Chordates the Voyage to Us Bones, Brawn and Brains
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
An Observation of Two Oceanic Salp Swarms in the Tasman Sea: Thetys Vagina and Cyclosalpa Affinis Natasha Henschke1,2,3*, Jason D
Henschke et al. Marine Biodiversity Records (2016) 9:21 DOI 10.1186/s41200-016-0023-8 MARINE RECORD Open Access An observation of two oceanic salp swarms in the Tasman Sea: Thetys vagina and Cyclosalpa affinis Natasha Henschke1,2,3*, Jason D. Everett1,2,3 and Iain M. Suthers1,2,3 Abstract Background: Large oceanic salps are rarely encountered. The highest recorded biomasses of the salps Thetys vagina (852 g WW m−3)andCyclosalpa affinis (1149 g WW m−3) were observed in the Tasman Sea during January 2009. Results: Due to their fast sinking rates the carcasses and faecal pellets of these and other large salps play a significant role in carbon transport to the seafloor. We calculated that faecal pellets from these swarms could have contributed up to 67 % of the mean organic daily carbon flux in the area. This suggests that the flux of carbon from salp swarms are not accurately captured in current estimates. Conclusion: This study contributes information on salp abundance and biomass to a relatively understudied field, improving estimates for biogeochemical cycles. Background (Henschke et al., 2013) can increase the carbon flux in an The role of gelatinous zooplankton, such as salps, pyro- area up to ten-fold the daily average (Fischer et al., 1988) somes and cnidarians, in ocean food webs and biogeo- for a sustained period of time (Smith et al. 2014). chemical cycling has garnered increased attention in Due to their regular occurrence (Henschke et al., recent years (Lebrato et al., 2011; Henschke et al., 2013; 2014) and coastal dominance (Henschke et al 2011), Lebrato et al., 2013; Smith et al. -
Lates Niloticus) Ecological Risk Screening Summary
U.S. Fish and Wildlife Service Nile Perch (Lates niloticus) Ecological Risk Screening Summary Web Version – September 2014 Photo: © Biopix: N Sloth 1 Native Range, and Status in the United States Native Range From Schofield (2011): “Much of central, western and eastern Africa: Nile River (below Murchison Falls), as well as the Congo, Niger, Volga, Senegal rivers and lakes Chad and Turkana (Greenwood 1966 [cited by Schofield (2011) but not accessed for this report]). Also present in the brackish Lake Mariot near Alexandria, Egypt.” Lates niloticus Ecological Risk Screening Summary U.S. Fish and Wildlife Service – Web Version - 8/14/2012 Status in the United States From Schofield (2011): “Scientists from Texas traveled to Tanzania in 1974-1975 to investigate the introduction potential of Lates spp. into Texas reservoirs (Thompson et al. 1977 [cited by Schofield (2011) but not accessed for this report]). Temperature tolerance and trophic dynamics were studied for three species (L. angustifrons, L. microlepis and L. mariae). Subsequently, several individuals of these three species were shipped to Heart of the Hills Research Station (HOHRS) in Ingram, Texas in 1975 (Rutledge and Lyons 1976 [cited by Schofield (2011) but not accessed for this report]). Also in 1975, Nile perch (L. niloticus) were transferred from Lake Turkana, Kenya, to HOHRS. All fishes were held in indoor, closed-circulating systems (Rutledge and Lyons 1976).” “From 1978 to 1985, Lates spp. was released into various Texas reservoirs (Howells and Garrett 1992 [cited by Schofield (2011) but not accessed for this report]). Almost 70,000 Lates spp. larvae were stocked into Victor Braunig (Bexar Co.), Coleto Creek (Goliad Co.) and Fairfield (Freestone Co.) reservoirs between 1978 and 1984. -
Salp Contributions to Vertical Carbon Flux in the Sargasso Sea
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by College of William & Mary: W&M Publish W&M ScholarWorks VIMS Articles Virginia Institute of Marine Science 2016 Salp contributions to vertical carbon flux in the Sargasso Sea JP Stone Virginia Institute of Marine Science Deborah K. Steinberg Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/vimsarticles Part of the Aquaculture and Fisheries Commons Recommended Citation Stone, JP and Steinberg, Deborah K., "Salp contributions to vertical carbon flux in the Sargasso Sea" (2016). VIMS Articles. 797. https://scholarworks.wm.edu/vimsarticles/797 This Article is brought to you for free and open access by the Virginia Institute of Marine Science at W&M ScholarWorks. It has been accepted for inclusion in VIMS Articles by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. 1 Salp contributions to vertical carbon flux in the Sargasso 2 Sea 3 4 5 Joshua P. Stonea,*, Deborah K. Steinberga 6 a Department of Biological Sciences, Virginia Institute of Marine Science, College of William & Mary, 7 PO Box 1346, Gloucester Point, VA 23062, USA 8 * Corresponding author. 9 E-mail addresses: [email protected] (J. Stone), [email protected] (D. Steinberg) 10 11 1 © 2016. This manuscript version is made available under the Elsevier user license http://www.elsevier.com/open-access/userlicense/1.0/ 12 Abstract 13 We developed a one-dimensional model to estimate salp contributions to vertical carbon flux at the 14 Bermuda Atlantic Time-series Study (BATS) site in the North Atlantic subtropical gyre for a 17-yr period 15 (April 1994 to December 2011). -
Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
The Origins of Chordate Larvae Donald I Williamson* Marine Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom
lopmen ve ta e l B Williamson, Cell Dev Biol 2012, 1:1 D io & l l o l g DOI: 10.4172/2168-9296.1000101 e y C Cell & Developmental Biology ISSN: 2168-9296 Research Article Open Access The Origins of Chordate Larvae Donald I Williamson* Marine Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom Abstract The larval transfer hypothesis states that larvae originated as adults in other taxa and their genomes were transferred by hybridization. It contests the view that larvae and corresponding adults evolved from common ancestors. The present paper reviews the life histories of chordates, and it interprets them in terms of the larval transfer hypothesis. It is the first paper to apply the hypothesis to craniates. I claim that the larvae of tunicates were acquired from adult larvaceans, the larvae of lampreys from adult cephalochordates, the larvae of lungfishes from adult craniate tadpoles, and the larvae of ray-finned fishes from other ray-finned fishes in different families. The occurrence of larvae in some fishes and their absence in others is correlated with reproductive behavior. Adult amphibians evolved from adult fishes, but larval amphibians did not evolve from either adult or larval fishes. I submit that [1] early amphibians had no larvae and that several families of urodeles and one subfamily of anurans have retained direct development, [2] the tadpole larvae of anurans and urodeles were acquired separately from different Mesozoic adult tadpoles, and [3] the post-tadpole larvae of salamanders were acquired from adults of other urodeles. Reptiles, birds and mammals probably evolved from amphibians that never acquired larvae. -
Towards an Understanding of Salp Swarm Dynamics. ICES CM 2002/N
CM 2002/ N:12 Towards an understanding of salp swarm dynamics by Patricia Kremer ABSTRACT Species of salps are characterized by intermittent blooms. Several studies have documented the importance of physical processes both in providing seed stocks of salps and creating an environment that is favorable for the rapid increase of salp populations. Although salps are typically oceanic, most observations of bloom dynamics have been made in more accessible inshore waters, so it is difficult to assess how frequent and widespread these swarms are. A review and comparison of existing data is helping to define geographic “hot spots” for salp blooms as well as the necessary physical and biological precursors. Although at this point, the review is far from complete, several generalities are emerging. The details of the physical forcing functions vary, but the overall physical regime seems to require a region of pulsed mixing of oceanic water that results in a relatively high standing stock of autotrophs. For a salp bloom to occur, there also needs to be an adequate seed population of salps and sufficient sustained primary production to support the biomass of the salp population as the bloom develops. As non-selective filter feeders, salps are able to remove a wide range of particulates from the water column, transforming the undigested portion into fast sinking feces. Therefore, when salps occur at high densities, the water is characterized by low abundance of other plankton, with obvious trophic implications. Patricia Kremer: Marine Sciences, University of Connecticut, Groton CT 06340-6097, USA [tel: +1 860 405 9140; fax: +1 860 405 9153; e-mail [email protected]] INTRODUCTION Salps are holoplanktonic grazers that have a life history, feeding biology, and population dynamics that contrasts sharply to copepods and other crustacean zooplankton (Madin and Deibel 1998). -
Curious Creatures Using Fossil and Modern Evidence to Work out the Lifestyles of Extinct Animals
Earthlearningidea http://www.earthlearningidea.com Curious creatures Using fossil and modern evidence to work out the lifestyles of extinct animals Try comparing the features of animals today with • Of what animal(s) alive today does it remind you? those of fossils - can you predict the lifestyles of the • How did the animal move? (swim, crawl, float, extinct animals? wriggle, hop). • How did it catch its food? (predators often have Divide the pupils into groups. Give each group a copy grasping limbs for catching prey. Not all animals of the diagrams of animals shown below and a copy are herbivores or carnivores; some are filter of the reconstruction of life on page 3. Tell the pupils feeders (like mussels) or deposit feeders (like that all of these creatures lived in the sea about 515 worms). million years ago before there were any plants or • Could it see? (predators often have large eyes for animals on land. hunting). (Further background information is given for teachers • Is there evidence of other organs that could sense on page 2). the environment around? (feelers). • Look at the diagram on page 3. Where do you For each of the five animals shown in the diagram, think it lived? (swimming around, on the seabed, ask the pupils to answer the following questions and burrowing, on another animal or plant). to list the evidence they have used:- • Can you deduce anything else about the lifestyles of these five animals? Images reproduced with kind permission of The Burgess Shale Geoscience Foundation http://www.burgess-shale.bc.ca ……………………………………………………………………………………………………………………………………. The back up: Title: Curious creatures Time needed to complete activity: 20 minutes Subtitle: Using fossil and modern evidence to work Pupil learning outcomes: Pupils can: out the lifestyles of extinct animals • relate characteristics of marine animals today to similar characteristics shown by fossil evidence Topic: A snapshot of the history of life on Earth from long-extinct creatures; • realise that there are no right answers to this Age range of pupils: 10 - 18 years activity. -
Monophyly and Interrelationships of Snook and Barramundi (Centropomidae Sensu Greenwood) and five New Markers for fish Phylogenetics ⇑ Chenhong Li A, , Betancur-R
Molecular Phylogenetics and Evolution 60 (2011) 463–471 Contents lists available at ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev Monophyly and interrelationships of Snook and Barramundi (Centropomidae sensu Greenwood) and five new markers for fish phylogenetics ⇑ Chenhong Li a, , Betancur-R. Ricardo b, Wm. Leo Smith c, Guillermo Ortí b a School of Biological Sciences, University of Nebraska, Lincoln, NE 68588-0118, USA b Department of Biological Sciences, The George Washington University, Washington, DC 200052, USA c The Field Museum, Department of Zoology, Fishes, 1400 South Lake Shore Drive, Chicago, IL 60605, USA article info abstract Article history: Centropomidae as defined by Greenwood (1976) is composed of three genera: Centropomus, Lates, and Received 24 January 2011 Psammoperca. But composition and monophyly of this family have been challenged in subsequent Revised 3 May 2011 morphological studies. In some classifications, Ambassis, Siniperca and Glaucosoma were added to the Accepted 5 May 2011 Centropomidae. In other studies, Lates + Psammoperca were excluded, restricting the family to Available online 12 May 2011 Centropomus. Recent analyses of DNA sequences did not solve the controversy, mainly due to limited taxonomic or character sampling. The present study is based on DNA sequence data from thirteen Keywords: genes (one mitochondrial and twelve nuclear markers) for 57 taxa, representative of all relevant Centropomidae species. Five of the nuclear markers are new for fish phylogenetic studies. The monophyly of Centrop- Lates Psammoperca omidae sensu Greenwood was supported by both maximum likelihood and Bayesian analyses of a Ambassidae concatenated data set (12,888 bp aligned). No support was found for previous morphological hypothe- Niphon spinosus ses suggesting that ambassids are closely allied to the Centropomidae. -
Description of Two New Species of Sea Bass (Teleostei: Latidae: Lates) from Myanmar and Sri Lanka
Zootaxa 3314: 1–16 (2012) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2012 · Magnolia Press ISSN 1175-5334 (online edition) Description of two new species of sea bass (Teleostei: Latidae: Lates) from Myanmar and Sri Lanka ROHAN PETHIYAGODA1 & ANTHONY C. GILL1,2 1Australian Museum, 6 College Street, Sydney NSW 2010, Australia. E-mail: [email protected] 2Macleay Museum and School of Biological Sciences, Macleay Building A12, University of Sydney, Sydney NSW 2006, Australia. E-mail: [email protected] Abstract Two new species of Lates Cuvier are described. Lates lakdiva, new species, from western Sri Lanka, differs from its Indo- Pacific congeners by its lesser body depth, 26.6‒27.6% SL; 5 rows of scales in transverse line between base of third dorsal- fin spine and lateral line; 31‒34 serrae on the posterior edge of the preoperculum; third anal-fin spine longer than second; 47‒52 lateral-line scales on body; and greatest depth of maxilla less than eye diameter. Lates uwisara, new species, from eastern Myanmar, is distinguished by possessing 7 scales in transverse line between base of third dorsal-fin spine and lat- eral line; eye diameter 4.4‒4.7% SL; body depth 28.4‒34.5% SL; and third anal-fin spine shorter than the second. Despite substantial genetic variation, L. calcarifer sensu lato is widely distributed, from tropical Australia through Indonesia, Sin- gapore and Thailand, westwards to at least the west coast of India. Caution is urged in translocating Lates in the Indo- Pacific region as other yet unrecognized species likely exist. -
Biomass of Zooplankton and Micronekton in the Southern Bluefin Tuna Fishing Grounds Off Eastern Tasmania, Australia
-- MARINE ECOLOGY PROGRESS SERIES Vol. 138: 1-14, 1996 Published July 25 , Mar Ecol Prog Ser Biomass of zooplankton and micronekton in the southern bluefin tuna fishing grounds off eastern Tasmania, Australia J. W. Young*, R. W. Bradford, T. D. Lamb, V. D. Lyne CSIRO Marine Laboratories, Division of Fisheries. GPO Box 1538. Hobart 7001, Tasmania, Australia ABSTRACT: The southern bluefin tuna (SBT) supports a seasonal fishery off the east coast of Tasmania, Australia. The distribution of zooplankton biomass in this region was examined as a means of finding out why the SBT are attracted to this area. We examined whether there was a particular area or depth stratum that supported significantly greater amounts of potential feed, directly or indirectly, for SBT Samples of zooplankton and micronekton were collected during the winter SBT fishery seasons in 1992-94. Five net types (mouth opening 0 25 to -80 m') w~thcodend mesh sizes ranging from 100 to 1000 pm were used. Samples were collected from 4 main hydrographic areas: warm East Australian Current water, cool subantarctic water, the front separating them (the subtrop~calconvergence), and the adjacent shelf. Four depth strata (50, 150, 250 and 350 m) were also sampled. In contrast to our expectations, the biomass in the subtropical convergence was no greater than that in the 3 other areas. Rather, it was the shelf, albeit with some inconsistencies, that generally had the greatest biomass of both zooplankton and micronekton. Offshore, there was no s~gnificantdifference in the biomass of the depth strata sampled, although the biomass of gelatinous zooplankton in the surface waters increased during the study period. -
Biology of Chordates Video Guide
Branches on the Tree of Life DVD – CHORDATES Written and photographed by David Denning and Bruce Russell ©2005, BioMEDIA ASSOCIATES (THUMBNAIL IMAGES IN THIS GUIDE ARE FROM THE DVD PROGRAM) .. .. To many students, the phylum Chordata doesn’t seem to make much sense. It contains such apparently disparate animals as tunicates (sea squirts), lancelets, fish and humans. This program explores the evolution, structure and classification of chordates with the main goal to clarify the unity of Phylum Chordata. All chordates possess four characteristics that define the phylum, although in most species, these characteristics can only be seen during a relatively small portion of the life cycle (and this is often an embryonic or larval stage, when the animal is difficult to observe). These defining characteristics are: the notochord (dorsal stiffening rod), a hollow dorsal nerve cord; pharyngeal gills; and a post anal tail that includes the notochord and nerve cord. Subphylum Urochordata The most primitive chordates are the tunicates or sea squirts, and closely related groups such as the larvaceans (Appendicularians). In tunicates, the chordate characteristics can be observed only by examining the entire life cycle. The adult feeds using a ‘pharyngeal basket’, a type of pharyngeal gill formed into a mesh-like basket. Cilia on the gill draw water into the mouth, through the basket mesh and out the excurrent siphon. Tunicates have an unusual heart which pumps by ‘wringing out’. It also reverses direction periodically. Tunicates are usually hermaphroditic, often casting eggs and sperm directly into the sea. After fertilization, the zygote develops into a ‘tadpole larva’. This swimming larva shows the remaining three chordate characters - notochord, dorsal nerve cord and post-anal tail. -
Using Information in Taxonomists' Heads to Resolve Hagfish And
This article was downloaded by: [Max Planck Inst fuer Evolutionsbiologie] On: 03 September 2013, At: 07:01 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Historical Biology: An International Journal of Paleobiology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ghbi20 Using information in taxonomists’ heads to resolve hagfish and lamprey relationships and recapitulate craniate–vertebrate phylogenetic history Maria Abou Chakra a , Brian Keith Hall b & Johnny Ricky Stone a b c d a Department of Biology , McMaster University , Hamilton , Canada b Department of Biology , Dalhousie University , Halifax , Canada c Origins Institute, McMaster University , Hamilton , Canada d SHARCNet, McMaster University , Hamilton , Canada Published online: 02 Sep 2013. To cite this article: Historical Biology (2013): Using information in taxonomists’ heads to resolve hagfish and lamprey relationships and recapitulate craniate–vertebrate phylogenetic history, Historical Biology: An International Journal of Paleobiology To link to this article: http://dx.doi.org/10.1080/08912963.2013.825792 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information.