada Received 3 June 2014; received in revised form 30 October 2014; accepted 3 February 2015 Available online 14 February 2015 Abstract Despite the well-established phylogeny and good fossil record of branchiopods, a consistent macro-evolutionary timescale for the group remains elusive. This study focuses on the early branchiopod divergence dates where fossil record is extremely fragmentary or missing. On the basis of a large genomic dataset and carefully evaluated fossil calibration points, we assess the quality of the branchiopod fossil record by calibrating the tree against well-established first occurrences, providing paleontological estimates of divergence times and completeness of their fossil record. The maximum age constraints were set using a quantitative approach of Marshall (2008). We tested the alternative placements of Yicaris and Wujicaris in the referred arthropod tree via the likelihood checkpoints method. Divergence dates were calculated using Bayesian relaxed molecular clock and penalized likelihood methods. Our results show that the stem group of Branchiopoda is rooted in the late Neoproterozoic (563 ± 7 Ma); the crown-Branchiopoda diverged during middle Cambrian to Early Ordovician (478–512 Ma), likely representing the origin of the freshwater biota; the Phyllopoda clade diverged during Ordovician (448–480 Ma) and Diplostraca during Late Ordovician to early Silurian (430–457 Ma). -
The Arthropod Assemblage of the Upper Devonian Strud Locality and Its Ecology
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1245 The Arthropod Assemblage of the Upper Devonian Strud locality and its Ecology LINDA LAGEBRO ACTA UNIVERSITATIS UPSALIENSIS ISSN 1651-6214 ISBN 978-91-554-9222-9 UPPSALA urn:nbn:se:uu:diva-248153 2015 Dissertation presented at Uppsala University to be publicly examined in Axel Hambergsalen, Villavägen 16, Uppsala, Friday, 22 May 2015 at 13:15 for the degree of Doctor of Philosophy. The examination will be conducted in English. Faculty examiner: Professor Gerhard Scholtz (Humboldt Universität zu Berlin). Abstract Lagebro, L. 2015. The Arthropod Assemblage of the Upper Devonian Strud locality and its Ecology. Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1245. 41 pp. Uppsala: Acta Universitatis Upsaliensis. ISBN 978-91-554-9222-9. The Devonian (419-359 million years ago) is the geological period when the terrestrial biota fully established. Early representatives from a terrestrial and continental aquatic biota have previously been reported from the Upper Devonian (Famennian) Strud quarry in Belgium, in the shape of seed-bearing plants and vertebrates (fish and early tetrapods). The palaeoenvironment is interpreted as a floodplain with slow accumulation of sediment in the river channels and adjacent shallow pools, subject to seasonal flooding and desiccation. This thesis presents the upper Famennian Strud ecosystem with representatives from the largest animal phylum – the Arthropoda. Pancrustaceans are dominating the arthropod assemblage by two eumalacostracans (previously described), three groups of branchiopods, and a putative insect, all collected in fine shales likely deposited in the shallow pools.