Life on Earth
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"Lophophorates" Brachiopoda Echinodermata Asterozoa
Deuterostomes Bryozoa Phoronida "lophophorates" Brachiopoda Echinodermata Asterozoa Stelleroidea Asteroidea Ophiuroidea Echinozoa Holothuroidea Echinoidea Crinozoa Crinoidea Chaetognatha (arrow worms) Hemichordata (acorn worms) Chordata Urochordata (sea squirt) Cephalochordata (amphioxoius) Vertebrata PHYLUM CHAETOGNATHA (70 spp) Arrow worms Fossils from the Cambrium Carnivorous - link between small phytoplankton and larger zooplankton (1-15 cm long) Pharyngeal gill pores No notochord Peculiar origin for mesoderm (not strictly enterocoelous) Uncertain relationship with echinoderms PHYLUM HEMICHORDATA (120 spp) Acorn worms Pharyngeal gill pores No notochord (Stomochord cartilaginous and once thought homologous w/notochord) Tornaria larvae very similar to asteroidea Bipinnaria larvae CLASS ENTEROPNEUSTA (acorn worms) Marine, bottom dwellers CLASS PTEROBRANCHIA Colonial, sessile, filter feeding, tube dwellers Small (1-2 mm), "U" shaped gut, no gill slits PHYLUM CHORDATA Body segmented Axial notochord Dorsal hollow nerve chord Paired gill slits Post anal tail SUBPHYLUM UROCHORDATA Marine, sessile Body covered in a cellulose tunic ("Tunicates") Filter feeder (» 200 L/day) - perforated pharnx adapted for filtering & repiration Pharyngeal basket contractable - squirts water when exposed at low tide Hermaphrodites Tadpole larvae w/chordate characteristics (neoteny) CLASS ASCIDIACEA (sea squirt/tunicate - sessile) No excretory system Open circulatory system (can reverse blood flow) Endostyle - (homologous to thyroid of vertebrates) ciliated groove -
Anoxygenic Photosynthesis in Photolithotrophic Sulfur Bacteria and Their Role in Detoxication of Hydrogen Sulfide
antioxidants Review Anoxygenic Photosynthesis in Photolithotrophic Sulfur Bacteria and Their Role in Detoxication of Hydrogen Sulfide Ivan Kushkevych 1,* , Veronika Bosáková 1,2 , Monika Vítˇezová 1 and Simon K.-M. R. Rittmann 3,* 1 Department of Experimental Biology, Faculty of Science, Masaryk University, 62500 Brno, Czech Republic; [email protected] (V.B.); [email protected] (M.V.) 2 Department of Biology, Faculty of Medicine, Masaryk University, 62500 Brno, Czech Republic 3 Archaea Physiology & Biotechnology Group, Department of Functional and Evolutionary Ecology, Universität Wien, 1090 Vienna, Austria * Correspondence: [email protected] (I.K.); [email protected] (S.K.-M.R.R.); Tel.: +420-549-495-315 (I.K.); +431-427-776-513 (S.K.-M.R.R.) Abstract: Hydrogen sulfide is a toxic compound that can affect various groups of water microorgan- isms. Photolithotrophic sulfur bacteria including Chromatiaceae and Chlorobiaceae are able to convert inorganic substrate (hydrogen sulfide and carbon dioxide) into organic matter deriving energy from photosynthesis. This process takes place in the absence of molecular oxygen and is referred to as anoxygenic photosynthesis, in which exogenous electron donors are needed. These donors may be reduced sulfur compounds such as hydrogen sulfide. This paper deals with the description of this metabolic process, representatives of the above-mentioned families, and discusses the possibility using anoxygenic phototrophic microorganisms for the detoxification of toxic hydrogen sulfide. Moreover, their general characteristics, morphology, metabolism, and taxonomy are described as Citation: Kushkevych, I.; Bosáková, well as the conditions for isolation and cultivation of these microorganisms will be presented. V.; Vítˇezová,M.; Rittmann, S.K.-M.R. -
Limits of Life on Earth Some Archaea and Bacteria
Limits of life on Earth Thermophiles Temperatures up to ~55C are common, but T > 55C is Some archaea and bacteria (extremophiles) can live in associated usually with geothermal features (hot springs, environments that we would consider inhospitable to volcanic activity etc) life (heat, cold, acidity, high pressure etc) Thermophiles are organisms that can successfully live Distinguish between growth and survival: many organisms can survive intervals of harsh conditions but could not at high temperatures live permanently in such conditions (e.g. seeds, spores) Best studied extremophiles: may be relevant to the Interest: origin of life. Very hot environments tolerable for life do not seem to exist elsewhere in the Solar System • analogs for extraterrestrial environments • `extreme’ conditions may have been more common on the early Earth - origin of life? • some unusual environments (e.g. subterranean) are very widespread Extraterrestrial Life: Spring 2008 Extraterrestrial Life: Spring 2008 Grand Prismatic Spring, Yellowstone National Park Hydrothermal vents: high pressure in the deep ocean allows liquid water Colors on the edge of the at T >> 100C spring are caused by different colonies of thermophilic Vents emit superheated water (300C or cyanobacteria and algae more) that is rich in minerals Hottest water is lifeless, but `cooler’ ~50 species of such thermophiles - mostly archae with some margins support array of thermophiles: cyanobacteria and anaerobic photosynthetic bacteria oxidize sulphur, manganese, grow on methane + carbon monoxide etc… Sulfolobus: optimum T ~ 80C, minimum 60C, maximum 90C, also prefer a moderately acidic pH. Live by oxidizing sulfur Known examples can grow (i.e. multiply) at temperatures which is abundant near hot springs. -
Number of Living Species in Australia and the World
Numbers of Living Species in Australia and the World 2nd edition Arthur D. Chapman Australian Biodiversity Information Services australia’s nature Toowoomba, Australia there is more still to be discovered… Report for the Australian Biological Resources Study Canberra, Australia September 2009 CONTENTS Foreword 1 Insecta (insects) 23 Plants 43 Viruses 59 Arachnida Magnoliophyta (flowering plants) 43 Protoctista (mainly Introduction 2 (spiders, scorpions, etc) 26 Gymnosperms (Coniferophyta, Protozoa—others included Executive Summary 6 Pycnogonida (sea spiders) 28 Cycadophyta, Gnetophyta under fungi, algae, Myriapoda and Ginkgophyta) 45 Chromista, etc) 60 Detailed discussion by Group 12 (millipedes, centipedes) 29 Ferns and Allies 46 Chordates 13 Acknowledgements 63 Crustacea (crabs, lobsters, etc) 31 Bryophyta Mammalia (mammals) 13 Onychophora (velvet worms) 32 (mosses, liverworts, hornworts) 47 References 66 Aves (birds) 14 Hexapoda (proturans, springtails) 33 Plant Algae (including green Reptilia (reptiles) 15 Mollusca (molluscs, shellfish) 34 algae, red algae, glaucophytes) 49 Amphibia (frogs, etc) 16 Annelida (segmented worms) 35 Fungi 51 Pisces (fishes including Nematoda Fungi (excluding taxa Chondrichthyes and (nematodes, roundworms) 36 treated under Chromista Osteichthyes) 17 and Protoctista) 51 Acanthocephala Agnatha (hagfish, (thorny-headed worms) 37 Lichen-forming fungi 53 lampreys, slime eels) 18 Platyhelminthes (flat worms) 38 Others 54 Cephalochordata (lancelets) 19 Cnidaria (jellyfish, Prokaryota (Bacteria Tunicata or Urochordata sea anenomes, corals) 39 [Monera] of previous report) 54 (sea squirts, doliolids, salps) 20 Porifera (sponges) 40 Cyanophyta (Cyanobacteria) 55 Invertebrates 21 Other Invertebrates 41 Chromista (including some Hemichordata (hemichordates) 21 species previously included Echinodermata (starfish, under either algae or fungi) 56 sea cucumbers, etc) 22 FOREWORD In Australia and around the world, biodiversity is under huge Harnessing core science and knowledge bases, like and growing pressure. -
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MARINE ECOLOGY PROGRESS SERIES Vol. 166: 301-306, 1998 Published May 28 Mar Ecol Prog Ser l NOTE Diel vertical movement by mesograzers on seaweeds Cary N. Rogers*, Jane E. Williamson, David G. Carson, Peter D. Steinberg School of Biological Science. University of New South Wales. Sydney 2052. Australia ABSTRACT- Diel vertical movement is well documented for nutrients across trophic levels in such systems (Kitting many zooplankton. The ecology of small benthic herbivores et al. 1984, Longhurst & Harrison 1989). which use seaweeds as food and habitat, known as 'meso- Arguably, the dominant model to explain die1 verti- grazers', is similar in some regards to zooplankton, and we hypothesised that mesograzers might also exhlbit diel pat- cal movement by zooplankton is avoidance of visually terns of movement on host algae. We studied 3 non-swim- feeding predators in surface waters during the day ming species of mesograzer, the sea hare Aplysia parvula, the (Zaret & Suffern 1976, Stich & Lampert 1981, Bollens & sea urchin Holopneustes purpurascens, and the prosobranch Frost 1989).This model is supported by studies of both mollusc Phasianotrochus eximius. All exhibited diel move- & ment on host algae. This behaviour occurred on different host demersal and pelagic zooplankton (Robertson algae, despite variation in algal morphology and other char- Howard 1978, Alldredge & King 1985, Ohman 1990, acters. Possible factors causing diel movement by mesograz- Osgood & Frost 1994), although the impact of preda- ers include predation, nutritional gain, avoidance of photo- tion on zooplankton vanes with nntogenetic stage, damage, micro-environmental vanation near host algae, and food availability, and predator evasion or defence reproductive strategies. -
The Plankton Lifeform Extraction Tool: a Digital Tool to Increase The
Discussions https://doi.org/10.5194/essd-2021-171 Earth System Preprint. Discussion started: 21 July 2021 Science c Author(s) 2021. CC BY 4.0 License. Open Access Open Data The Plankton Lifeform Extraction Tool: A digital tool to increase the discoverability and usability of plankton time-series data Clare Ostle1*, Kevin Paxman1, Carolyn A. Graves2, Mathew Arnold1, Felipe Artigas3, Angus Atkinson4, Anaïs Aubert5, Malcolm Baptie6, Beth Bear7, Jacob Bedford8, Michael Best9, Eileen 5 Bresnan10, Rachel Brittain1, Derek Broughton1, Alexandre Budria5,11, Kathryn Cook12, Michelle Devlin7, George Graham1, Nick Halliday1, Pierre Hélaouët1, Marie Johansen13, David G. Johns1, Dan Lear1, Margarita Machairopoulou10, April McKinney14, Adam Mellor14, Alex Milligan7, Sophie Pitois7, Isabelle Rombouts5, Cordula Scherer15, Paul Tett16, Claire Widdicombe4, and Abigail McQuatters-Gollop8 1 10 The Marine Biological Association (MBA), The Laboratory, Citadel Hill, Plymouth, PL1 2PB, UK. 2 Centre for Environment Fisheries and Aquacu∑lture Science (Cefas), Weymouth, UK. 3 Université du Littoral Côte d’Opale, Université de Lille, CNRS UMR 8187 LOG, Laboratoire d’Océanologie et de Géosciences, Wimereux, France. 4 Plymouth Marine Laboratory, Prospect Place, Plymouth, PL1 3DH, UK. 5 15 Muséum National d’Histoire Naturelle (MNHN), CRESCO, 38 UMS Patrinat, Dinard, France. 6 Scottish Environment Protection Agency, Angus Smith Building, Maxim 6, Parklands Avenue, Eurocentral, Holytown, North Lanarkshire ML1 4WQ, UK. 7 Centre for Environment Fisheries and Aquaculture Science (Cefas), Lowestoft, UK. 8 Marine Conservation Research Group, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK. 9 20 The Environment Agency, Kingfisher House, Goldhay Way, Peterborough, PE4 6HL, UK. 10 Marine Scotland Science, Marine Laboratory, 375 Victoria Road, Aberdeen, AB11 9DB, UK. -
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. -
Zooplankton Community Response to Seasonal Hypoxia: a Test of Three Hypotheses
diversity Article Zooplankton Community Response to Seasonal Hypoxia: A Test of Three Hypotheses Julie E. Keister *, Amanda K. Winans and BethElLee Herrmann School of Oceanography, University of Washington, Box 357940, Seattle, WA 98195, USA; [email protected] (A.K.W.); [email protected] (B.H.) * Correspondence: [email protected] Received: 7 November 2019; Accepted: 28 December 2019; Published: 1 January 2020 Abstract: Several hypotheses of how zooplankton communities respond to coastal hypoxia have been put forward in the literature over the past few decades. We explored three of those that are focused on how zooplankton composition or biomass is affected by seasonal hypoxia using data collected over two summers in Hood Canal, a seasonally-hypoxic sub-basin of Puget Sound, Washington. We conducted hydrographic profiles and zooplankton net tows at four stations, from a region in the south that annually experiences moderate hypoxia to a region in the north where oxygen remains above hypoxic levels. The specific hypotheses tested were that low oxygen leads to: (1) increased dominance of gelatinous relative to crustacean zooplankton, (2) increased dominance of cyclopoid copepods relative to calanoid copepods, and (3) overall decreased zooplankton abundance and biomass at hypoxic sites compared to where oxygen levels are high. Additionally, we examined whether the temporal stability of community structure was decreased by hypoxia. We found evidence of a shift toward more gelatinous zooplankton and lower total zooplankton abundance and biomass at hypoxic sites, but no clear increase in the dominance of cyclopoid relative to calanoid copepods. We also found the lowest variance in community structure at the most hypoxic site, in contrast to our prediction. -
Algae and Cyanobacteria in Coastal and Estuarine Waters
CHAPTER 7 Algae and cyanobacteria in coastal and estuarine waters n coastal and estuarine waters, algae range from single-celled forms to the seaweeds. ICyanobacteria are organisms with some characteristics of bacteria and some of algae. They are similar in size to the unicellular algae and, unlike other bacteria, contain blue-green or green pigments and are able to perform photosynthesis; thus, they are also termed blue-green algae. Algal blooms in the sea have occurred throughout recorded history but have been increasing during recent decades (Anderson, 1989; Smayda, 1989a; Hallegraeff, 1993). In several areas (e.g., the Baltic and North seas, the Adriatic Sea, Japanese coastal waters and the Gulf of Mexico), algal blooms are a recurring phe- nomenon. The increased frequency of occurrence has accompanied nutrient enrich- ment of coastal waters on a global scale (Smayda, 1989b). Blooms of non-toxic phytoplankton species and mass occurrences of macro-algae can affect the amenity value of recreational waters due to reduced transparency, dis- coloured water and scum formation. Furthermore, bloom degradation can be accom- panied by unpleasant odours, resulting in aesthetic problems (see chapter 9). Several human diseases have been reported to be associated with many toxic species of dinoflagellates, diatoms, nanoflagellates and cyanobacteria that occur in the marine environment (CDC, 1997). The effects of these algae on humans are due to some of their constituents, principally algal toxins. Marine algal toxins become a problem primarily because they may concentrate in shellfish and fish that are subsequently eaten by humans (CDR, 1991; Lehane, 2000), causing syndromes known as para- lytic shellfish poisoning (PSP), diarrhetic shellfish poisoning (DSP), amnesic shellfish poisoning (ASP), neurotoxic shellfish poisoning (NSP) and ciguatera fish poisoning (CFP). -
Check List of Plankton of the Northern Red Sea
Pakistan Journal of Marine Sciences, Vol. 9(1& 2), 61-78,2000. CHECK LIST OF PLANKTON OF THE NORTHERN RED SEA Zeinab M. El-Sherif and Sawsan M. Aboul Ezz National Institute of Oceanography and Fisheries, Kayet Bay, Alexandria, Egypt. ABSTRACT: Qualitative estimation of phytoplankton and zooplankton of the northern Red Sea and Gulf of Aqaba were carried out from four sites: Sharm El-Sheikh, Taba, Hurghada and Safaga. A total of 106 species and varieties of phytoplankton were identified including 41 diatoms, 53 dinoflagellates, 10 cyanophytes and 2 chlorophytes. The highest number of species was recorded at Sharm El-Sheikh (46 spp), followed by Safaga (40 spp), Taba (30 spp), and Hurghada (23 spp). About 95 of the recorded species were previously mentioned by different authors in the Red Sea and Gulf of Suez. Eleven species are considered new to the Red Sea. About 115 species of zooplankton were recorded from the different sites. They were dominated by four main phyla namely: Arthropoda, Protozoa, Mollusca, and Urochordata. Sharm El-Sheikh contributed the highest number of species (91) followed by Safaga (47) and Taba (34). Hurghada contributed the least (26). Copepoda dominated the other groups at the four sites. The appearances of Spirulina platensis, Pediastrum simplex, and Oscillatoria spp. of phyto plankton in addition to the rotifer species and the protozoan Difflugia oblongata of zooplankton impart a characteristic feature of inland freshwater discharge due to wastewater dumping at sea in these regions resulting from the expansion of cities and hotels along the coast. KEY WORDS: Plankton, Northern Red Sea, Check list. -
Basal Metazoans - Dirk Erpenbeck, Simion Paul, Michael Manuel, Paulyn Cartwright, Oliver Voigt and Gert Worheide
EVOLUTION OF PHYLOGENETIC TREE OF LIFE - Basal Metazoans - Dirk Erpenbeck, Simion Paul, Michael Manuel, Paulyn Cartwright, Oliver Voigt and Gert Worheide BASAL METAZOANS Dirk Erpenbeck Ludwig-Maximilians Universität München, Germany Simion Paul and Michaël Manuel Université Pierre et Marie Curie in Paris, France. Paulyn Cartwright University of Kansas USA. Oliver Voigt and Gert Wörheide Ludwig-Maximilians Universität München, Germany Keywords: Metazoa, Porifera, sponges, Placozoa, Cnidaria, anthozoans, jellyfishes, Ctenophora, comb jellies Contents 1. Introduction on ―Basal Metazoans‖ 2. Phylogenetic relationships among non-bilaterian Metazoa 3. Porifera (Sponges) 4. Placozoa 5. Ctenophora (Comb-jellies) 6. Cnidaria 7. Cultural impact and relevance to human welfare Glossary Bibliography Biographical Sketch Summary Basal metazoans comprise the four non-bilaterian animal phyla Porifera (sponges), Cnidaria (anthozoans and jellyfishes), Placozoa (Trichoplax) and Ctenophora (comb jellies). The phylogenetic position of these taxa in the animal tree is pivotal for our understanding of the last common metazoan ancestor and the character evolution all Metazoa,UNESCO-EOLSS but is much debated. Morphological, evolutionary, internal and external phylogenetic aspects of the four phyla are highlighted and discussed. SAMPLE CHAPTERS 1. Introduction on “Basal Metazoans” In many textbooks the term ―lower metazoans‖ still refers to an undefined assemblage of invertebrate phyla, whose phylogenetic relationships were rather undefined. This assemblage may contain both bilaterian and non-bilaterian taxa. Currently, ―Basal Metazoa‖ refers to non-bilaterian animals only, four phyla that lack obvious bilateral symmetry, Porifera, Placozoa, Cnidaria and Ctenophora. ©Encyclopedia of Life Support Systems (EOLSS) EVOLUTION OF PHYLOGENETIC TREE OF LIFE - Basal Metazoans - Dirk Erpenbeck, Simion Paul, Michael Manuel, Paulyn Cartwright, Oliver Voigt and Gert Worheide These four phyla have classically been known as ―diploblastic‖ Metazoa. -
Animal Diversity Part 2
Textbook resources • pp. 517-522 • pp. 527-8 Animal Diversity • p. 530 part 2 • pp. 531-2 Clicker question In protostomes A. The blastopore becomes the mouth. B. The blastopore becomes the anus. C. Development involves indeterminate cleavage. D. B and C Fig. 25.2 Phylogeny to know (1). Symmetry Critical innovations to insert: Oral bilateral symmetry ecdysis mouth develops after anus multicellularity Aboral tissues 1 Animal diversity, part 2 Parazoa Diversity 2 I. Parazoa • Porifera: Sponges II. Cnidaria & Ctenophora • Tissues • Symmetry I. Outline the • Germ Layers III. Lophotrochozoa unique • Embryonic characteristics Development of sponges IV. Ecdysozoa • Body Cavities • Segmentation Parazoa Parazoa • Porifera: Sponges • Porifera: Sponges – Multicellular without – Hermaphrodites tissues – Sexual and asexual reproduction – Choanocytes (collar cells) use flagella to move water and nutrients into pores – Intracellular digestion Fig. 25.11 Animal diversity, part 2 Clicker Question Diversity 2 I. Parazoa In diploblastic animals, the inner lining of the digestive cavity or tract is derived from II. Cnidaria & Ctenophora A. Endoderm. II. Outline the B. Ectoderm. unique III. Lophotrochozoa C. Mesoderm. characteristics D. Coelom. of cnidarians and IV. Ecdysozoa ctenophores 2 Coral Box jelly Cnidaria and Ctenophora • Cnidarians – Coral; sea anemone; jellyfish; hydra; box jellies • Ctenophores – Comb jellies Sea anemone Jellyfish Hydra Comb jelly Cnidaria and Ctenophora Fig. 25.12 Coral Box jelly Cnidaria and Ctenophora • Tissues Fig. 25.12 –