Structure and Functioning of the Benthic Communities in the Extreme

Total Page:16

File Type:pdf, Size:1020Kb

Structure and Functioning of the Benthic Communities in the Extreme Structure and functioning of the benthic communities in the extreme dynamic intertidal mudflats along the Guianas coasts : trophic fate of the infauna Thanh Hien Nguyen To cite this version: Thanh Hien Nguyen. Structure and functioning of the benthic communities in the extreme dynamic intertidal mudflats along the Guianas coasts : trophic fate of the infauna. Ecosystems. Université de La Rochelle, 2018. English. NNT : 2018LAROS009. tel-02009850 HAL Id: tel-02009850 https://tel.archives-ouvertes.fr/tel-02009850 Submitted on 6 Feb 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. STRUCTURE AND FUNCTIONING OF THE BENTHIC COMMUNITIES IN THE EXTREME DYNAMIC INTERTIDAL MUDFLATS ALONG THE GUIANAS COASTS: TROPHIC FATE OF THE INFAUNA Nguyen Thanh Hien 13 FEVRIER 2018 UNIVERSITY OF LA ROCHELLE Laboratoire Littoral, Environnement et SociétéS i UNIVERSITÉ DE LA ROCHELLE ÉCOLE DOCTORALE GAY LUSSAC Laboratoire Littoral, Environnement et SociétéS Thèse présentée par Thanh-Hien NGUYEN 13 February 2018 pour obtenir le grade de : Docteur de l’Université de La Rochelle Spécialité : Biologie de l’environnement, des populations, écologie STRUCTURE AND FUNCTIONING OF THE BENTHIC COMMUNITIES IN THE EXTREME DYNAMIC INTERTIDAL MUDFLATS ALONG THE GUIANAS COASTS: TROPHIC FATE OF THE INFAUNA JURY: Tom MOENS Professeur, Ghent University, Belgium, Reviewer Eric THIEBAUT Professeur, University Pierre & Marie Curie, Reviewer Emmanuelle GESLIN Professeur, Université d'Angers, Examiner Olivier MAIRE Maître de Conférences, Université de Bordeaux, Examiner Christine DUPUY Professeur, Université de La Rochelle, Director of the thesis Pierrick BOCHER Maître de conférences (HDR), Université de La Rochelle, Co-supervisor Christel LEFRANCOIS Maître de conférences (HDR), Université de La Rochelle, Co- supervisor ii iii Acknowledgements The elaboration of this thesis would not have been possible without the supervision, collaboration and encouragement of many people to whom I would like to express my sincerest thanks. First of all, I would like to thank my supervisors, Professor Christine Dupuy, Dr. Pierrick Bocher and Dr. Christel Lefrancois, for their continued support and contributions towards the compilation of this thesis and the work within it. Especially, Christine, you were always there for me, whether I needed to discuss data, papers, or my personal life, and listened to, and supported me throughout. Words could never be enough to express my gratitude. Secondly, I would like to acknowledge the Ministry of Education and Training of Vietnam, the University of Science and Technology of Hanoi (USTH), who granted me a scholarship to pursue my PhD study. I am also grateful to my host institutions, LIENSs and University of La Rochelle, for kindly providing such a friendly working environment and for all the facilities needed for my thesis. My special thanks also go to my husband for supporting every choice I have ever made. Thanks for helping me in many crucial points in my life, when I was about to give up, especially for your willingness to take care of our little son, therefore, I could totally focus on my study in France. For sure, you have endured having a PhD wife. Thank you for your patience, particularly, your trust in me through the three consecutive years I was living far away from home. For this and much more I will always be grateful to you. I also want to thank to Jérôme Jourde for his invaluable guidance in macrofauna taxonomy and to Hélène Agogué for provided me great support and assistance during the “battle” with tiny specimens for molecular analyses. And to all the enthusiastic people who carried endless buckets of mud, your help was very much appreciated: Pierre-Yves Pascal, Celine Paris, Tony Bui, Antoine Gardel and, of course, Thierry Guyot for the map. Extra thanks go to Alexandre Carpentier for his expertise on trophic linkages. Finally, to my friends who have come through these last few years with me, I would like to say thank you for your encouragement. Thanks to Mathilde, Benoit, Cyril, Anouk, Yann, Eva and Katherine for sharing with me so many great moments. You all made my days in La Rochelle the best. iv v TABLE OF CONTENTS ACKNOWLEDGEMENTS ............................................................................................................. iv CHAPTER 1: GENERAL INTRODUCTION ................................................................................. 1 1.1. Mechanisms structuring ecological communities..................................................................... 3 1.2. Trophic structure and feeding relationships in ecological communities ................................... 4 1.3. Ecological functioning in the view of trophic linkages ........................................................... 6 1.4. Ecological communities associated with the intertidal mudflats ............................................ 10 1.5. The context of the thesis: Dynamics of the Guianas mudbanks .............................................. 16 Rationale and thesis layout ................................................................................................... 19 CHAPTER 2: AN OVERVIEW OF BENTHIC COMMUNITIES INHABITING MUDFLAT HABITAT ALONG THE GUIANAS COAST ............................................................................... 23 Paper 1. Macrofauna along the Guianas coast ................................................................................ 27 Paper 2. Meiofauna along the Guianas coast .................................................................................. 41 CHAPTER 3: FACTORS STRUCTURING THE BENTHIC COMMUNITIES IN FRENCH GUIANA MUDFLAT .................................................................................................... 53 Paper 3. Dynamics of the Tanaidacea ............................................................................................ 57 Paper 4. Dynamics of the meiofauna ............................................................................................. 73 CHAPTER 4: TROPHIC LINKAGES AND CONCEPTUAL MODELOF INTERTIDAL FOOD WEB IN THE FRENCH GUIANA MUDFLATS ............................................................ 105 Paper 5. Ecological functioning of the benthic communities in the view of trophic linkages ......... 109 CHAPTER 5: GENERAL DISCUSSION, GENERAL CONCLUSIONS, PERSPECTIVES ......................................................................................................................... 139 General discussion ...................................................................................................................... 141 Conclusions ................................................................................................................................ 148 Perspectives ................................................................................................................................ 150 REFERENCES USED IN CHAPTER 1 & CHAPTER 5 ............................................................ 151 vi 0 CHAPTER 1 GENERAL INTRODUCTION 1 2 GENERAL INTRODUCTION 1.1. Mechanisms structuring ecological communities Generally, an ecological community is defined as naturally occurring group of species that are interacting in a unique habitat (Purves et al., 2004). This community is bound together by the network of influences that species have on each other and by the physical characteristics of the environment they inhabit. In intertidal flats, community structure have been long found to be regulated by sets of abiotic variables such as grain size, oxygen concentration, salinity, temperature, etc., to which the species in the community may respond differently (Warwick & Clarke, 1991; Coull, 1999; Lu et al., 2008; Schweiger et al., 2008). Particularly, the greater magnitude fluctuation of physical parameters in intertidal mudflats can put higher stress on the organisms inhabiting these areas (Woodin, 1974). Likewise, community structure is also massively influenced by the various biotic interactions, which mainly involve food availability and interconnections between species (Woodin & Jackson, 1979; Buffan-Dubau & Carman, 2000) (Fig. 1.1.). Figure 1.1. An example of abiotic and biotic parameters governing intertidal ecosystem 3 Within a community, organisms can interact with each other in varieties of ways, in which competition and predation are believed to strongly affect community dynamics and composition (Coneil, 1961a; Wilson, 1991; Hiltunen & Laakso, 2013). Competition occurs when the interactions between organisms result in a reduction of growth, survival or reproduction for both partners of the interactions (each species affected negatively). It commonly involves the use of a limiting resource (Schoener, 1974) (e.g. food, water, light, shelter, nesting site…) and can occur between individuals of the same species/population (intraspecific competition) as well as between individuals from different species/populations (interspecific competition). For example, competition for space among algae and sessile invertebrates is prevalent
Recommended publications
  • (Sea of Okhotsk, Sakhalin Island): 2. Cyclopteridae−Molidae Families
    ISSN 0032-9452, Journal of Ichthyology, 2018, Vol. 58, No. 5, pp. 633–661. © Pleiades Publishing, Ltd., 2018. An Annotated List of the Marine and Brackish-Water Ichthyofauna of Aniva Bay (Sea of Okhotsk, Sakhalin Island): 2. Cyclopteridae−Molidae Families Yu. V. Dyldina, *, A. M. Orlova, b, c, d, A. Ya. Velikanove, S. S. Makeevf, V. I. Romanova, and L. Hanel’g aTomsk State University (TSU), Tomsk, Russia bRussian Federal Research Institute of Fishery and Oceanography (VNIRO), Moscow, Russia cInstitute of Ecology and Evolution, Russian Academy of Sciences (IPEE), Moscow, Russia d Dagestan State University (DSU), Makhachkala, Russia eSakhalin Research Institute of Fisheries and Oceanography (SakhNIRO), Yuzhno-Sakhalinsk, Russia fSakhalin Basin Administration for Fisheries and Conservation of Aquatic Biological Resources—Sakhalinrybvod, Aniva, Yuzhno-Sakhalinsk, Russia gCharles University in Prague, Prague, Czech Republic *e-mail: [email protected] Received March 1, 2018 Abstract—The second, final part of the work contains a continuation of the annotated list of fish species found in the marine and brackish waters of Aniva Bay (southern part of the Sea of Okhotsk, southern part of Sakhalin Island): 137 species belonging to three orders (Perciformes, Pleuronectiformes, Tetraodon- tiformes), 31 family, and 124 genera. The general characteristics of ichthyofauna and a review of the commer- cial fishery of the bay fish, as well as the final systematic essay, are presented. Keywords: ichthyofauna, annotated list, conservation status, commercial importance, marine and brackish waters, Aniva Bay, southern part of the Sea of Okhotsk, Sakhalin Island DOI: 10.1134/S0032945218050053 INTRODUCTION ANNOTATED LIST OF FISHES OF ANIVA BAY The second part concludes the publication on the 19.
    [Show full text]
  • Classification of Wetlands and Deepwater Habitats of the United States
    Pfego-/6^7fV SDMS DocID 463450 ^7'7/ Biological Services Program \ ^ FWS/OBS-79/31 DECEMBER 1979 Superfund Records Center ClassificaHioFF^^^ V\Aetlands and Deepwater Habitats of the United States KPHODtKtD BY NATIONAL TECHNICAL INFOR/V^ATION SERVICE U.S. IKPARTMEN TOF COMMERCt SPRINGMflO, VA. 22161 Fish and Wildlife Service U.S. Department of the Interior (USDI) C # The Biological Services Program was established within the U.S. Fish . and Wildlife Service to supply scientific information and methodologies on key environmental issues which have an impact on fish and wildlife resources and their supporting ecosystems. The mission of the Program is as follows: 1. To strengthen the Fish and Wildlife Service in its role as a primary source of Information on natural fish and wildlife resources, par­ ticularly with respect to environmental impact assessment. 2. To gather, analyze, and present information that will aid decision­ makers in the identification and resolution of problems asso­ ciated with major land and water use changes. 3. To provide better ecological information and evaluation for Department of the Interior development programs, such as those relating to energy development. Information developed by the Biological Services Program is intended for use in the planning and decisionmaking process, to prevent or minimize the impact of development on fish and wildlife. Biological Services research activities and technical assistance services are based on an analysis of the issues, the decisionmakers involved and their information neeids, and an evaluation of the state^f-the-art to Identify information gaps and determine priorities. This Is a strategy to assure that the products produced and disseminated will be timely and useful.
    [Show full text]
  • INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The
    INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The Intertidal Zone is the narrow belt along the shoreline lying between the lowest and highest tide marks. The intertidal or littoral zone is subdivided broadly into four vertical zones based on the amount of time the zone is submerged. From highest to lowest, they are Supratidal or Spray Zone Upper Intertidal submergence time Middle Intertidal Littoral Zone influenced by tides Lower Intertidal Subtidal Sublittoral Zone permanently submerged The intertidal zone may also be subdivided on the basis of the vertical distribution of the species that dominate a particular zone. However, zone divisions should, in most cases, be regarded as approximate! No single system of subdivision gives perfectly consistent results everywhere. Please refer to the intertidal zonation scheme given in the attached table (last page). Zonal Distribution of organisms is controlled by PHYSICAL factors (which set the UPPER limit of each zone): 1) tidal range 2) wave exposure or the degree of sheltering from surf 3) type of substrate, e.g., sand, cobble, rock 4) relative time exposed to air (controls overheating, desiccation, and salinity changes). BIOLOGICAL factors (which set the LOWER limit of each zone): 1) predation 2) competition for space 3) adaptation to biological or physical factors of the environment Species dominance patterns change abruptly in response to physical and/or biological factors. For example, tide pools provide permanently submerged areas in higher tidal zones; overhangs provide shaded areas of lower temperature; protected crevices provide permanently moist areas. Such subhabitats within a zone can contain quite different organisms from those typical for the zone.
    [Show full text]
  • Grade 3 Unit 2 Overview Open Ocean Habitats Introduction
    G3 U2 OVR GRADE 3 UNIT 2 OVERVIEW Open Ocean Habitats Introduction The open ocean has always played a vital role in the culture, subsistence, and economic well-being of Hawai‘i’s inhabitants. The Hawaiian Islands lie in the Pacifi c Ocean, a body of water covering more than one-third of the Earth’s surface. In the following four lessons, students learn about open ocean habitats, from the ocean’s lighter surface to the darker bottom fl oor thousands of feet below the surface. Although organisms are scarce in the deep sea, there is a large diversity of organisms in addition to bottom fi sh such as polycheate worms, crustaceans, and bivalve mollusks. They come to realize that few things in the open ocean have adapted to cope with the increased pressure from the weight of the water column at that depth, in complete darkness and frigid temperatures. Students fi nd out, through instruction, presentations, and website research, that the vast open ocean is divided into zones. The pelagic zone consists of the open ocean habitat that begins at the edge of the continental shelf and extends from the surface to the ocean bottom. This zone is further sub-divided into the photic (sunlight) and disphotic (twilight) zones where most ocean organisms live. Below these two sub-zones is the aphotic (darkness) zone. In this unit, students learn about each of the ocean zones, and identify and note animals living in each zone. They also research and keep records of the evolutionary physical features and functions that animals they study have acquired to survive in harsh open ocean habitats.
    [Show full text]
  • From the Southeast Australian Coast, with Comments on the Distribution and Habitat Preferences of Chondropodinae
    Muvi schmallenbergi gen. nov., sp. nov. (Crustacea, Tanaidacea) from the southeast Australian coast, with comments on the distribution and habitat preferences of Chondropodinae Piotr Jóźwiak and Magdalena Błażewicz Department of Invertebrate Zoology and Hydrobiology, Faculty of Biology and Environmental Protection, University of Łódź, Łódź, Poland ABSTRACT Based on material collected from the shelf off southeast Australia (offshore of Portland), a new genus and new species, Muvi schmallenbergi gen. nov., sp. nov., of the tanaidacean family Metapseudidae, is described. Muvi is distinguishable from other genera within the subfamily Chondropodinae by having equally long antennular flagella. It also differs from other Chondropodinae by a combination of characters such as eyelobes with a group of visual elements, rostrum with smooth lateral edges, pereonites with lateral processes and pleotelson lacking lateral process, antennule article-1 with a single apophysis, maxillule inner lobe well-developed, labial palp bearing three distal setae, cheliped exopod well-developed and setose, pereopod-1 coxa with distinct apophysis, pleopods in five pairs, and uropod basis without apophysis. The genus Deidamiapseudes Sganga & Roccatagliata, 2016 is moved from Chondropodinae (Metapseudidae) to Apseudoidea incertae sedis. An identification key for the genera within Chondropodinae is given, and their distribution is discussed. Submitted 19 February 2020 Subjects Biodiversity, Ecology, Taxonomy, Zoology Accepted 23 May 2021 Published 11 August 2021 Keywords Tanaidacea, Distribution, Shelf, South Australia, Metapseudidae Corresponding author INTRODUCTION Piotr Jóźwiak, [email protected] Tanaidacea, small benthic peracarid crustaceans, represent a poorly recognized Academic editor component of marine ecosystems. Until the end of millennium, the Australian Tanaidacea James Reimer were known only from few taxonomic publications (Haswell, 1882a, 1882b; Haswell, 1885; Additional Information and Whitelegge, 1901; Boesch, 1973; Băcescu, 1981; Sieg, 1993; Edgar, 1997).
    [Show full text]
  • Revised Essd-2020-161 (20 September 2020)
    1 1 Half-hourly changes in intertidal temperature at nine wave-exposed 2 locations along the Atlantic Canadian coast: a 5.5-year study 3 Ricardo A. Scrosati, Julius A. Ellrich, Matthew J. Freeman 4 Department of Biology, St. Francis Xavier University, Antigonish, Nova Scotia B2G 2W5, Canada 5 Correspondence to: Ricardo A. Scrosati ([email protected]) 6 Abstract. Intertidal habitats are unique because they spend alternating periods of 7 submergence (at high tide) and emergence (at low tide) every day. Thus, intertidal temperature 8 is mainly driven by sea surface temperature (SST) during high tides and by air temperature 9 during low tides. Because of that, the switch from high to low tides and viceversa can determine 10 rapid changes in intertidal thermal conditions. On cold-temperate shores, which are 11 characterized by cold winters and warm summers, intertidal thermal conditions can also change 12 considerably with seasons. Despite this uniqueness, knowledge on intertidal temperature 13 dynamics is more limited than for open seas. This is especially true for wave-exposed intertidal 14 habitats, which, in addition to the unique properties described above, are also characterized by 15 wave splash being able to moderate intertidal thermal extremes during low tides. To address this 16 knowledge gap, we measured temperature every half hour during a period of 5.5 years (2014- 17 2019) at nine wave-exposed rocky intertidal locations along the Atlantic coast of Nova Scotia, 18 Canada. This data set is freely available from the figshare online repository (Scrosati and 19 Ellrich, 2020a; https://doi.org/10.6084/m9.figshare.12462065.v1).
    [Show full text]
  • Marsupial Brood Care in Cretaceous Tanaidaceans Alba Sánchez-García 1, Xavier Delclòs 1, Michael S
    www.nature.com/scientificreports OPEN Marsupial brood care in Cretaceous tanaidaceans Alba Sánchez-García 1, Xavier Delclòs 1, Michael S. Engel 2,3, Graham J. Bird4, Vincent Perrichot 5 & Enrique Peñalver 6 Received: 2 December 2016 Parental care in animal evolution has long fascinated biologists, but tracing this complex of behavioural Accepted: 9 May 2017 repertoires is challenging, as these transitory states often leave no corporeal traces as fossils. Among Published: xx xx xxxx modern invertebrates, the tanaidaceans (Malacostraca: Peracarida), a lineage of marsupial crustaceans, show an interesting variety of brooding strategies. Here we report on fossil tanaidaceans from the Cretaceous of Spain and France that provide conclusive evidence for marsupial care of brood-offspring. Two exceptionally preserved female specimens of Alavatanais carabe and A. margulisae from Late Albian Peñacerrada I amber (Spain) possess four pairs of rudimentary oostegites, indicating formation of a marsupium. From Recent data, given the taxonomic distribution of a marsupium of four pairs of oostegites, we hypothesize that this may be plesiomorphic for the Tanaidomorpha. We also report on a peculiar tanaidacean specimen referable to the fossil family Alavatanaidae, Daenerytanais maieuticus gen. et sp. nov., from Early Cenomanian La Buzinie amber (France), preserved with its marsupial pouch and content. Our discoveries provide early evidence of the peracarid reproductive strategy, as seen in modern Tanaidacea, and argue that this form of parental care may have played a role in the diversification of the lineage during this period. The fossil record provides a rich and valuable repository of behavioural and evolutionary developments despite the influence of biases in preservation or density of taxonomic representation.
    [Show full text]
  • PROTISTS Shore and the Waves Are Large, Often the Largest of a Storm Event, and with a Long Period
    (seas), and these waves can mobilize boulders. During this phase of the storm the rapid changes in current direction caused by these large, short-period waves generate high accelerative forces, and it is these forces that ultimately can move even large boulders. Traditionally, most rocky-intertidal ecological stud- ies have been conducted on rocky platforms where the substrate is composed of stable basement rock. Projec- tiles tend to be uncommon in these types of habitats, and damage from projectiles is usually light. Perhaps for this reason the role of projectiles in intertidal ecology has received little attention. Boulder-fi eld intertidal zones are as common as, if not more common than, rock plat- forms. In boulder fi elds, projectiles are abundant, and the evidence of damage due to projectiles is obvious. Here projectiles may be one of the most important defi ning physical forces in the habitat. SEE ALSO THE FOLLOWING ARTICLES Geology, Coastal / Habitat Alteration / Hydrodynamic Forces / Wave Exposure FURTHER READING Carstens. T. 1968. Wave forces on boundaries and submerged bodies. Sarsia FIGURE 6 The intertidal zone on the north side of Cape Blanco, 34: 37–60. Oregon. The large, smooth boulders are made of serpentine, while Dayton, P. K. 1971. Competition, disturbance, and community organi- the surrounding rock from which the intertidal platform is formed zation: the provision and subsequent utilization of space in a rocky is sandstone. The smooth boulders are from a source outside the intertidal community. Ecological Monographs 45: 137–159. intertidal zone and were carried into the intertidal zone by waves. Levin, S. A., and R.
    [Show full text]
  • Climate Change Report for Gulf of the Farallones and Cordell
    Chapter 6 Responses in Marine Habitats Sea Level Rise: Intertidal organisms will respond to sea level rise by shifting their distributions to keep pace with rising sea level. It has been suggested that all but the slowest growing organisms will be able to keep pace with rising sea level (Harley et al. 2006) but few studies have thoroughly examined this phenomenon. As in soft sediment systems, the ability of intertidal organisms to migrate will depend on available upland habitat. If these communities are adjacent to steep coastal bluffs it is unclear if they will be able to colonize this habitat. Further, increased erosion and sedimentation may impede their ability to move. Waves: Greater wave activity (see 3.3.2 Waves) suggests that intertidal and subtidal organisms may experience greater physical forces. A number of studies indicate that the strength of organisms does not always scale with their size (Denny et al. 1985; Carrington 1990; Gaylord et al. 1994; Denny and Kitzes 2005; Gaylord et al. 2008), which can lead to selective removal of larger organisms, influencing size structure and species interactions that depend on size. However, the relationship between offshore significant wave height and hydrodynamic force is not simple. Although local wave height inside the surf zone is a good predictor of wave velocity and force (Gaylord 1999, 2000), the relationship between offshore Hs and intertidal force cannot be expressed via a simple linear relationship (Helmuth and Denny 2003). In many cases (89% of sites examined), elevated offshore wave activity increased force up to a point (Hs > 2-2.5 m), after which force did not increase with wave height.
    [Show full text]
  • Crustacea: Peracarida: Tanaidacea: Apseudomorpha), with Descriptions of a New Genus and Six New Species
    Zootaxa 3734 (4): 401–441 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2013 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3734.4.1 http://zoobank.org/urn:lsid:zoobank.org:pub:00DC3ED7-62FD-4D99-ABCC-0DC57D1A51E7 Tanaidaceans from Brunei, IV. The Families Kalliapseudidae, Pagurapseudopsi- dae, Parapseudidae and Apseudidae (Crustacea: Peracarida: Tanaidacea: Apseudomorpha), with descriptions of a new genus and six new species ROGER N. BAMBER ARTOO Marine Biology Consultants, Ocean Quay Marina, Belvidere Road, Southampton SO14 5QY, United Kingdom. E-mail: [email protected] Abstract Apseudomorph tanaidaceans from recent samples of the South China Sea benthos off Brunei have been examined. The habitats were sandy substrata from between 5 and 90 m depth. Fourteen species of the four families considered here were discovered. A new species of Tanapseudes is described. The distribution of Phoxokalliapseudes gobinae is analyzed. Biropalostoma goofi is recorded for the first time in Brunei waters. One new species of the Apseudidae (in the genus Bunakenia) and four new species of the Parapseudidae (one each in the genera Platylicoa and Pakistanapeudes, and two in a new genus Actenos, of the subfamily Pakistanapseudinae) are described. The genus Platylicoa is moved to the Pakistanapseudinae, and the genus Hainanius is returned to the Parapseudidae (Parapseudinae). Apseudes tenuicorporeus is moved from Biropalostoma to the new pakistanapseudin genus described herein. Key words: Tanaidacea, Pagurapseudidae, Kalliapseudidae, Parapseudidae, Apseudidae, Actenos, Aponychos, Apseudopsis, Bilobatus, Biropalostoma, Bunakenia, Mendamanus, Pakistanapseudes, Pagurapseudopsis, Phoxokalliapseudes, Platylicoa, Tanapseudes, South China Sea Introduction This paper is the fourth on the South China Sea tanaidacean fauna of the waters off Brunei.
    [Show full text]
  • Life in the Intertidal Zone
    Life in the Rocky Intertidal Zone Tidepools provide a home for many animals. Tidepools are created by the changing water level, or tides. The high energy waves make this a harsh habitat, but the animals living here have adapted over time. When the earth, sun and moon align during the full and new moon we have extreme high and low tides. Generally, there are two high tides and two low tides a day. An example of low and high tide is seen on the right. There are three zones within the tidepools: the high zone, the middle zone, and the low zone. Animals are distributed based on their adaptations to different living (competition and predation) and non living (wave action and water loss) factors. The tidepools at Cabrillo are protected and have been monitored by the National Park Service since 1990. You may notice bolts in Low Tide the rocky intertidal, these are used to assist scientists in gathering data to monitor changes. Tidepool Etiquette: Human impact can hurt the animals. As you explore the tidepools, you may touch the animals living here, but only as gently as you would touch your own eyeball. Some animals may die if moved even a few inches from where they are found. Federal law prohibits collection and removal of any shells, rocks and marine specimens. Also, be aware of the changing tides, slippery rocks and unstable cliffs. Have fun exploring! High Tide High Zone The high zone is covered by the highest tides. Often this area is only sprayed by the (Supralittoral or crashing waves.
    [Show full text]
  • Diversity of Tanaidacea (Crustacea: Peracarida) in the World's Oceans - How Far Have We Come?
    The University of Southern Mississippi The Aquila Digital Community Faculty Publications 4-1-2012 Diversity of Tanaidacea (Crustacea: Peracarida) in the World's Oceans - How Far Have We Come? Gary Anderson University of Southern Mississippi, [email protected] Magdalena Blazewicz-Paszkowycz University of Łódź, [email protected] Roger Bamber Artoo Marine Biology Consultants, [email protected] Follow this and additional works at: https://aquila.usm.edu/fac_pubs Part of the Marine Biology Commons Recommended Citation Anderson, G., Blazewicz-Paszkowycz, M., Bamber, R. (2012). Diversity of Tanaidacea (Crustacea: Peracarida) in the World's Oceans - How Far Have We Come?. PLoS One, 7(4), 1-11. Available at: https://aquila.usm.edu/fac_pubs/160 This Article is brought to you for free and open access by The Aquila Digital Community. It has been accepted for inclusion in Faculty Publications by an authorized administrator of The Aquila Digital Community. For more information, please contact [email protected]. Diversity of Tanaidacea (Crustacea: Peracarida) in the World’s Oceans – How Far Have We Come? Magdalena Blazewicz-Paszkowycz1*, Roger Bamber2, Gary Anderson3 1 Department of Polar Biology and Oceanobiology, University of Ło´dz´,Ło´dz´, Poland, 2 Artoo Marine Biology Consultants, Ocean Quay Marina, Southampton, Hants, United Kingdom, 3 Department of Biological Sciences, University of Southern Mississippi, Hattiesburg, Mississippi, United States of America Abstract Tanaidaceans are small peracarid crustaceans which occur in all marine habitats, over the full range of depths, and rarely into fresh waters. Yet they have no obligate dispersive phase in their life-cycle. Populations are thus inevitably isolated, and allopatric speciation and high regional diversity are inevitable; cosmopolitan distributions are considered to be unlikely or non-existent.
    [Show full text]