Phylum Echinodermata; Ziser Lecture Notes 2008 1 Phylum: Echinodermata Means “Prickly Skin”
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Flatworms Phylum Platyhelminthes
Flatworms Phylum Platyhelminthes The flatworms include more than 13,000 species of free-living and parasitic species.There are 3 classes of flat- worms, the planarians, flukes and tapeworms. General Physical Traits (Anatomy): Flatworms are bilaterally symmetrical. This means that they can only be cut them length-wise to produce two mirror-image halves. They have a distinct right and left half. This is differ- ent from radially symmetrical animals, like the anemones, which can be cut anywhere top to bottom to get two similar halves. Flatworms have 3 tissue layers, compared to the 2 layers in sponges and cnidarians (jellyfishes, anemones and corals). They also have only one opening for food to enter and waste to leave, like the sponges and cnidarians. This is called a “sac” body plan. Planarian (class Tubellaria) Habitat: They live mostly in saltwater (marine) habitats, but are also found in freshwater. Habits: They are free-living flatworms (not parasites). Physical Traits (Anatomy): Planarians are small - less than a centimeter long. They have a head, brain and sense organs. This is called “cephalization.” The sense organs – called eyespots – look like eyes and are sensitive to light changes, but are not like human eyes. They are made up of simple nerve cells that respond to stimuli, like light. When many nerve cells are gathered in one place, they are called a “ganglion,” so the two eyespots are actually ganglia. They also have points on either side of the head that look a bit like ears, called “sensory lobes” or auricles. They do not hear, but can sense food. -
Ediacaran) of Earth – Nature’S Experiments
The Early Animals (Ediacaran) of Earth – Nature’s Experiments Donald Baumgartner Medical Entomologist, Biologist, and Fossil Enthusiast Presentation before Chicago Rocks and Mineral Society May 10, 2014 Illinois Famous for Pennsylvanian Fossils 3 In the Beginning: The Big Bang . Earth formed 4.6 billion years ago Fossil Record Order 95% of higher taxa: Random plant divisions domains & kingdoms Cambrian Atdabanian Fauna Vendian Tommotian Fauna Ediacaran Fauna protists Proterozoic algae McConnell (Baptist)College Pre C - Fossil Order Archaean bacteria Source: Truett Kurt Wise The First Cells . 3.8 billion years ago, oxygen levels in atmosphere and seas were low • Early prokaryotic cells probably were anaerobic • Stromatolites . Divergence separated bacteria from ancestors of archaeans and eukaryotes Stromatolites Dominated the Earth Stromatolites of cyanobacteria ruled the Earth from 3.8 b.y. to 600 m. [2.5 b.y.]. Believed that Earth glaciations are correlated with great demise of stromatolites world-wide. 8 The Oxygen Atmosphere . Cyanobacteria evolved an oxygen-releasing, noncyclic pathway of photosynthesis • Changed Earth’s atmosphere . Increased oxygen favored aerobic respiration Early Multi-Cellular Life Was Born Eosphaera & Kakabekia at 2 b.y in Canada Gunflint Chert 11 Earliest Multi-Cellular Metazoan Life (1) Alga Eukaryote Grypania of MI at 1.85 b.y. MI fossil outcrop 12 Earliest Multi-Cellular Metazoan Life (2) Beads Horodyskia of MT and Aust. at 1.5 b.y. thought to be algae 13 Source: Fedonkin et al. 2007 Rise of Animals Tappania Fungus at 1.5 b.y Described now from China, Russia, Canada, India, & Australia 14 Earliest Multi-Cellular Metazoan Animals (3) Worm-like Parmia of N.E. -
Late Cretaceous-Early Palaeogene Echinoderms and the K/T Boundary in the Southeast Netherlands and Northeast Belgium — Part 6: Conclusions
pp 507-580 15-01-2007 14:51 Pagina 505 Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions John W.M. Jagt Jagt, J.W.M. Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions. — Scripta Geol., 121: 505-577, 8 figs., 9 tables, Leiden, December 2000. John W.M. Jagt, Natuurhistorisch Museum Maastricht, Postbus 882, NL-6200 AW Maastricht, The Netherlands, E-mail: [email protected] Key words: Echinodermata, Late Cretaceous, Early Palaeogene, palaeobiology, K/T boundary, extinc- tion. The palaeobiology of echinoderms occurring in the Meerssen and Geulhem members is discussed and changes in diversity across the K/T boundary are documented. Using literature data on the ecology of extant faunas, the various echinoderm groups are considered. Naturally, such data can only be applied with due caution to fossil forms, whose skeletal morphology is often incompletely known. This holds especially true for asteroids, ophiuroids, and crinoids, which, upon death, rapidly disinte- grate into jumbles of dissociated ossicles. Bioturbation, scavenging, and current winnowing all con- tribute to blurring the picture still further. However, data on extant forms do allow a preliminary sub- division of fossil species into various ecological groups, which are discussed herein. Combining recently published data on K/T boundary sections in Jylland and Sjælland (Denmark) with the pic- ture drawn here for the Maastricht area results in the following best constrained scenario. The demise of the highly diverse latest Maastrichtian echinoderm faunas, typical of shallow-water settings with local palaeorelief and associated unconsolidated bottoms, was rapid, suggestive of a catastrophic event (e.g. -
Phylum Chordata
Phylum Chordata 48,000 species very diverse phylum but still more unity in major characteristics than in most other phyla most advanced phylum of animal kingdom one to which we belong along with fish, amphibians reptiles, birds and other mammals some of the largest or most massive animals true coelom 4 major identifying characteristics: 1. Notochord flexible rodlike structure enclosed by a fibrous sheath extends the length of the body in larva and/or adult provides basic support and serves as main axis for muscle attachments to permit “fishlike” undulatory movements first part of skeleton to form in embryo in primitive chordates the notochord persists through life Animals: Chordates & Introduction to Vertebrates; Ziser Lecture Notes, 2006 1 in most chordates the notochord is replaced by a vertebral column of bone remnants of the notochord remain as “intervertebral discs” 2. Dorsal tubular nerve cord in most invert groups; nerve cord is ventral & paired in chordates the nerve cord is a single dorsal hollow nerve cord front end usually enlarged to form brain 3. Pharyngeal (gill) slits slit-like opening sleading from throat to outside first evolved as a filter feeding apparatus still used by some to filter water for food in others as gills in some groups they are only found in embryo and lost as adults 4. endostyle or thyroid gland specific kind of tissue found only in chordates was originally part of the feeding apparatus endostyle secretes mucus and traps food inside the pharyngeal cavity eg. lamprey larva in most chordates the same tissue has become an endocrine Animals: Chordates & Introduction to Vertebrates; Ziser Lecture Notes, 2006 2 gland in the neck region that helps control metabolism 5. -
Animal Phylum Poster Porifera
Phylum PORIFERA CNIDARIA PLATYHELMINTHES ANNELIDA MOLLUSCA ECHINODERMATA ARTHROPODA CHORDATA Hexactinellida -- glass (siliceous) Anthozoa -- corals and sea Turbellaria -- free-living or symbiotic Polychaetes -- segmented Gastopods -- snails and slugs Asteroidea -- starfish Trilobitomorpha -- tribolites (extinct) Urochordata -- tunicates Groups sponges anemones flatworms (Dugusia) bristleworms Bivalves -- clams, scallops, mussels Echinoidea -- sea urchins, sand Chelicerata Cephalochordata -- lancelets (organisms studied in detail in Demospongia -- spongin or Hydrazoa -- hydras, some corals Trematoda -- flukes (parasitic) Oligochaetes -- earthworms (Lumbricus) Cephalopods -- squid, octopus, dollars Arachnida -- spiders, scorpions Mixini -- hagfish siliceous sponges Xiphosura -- horseshoe crabs Bio1AL are underlined) Cubozoa -- box jellyfish, sea wasps Cestoda -- tapeworms (parasitic) Hirudinea -- leeches nautilus Holothuroidea -- sea cucumbers Petromyzontida -- lamprey Mandibulata Calcarea -- calcareous sponges Scyphozoa -- jellyfish, sea nettles Monogenea -- parasitic flatworms Polyplacophora -- chitons Ophiuroidea -- brittle stars Chondrichtyes -- sharks, skates Crustacea -- crustaceans (shrimp, crayfish Scleropongiae -- coralline or Crinoidea -- sea lily, feather stars Actinipterygia -- ray-finned fish tropical reef sponges Hexapoda -- insects (cockroach, fruit fly) Sarcopterygia -- lobed-finned fish Myriapoda Amphibia (frog, newt) Chilopoda -- centipedes Diplopoda -- millipedes Reptilia (snake, turtle) Aves (chicken, hummingbird) Mammalia -
Echinoderms for Dummies Colwyn Sleep Echinoderm Classification and Examples
ECHINODERMS FOR DUMMIES COLWYN SLEEP ECHINODERM CLASSIFICATION AND EXAMPLES What exactly is an Echinoderm? Echinoderms (or “Echinodermata”) are a group of animals which exist only in a marine (ocean) environment. Their name comes from the Greek word for "spiny skin". They inhabit a diverse range of marine habitats and are found on the sea floor from the intertidal zone to great ocean depths. In the following slides we will explore echinoderms and look into their body systems and structures more closely. A FEW EXAMPLES OF ECHINODERMS Sea star Kingdom: Animalia Phylum: Echinodermata Class: Asteroidea Feather Star Kingdom: Animalia Phylum: Echinodermata Subphylum: Crinozoa Class: Crinoidea Probably one of the best known echinoderms This lesser-known star, the feather star gains is the easily recognized sea star. The its name from its featherlike arms, which it echinoderm phylum contains many more uses to swim through the water. Like all species, in fact there are around 7000 known echinoderms, they are “Deuterostomes.” echinoderms. Later, we will investigate the This means that during their embryonic sea star and it’s classification as an development the first embryonic opening echinoderm in greater detail. becomes the anus and the second becomes the mouth. Because of this, biologists believe that echinoderms are more evolutionarily advanced than some of the other animals. A FEW MORE… Sea cucumber Kingdom: Animalia Phylum: Echinodermata Class: Holothuroidea Sea Urchin Kingdom: Animalia Phylum: Echinodermata Class: Echinoidea Related to Jabba the Hutt in appearance Like other echinoderms, the sea urchin has only, the sea cucumber is actually another radial symmetry. Its pointed spines offer example of an echinoderm. -
Introduction to Phylum Chordata
Unifying Themes 1. Chordate evolution is a history of innovations that is built upon major invertebrate traits •bilateral symmetry •cephalization •segmentation •coelom or "gut" tube 2. Chordate evolution is marked by physical and behavioral specializations • For example the forelimb of mammals has a wide range of structural variation, specialized by natural selection 3. Evolutionary innovations and specializations led to adaptive radiations - the development of a variety of forms from a single ancestral group Characteristics of the Chordates 1. Notochord 2. dorsal hollow nerve cord 3. pharyngeal gill slits 4. postanal tail 5. endostyle Characteristics of the Chordates Notochord •stiff, flexible rod, provides internal support • Remains throughout the life of most invertebrate chordates • only in the embryos of vertebrate chordates Characteristics of the Chordates cont. Dorsal Hollow Nerve Cord (Spinal Cord) •fluid-filled tube of nerve tissue, runs the length of the animal, just dorsal to the notochord • Present in chordates throughout embryonic and adult life Characteristics of the Chordates cont. Pharyngeal gill slits • Pairs of opening through the pharynx • Invertebrate chordates use them to filter food •In fishes the gill sits develop into true gills • In reptiles, birds, and mammals the gill slits are vestiges (occurring only in the embryo) Characteristics of the Chordates cont. Endostyle • mucous secreting structure found in the pharynx floor (traps small food particles) Characteristics of the Chordates cont. Postanal Tail • works with muscles (myomeres) & notochord to provide motility & stability • Aids in propulsion in nonvertebrates & fish but vestigial in later lineages SubPhylum Urochordata Ex: tunicates or sea squirts • Sessile as adults, but motile during the larval stages • Possess all 5 chordate characteristics as larvae • Settle head first on hard substrates and undergo a dramatic metamorphosis • tail, notochord, muscle segments, and nerve cord disappear SubPhylum Urochordata cont. -
The Role of Chemical Signals on the Feeding Behavior of the Crown-Of-Thorns Seastar, Acanthaster Planci (Linnaeus, 1758)
THE ROLE OF CHEMICAL SIGNALS ON THE FEEDING BEHAVIOR OF THE CROWN-OF-THORNS SEASTAR, ACANTHASTER PLANCI (LINNAEUS, 1758) BY CIEMON FRANK CABALLES A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE IN BIOLOGY UNIVERSITY OF GUAM SEPTEMBER, 2009 AN ABSTRACT OF THE THESIS of Ciemon Frank Caballes for the Master of Science in Biology presented 25 September, 2009. Title: The Role of Chemical Signals on the Feeding Behavior of the Crown-of- Thorns Seastar, Acanthaster planci (Linnaeus, 1758) Approved: ______________________________________________________________ Peter J. Schupp, Chairman, Thesis Committee Coral reefs are among the world’s most diverse and productive ecosystems, but at the same time also one of the most threatened. Increasing anthropogenic pressure has limited the resilience of reefs to natural disturbances, such as outbreaks of crown-of- thorns seastar, Acanthaster planci. A. planci is a corallivore known to inflict large-scale coral mortality at high population densities and continues to be a reef management problem despite previous control efforts. There has been no active control of A. planci populations on Guam since the 1970’s despite recent surveys showing that A. planci outbreaks continue to damage large areas of reef and is one of the primary sources of coral mortality around Guam. Large aggregations of up to 522 individuals/ha of reef were observed to feed mainly on Acroporids, especially encrusting Montipora and branching Acropora. Preferential feeding by A. planci, even at moderate densities, causes differential mortality among coral species, which can exert a major influence on community structure. Despite this, the underlying mechanisms involved in this feeding behavior are still poorly understood. -
An Early Cretaceous Astropectinid (Echinodermata, Asteroidea)
Andean Geology 41 (1): 210-223. January, 2014 Andean Geology doi: 10.5027/andgeoV41n1-a0810.5027/andgeoV40n2-a?? formerly Revista Geológica de Chile www.andeangeology.cl An Early Cretaceous astropectinid (Echinodermata, Asteroidea) from Patagonia (Argentina): A new species and the oldest record of the family for the Southern Hemisphere Diana E. Fernández1, Damián E. Pérez2, Leticia Luci1, Martín A. Carrizo2 1 Instituto de Estudios Andinos Don Pablo Groeber (IDEAN-CONICET), Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Intendente Güiraldes 2160, Pabellón 2, Ciudad Universitaria, Ciudad Autónoma de Buenos Aires, Argentina. [email protected]; [email protected] 2 Museo de Ciencias Naturales Bernardino Rivadavia, Ángel Gallardo 470, Ciudad Autónoma de Buenos Aires, Argentina. [email protected]; [email protected] ABSTRACT. Asterozoans are free living, star-shaped echinoderms which are important components of benthic marine faunas worldwide. Their fossil record is, however, poor and fragmentary, probably due to dissarticulation of ossicles. In particular, fossil asteroids are infrequent in South America. A new species of starfish is reported from the early Valanginian of the Mulichinco Formation, Neuquén Basin, in the context of a shallow-water, storm-dominated shoreface environment. The specimen belongs to the Astropectinidae, and was assigned to a new species within the genus Tethyaster Sladen, T. antares sp. nov., characterized by a R:r ratio of 2.43:1, rectangular marginals wider in the interbrachial angles, infero- marginals (28 pairs along a median arc) with slightly convex profile and flat spines (one per ossicle in the interbrachials and two per ossicle in the arms). -
Brain-Size Evolution and Sociality in Carnivora
Brain-size evolution and sociality in Carnivora John A. Finarellia,b,1 and John J. Flynnc aDepartment of Geological Sciences, University of Michigan, 2534 C.C. Little Building, 1100 North University Avenue, Ann Arbor, MI 48109; bMuseum of Paleontology, University of Michigan, 1529 Ruthven Museum, 1109 Geddes Road, Ann Arbor, MI 48109; and cDivision of Paleontology and Richard Gilder Graduate School, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024 Edited by Alan Walker, Pennsylvania State University, University Park, PA, and approved April 22, 2009 (received for review February 16, 2009) Increased encephalization, or larger brain volume relative to body develop a comprehensive view of the evolutionary history of mass, is a repeated theme in vertebrate evolution. Here we present encephalization across 289 terrestrial species (including 125 an extensive sampling of relative brain sizes in fossil and extant extinct species) of Carnivora, providing an extensive sampling of taxa in the mammalian order Carnivora (cats, dogs, bears, weasels, fossil and living taxa for both major subclades: Caniformia and and their relatives). By using Akaike Information Criterion model Feliformia. selection and endocranial volume and body mass data for 289 species (including 125 fossil taxa), we document clade-specific Results evolutionary transformations in encephalization allometries. Akaike Information Criterion (AIC) model selection recovered These evolutionary transformations include multiple independent 4 optimal models (OM) within 2 log-likelihood units of the encephalization increases and decreases in addition to a remark- highest score (Table 1). There is broad agreement among the ably static basal Carnivora allometry that characterizes much of the OM with differences primarily in estimates of allometric slopes. -
Study Questions 2 (Through Arthropod 1)
Study Questions 2 (through Arthropod 1) 1. Name the three embryonic germ layers found in all triploblastic animals. 2. What is a coelom? Which Phyla that we have discussed thus far have a true coelom? 3. Define cephalization. What is the name of the most primitive Phylum we have discussed that displays cephalization? 4. How is the digestive system of a Turbellarian similar to the digestive system of a Hydrozoan? Describe one way that they are different. 5. What is the function of flame cells? 6. How is the nervous system of a flatworm (Phylum Platyhelminthes) different from that of a Cnidarian? 7. Which two classes of flatworms are entirely parasitic? Describe some adaptations for parasitism that are found in these classes. 8. What are some of the major differences between Nemertine worms (Phylum Nemertea) and flatworms (Phylum Platyhelminthes)? In what major way are these two phyla similar? 9. What is a pseudocoelom? What are some of the functions of the pseudocoelom in Phylum Nematoda? 10. Nematodes have move in a characteristic whip like fashion. What aspect of their anatomy is responsible for this type of movement? 11. Describe the general structure of the Nematode nervous system. How is it different from the nervous system of Platyhelminthes? 12. What is unique about Nematode muscle cells? 13. What is unique about the way Nematode sperm move? 14. Many Nematodes are parasitic. Describe some adaptations that Nematodes have for parasitism. 15. What characteristics of the Nematode Caenorhabditis elegans make such an important model organism for the study of developmental genetics? 16. List two functions of the Rotifer corona. -
Outline 11: Fossil Record of Early Life Life in the Precambrian Time Line
Outline 11: Fossil Record of Early Life Life in the Precambrian Time Line • 0.545 BY – animals with hard parts, start of the Phanerozoic Eon • 0.600 BY – first animals, no hard parts • 2.0 BY – first definite eukaryotes • 2.0-3.5 BY – formation of BIF’s, stromatolites common • 3.5 BY – oldest definite fossils: stromatolites • 3.8 BY – C12 enrichment in sedimentary rocks, chemical evidence for life; not definitive of life • 4.0 BY – oldest rocks of sedimentary origin Fossil Evidence • 3.8 BY ago: small carbon compound spheres - early cells? Maybe not. • 3.5 BY ago: definite fossils consisting of stromatolites and the cyanobacteria that formed them. The cyanobacteria resemble living aerobic photosynthesizers. • 3.2 BY ago: rod-shaped bacteria Fossil Cell? 3.8 BY old from Greenland Modern stromatolites, Bahamas Modern stromatolites produced by cyanobacteria, Sharks Bay, Australia Modern stromatolites produced by cyanobacteria, Sharks Bay, Australia 2 B.Y. old stromatolites from NW Canada Stromatolites, 2 BY old, Minnesota Cyanobacteria, makers of stromatolites Microscopic views Cyanobacteria, makers of stromatolites 1.0 BY old Cyanobacteria 3.5 BY old, Australia Microscopic views Stromatolite, 3.5 BY old, Australia Closeup of stromatolite layers in last slide Modern archaea Fossil archaea or bacteria, 3.2 BY old from Africa Fossil bacteria 2BY Modern bacteria old from Minnesota The Banded Iron Formations • Billions of tons of iron ore, the world’s chief reserves. • Formed between 3.5 and 2.0 BY ago. • They record the gradual oxidation of the oceans by photosynthetic cyanobacteria. • When the oceans finished rusting, oxygen accumulated in the atmosphere.