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MARINE FAUNA and FLORA of BERMUDA a Systematic Guide to the Identification of Marine Organisms
MARINE FAUNA AND FLORA OF BERMUDA A Systematic Guide to the Identification of Marine Organisms Edited by WOLFGANG STERRER Bermuda Biological Station St. George's, Bermuda in cooperation with Christiane Schoepfer-Sterrer and 63 text contributors A Wiley-Interscience Publication JOHN WILEY & SONS New York Chichester Brisbane Toronto Singapore ANTHOZOA 159 sucker) on the exumbrella. Color vari many Actiniaria and Ceriantharia can able, mostly greenish gray-blue, the move if exposed to unfavorable condi greenish color due to zooxanthellae tions. Actiniaria can creep along on their embedded in the mesoglea. Polyp pedal discs at 8-10 cm/hr, pull themselves slender; strobilation of the monodisc by their tentacles, move by peristalsis type. Medusae are found, upside through loose sediment, float in currents, down and usually in large congrega and even swim by coordinated tentacular tions, on the muddy bottoms of in motion. shore bays and ponds. Both subclasses are represented in Ber W. STERRER muda. Because the orders are so diverse morphologically, they are often discussed separately. In some classifications the an Class Anthozoa (Corals, anemones) thozoan orders are grouped into 3 (not the 2 considered here) subclasses, splitting off CHARACTERISTICS: Exclusively polypoid, sol the Ceriantharia and Antipatharia into a itary or colonial eNIDARIA. Oral end ex separate subclass, the Ceriantipatharia. panded into oral disc which bears the mouth and Corallimorpharia are sometimes consid one or more rings of hollow tentacles. ered a suborder of Scleractinia. Approxi Stomodeum well developed, often with 1 or 2 mately 6,500 species of Anthozoa are siphonoglyphs. Gastrovascular cavity compart known. Of 93 species reported from Ber mentalized by radially arranged mesenteries. -
Animal Adaptations
Animal Adaptations The Animal Adaptations program at Hatfield Marine Science Center is designed to be a 50- minute lab-based program for 3rd-12th grade students that examines marine organisms from three different habitats (sandy beach, rocky shore and estuary) and explores the many ways they are adapted to their particular environment. This lab focuses on the adaptations of several groups of marine animals including Mollusks, Crustaceans, and Echinoderms, and investigates how they differ depending on whether they are found in a sandy beach, rocky shore, or estuary environment. Students will work in small groups with a variety of live animals, studying individual characteristics and how these organisms interact with their environment and one another. Background Information The Oregon Coast is made up of a series of rocky shores, sandy beaches, and estuaries, all of which are greatly affected by fluctuating tides. Many of these areas are intertidal and are alternately inundated by seawater and exposed to air, wind, and dramatic changes in temperature and salinity. High tide floods these areas with cold, nutrient laden seawater, bringing food to organisms that live there in the form of plankton and detritus. Low tides often expose these organisms to the dangers of predation and desiccation. In addition to tidal effects, organisms that inhabit sandy beaches and rocky shores also have to deal with the physical stresses of pounding waves. Because of these harsh conditions, organisms have developed special adaptations that not only help them to survive but thrive in these environments. An adaptation is a physical or behavioral trait that helps a plant or animal survive in a specific environment or habitat. -
Seashore the SANDYSEASHORE the Soilisinfertile, Anditisoften Windy, Andsalty
SEASHORE DESCRIPTION The seashore is an area fi lled with an interesting mix of unique plants and animals that have adapted to cope with this environment. Living on the edge of the sea is not easy. The soil is infertile, and it is often windy, dry and salty. THE SANDY SEASHORE Along a sandy shore there are no large rocks, algae or tidal pools. The sandy seashore can be divided into four general zones: Intertidal, Pioneer, Fixed Dune and Scrub Woodland. 1. Intertidal Zone: Between the low tide and the high tide mark is the intertidal zone. When the tide goes out the creatures living in this zone are left stranded. They have to endure the heat of the sun and the higher salinity of the water resulting from evaporation. Notice the many small holes on a sandy beach; they are the doorways to the homes of many animals which burrow under the sand where it is cooler. Some of Ecosystems of The Bahamas the creatures living in this zone are sea worms, sand fl eas and sand crabs. 2. Pioneer Zone: So named because it is where the fi rst plants to try to grow over sand. These plants must adapt to loose, shifting sand and poor soil. There is no protection from wind or salt spray. Plants here are usually low growing vines with waxy leaves. Some plants found in the pioneer zone are Purple seaside bean (C. rosea), Saltwort (Batis maritima), Goat's foot (Ipomea pes-caprae), and Sea purslane (Sesuvium portulacastrum). 3. Fixed Dune Zone: The next zone is the fi xed dune, so named because as the plants in the pioneer zone grip the sand around their roots and make the beach more stable, the sand mounds up into small humps or dunes. -
Tampa Bay Benthic Monitoring Program: Status of Middle Tampa Bay: 1993-1998
Tampa Bay Benthic Monitoring Program: Status of Middle Tampa Bay: 1993-1998 Stephen A. Grabe Environmental Supervisor David J. Karlen Environmental Scientist II Christina M. Holden Environmental Scientist I Barbara Goetting Environmental Specialist I Thomas Dix Environmental Scientist II MARCH 2003 1 Environmental Protection Commission of Hillsborough County Richard Garrity, Ph.D. Executive Director Gerold Morrison, Ph.D. Director, Environmental Resources Management Division 2 INTRODUCTION The Environmental Protection Commission of Hillsborough County (EPCHC) has been collecting samples in Middle Tampa Bay 1993 as part of the bay-wide benthic monitoring program developed to (Tampa Bay National Estuary Program 1996). The original objectives of this program were to discern the ―health‖—or ―status‖-- of the bay’s sediments by developing a Benthic Index for Tampa Bay as well as evaluating sediment quality by means of Sediment Quality Assessment Guidelines (SQAGs). The Tampa Bay Estuary Program provided partial support for this monitoring. This report summarizes data collected during 1993-1998 from the Middle Tampa Bay segment of Tampa Bay. 3 METHODS Field Collection and Laboratory Procedures: A total of 127 stations (20 to 24 per year) were sampled during late summer/early fall ―Index Period‖ 1993-1998 (Appendix A). Sample locations were randomly selected from computer- generated coordinates. Benthic samples were collected using a Young grab sampler following the field protocols outlined in Courtney et al. (1993). Laboratory procedures followed the protocols set forth in Courtney et al. (1995). Data Analysis: Species richness, Shannon-Wiener diversity, and Evenness were calculated using PISCES Conservation Ltd.’s (2001) ―Species Diversity and Richness II‖ software. -
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. -
Biodiversity and Distribution of Cyanobacteria at Dronning Maud Land, East Antarctica
ACyctaan oBboatcatneriicaa eMasat lAacnittaarnctai c3a3. 17-28 Málaga, 201078 BIODIVERSITY AND DISTRIBUTION OF CYANOBACTERIA AT DRONNING MAUD LAND, EAST ANTARCTICA Shiv Mohan SINGH1, Purnima SINGH2 & Nooruddin THAJUDDIN3* 1National Centre for Antarctic and Ocean Research, Headland Sada, Vasco-Da-Gama, Goa 403804, India. 2Department of Biotechnology, Purvanchal University, Jaunpur, India. 3Department of Microbiology, Bharathidasan University, Tiruchirappalli – 620 024, Tamilnadu, India. *Author for correspondence: [email protected] Recibido el 20 febrero de 2008, aceptado para su publicación el 5 de junio de 2008 Publicado "on line" en junio de 2008 ABSTRACT. Biodiversity and distribution of cyanobacteria at Dronning Maud Land, East Antarctica.The current study describes the biodiversity and distribution of cyanobacteria from the natural habitats of Schirmacher land, East Antarctica surveyed during 23rd Indian Antarctic Expedition (2003–2004). Cyanobacteria were mapped using the Global Positioning System (GPS). A total of 109 species (91 species were non-heterocystous and 18 species were heterocystous) from 30 genera and 9 families were recorded; 67, 86 and 14 species of cyanobacteria were identified at altitudes of sea level >100 m, 101–150 m and 398–461 m, respectively. The relative frequency and relative density of cyanobacterial populations in the microbial mats showed that 11 species from 8 genera were abundant and 6 species (Phormidium angustissimum, P. tenue, P. uncinatum Schizothrix vaginata, Nostoc kihlmanii and Plectonema terebrans) could be considered as dominant species in the study area. Key words. Antarctic, cyanobacteria, biodiversity, blue-green algae, Schirmacher oasis, Species distribution. RESUMEN. Biodiversidad y distribución de las cianobacterias de Dronning Maud Land, Antártida Oriental. En este estudio se describe la biodiversidad y distribución de las cianobacterias presentes en los hábitats naturales de Schirmacher, Antártida Oriental, muestreados durante la 23ª Expedición India a la Antártida (2003-2004). -
Marine Biological Investigations in the Bahamas 23. Description of the Littoral Zonation at Nine Bahamian Rocky-Shore Localities
Marine biological investigations in the Bahamas 23. Description of the littoral zonation at nine Bahamian rocky-shore localities Hans Brattström Brattström H. 1999. Description of the littoral zonation at nine Bahamian rocky-shore localities. SARSIA Sarsia 84:319-365. Nine typical, more or less vertical, rocky-shore localities were visited in April-May 1967, and one of these was revisited in March 1968. The topographies of the stations are described and illustrated, and the vertical zonation of their flora and fauna is documented. On the whole the flora and fauna at the stations investigated was fairly poor. At least 37 species of algae and 85 animal species were recorded, but only 15 algae and 71 animals could be identified to species. Most of the algae were too undeveloped or grazed down to permit a reliable identification. Only half as many species were found at these nine stations as were found on three almost horizontal beach-rock stations described in an earlier article. Whereas many of the latter lived in a system of cavities below the rocks, all species found on the nine vertical stations were exposed to waves and the hot midday sun. The common yellow, black, grey, and white zones typical of the Bahamas, were often well-devel- oped. Some algae and many of the animals formed distinct belts within these zones, the higher up the more exposed the rocks were. Though tides and exposure presumably are responsible for the general zonation pattern, it is likely that in the cirripeds and vermetids the way of food-intake determines their upper limit. -
Molluscs (Mollusca: Gastropoda, Bivalvia, Polyplacophora)
Gulf of Mexico Science Volume 34 Article 4 Number 1 Number 1/2 (Combined Issue) 2018 Molluscs (Mollusca: Gastropoda, Bivalvia, Polyplacophora) of Laguna Madre, Tamaulipas, Mexico: Spatial and Temporal Distribution Martha Reguero Universidad Nacional Autónoma de México Andrea Raz-Guzmán Universidad Nacional Autónoma de México DOI: 10.18785/goms.3401.04 Follow this and additional works at: https://aquila.usm.edu/goms Recommended Citation Reguero, M. and A. Raz-Guzmán. 2018. Molluscs (Mollusca: Gastropoda, Bivalvia, Polyplacophora) of Laguna Madre, Tamaulipas, Mexico: Spatial and Temporal Distribution. Gulf of Mexico Science 34 (1). Retrieved from https://aquila.usm.edu/goms/vol34/iss1/4 This Article is brought to you for free and open access by The Aquila Digital Community. It has been accepted for inclusion in Gulf of Mexico Science by an authorized editor of The Aquila Digital Community. For more information, please contact [email protected]. Reguero and Raz-Guzmán: Molluscs (Mollusca: Gastropoda, Bivalvia, Polyplacophora) of Lagu Gulf of Mexico Science, 2018(1), pp. 32–55 Molluscs (Mollusca: Gastropoda, Bivalvia, Polyplacophora) of Laguna Madre, Tamaulipas, Mexico: Spatial and Temporal Distribution MARTHA REGUERO AND ANDREA RAZ-GUZMA´ N Molluscs were collected in Laguna Madre from seagrass beds, macroalgae, and bare substrates with a Renfro beam net and an otter trawl. The species list includes 96 species and 48 families. Six species are dominant (Bittiolum varium, Costoanachis semiplicata, Brachidontes exustus, Crassostrea virginica, Chione cancellata, and Mulinia lateralis) and 25 are commercially important (e.g., Strombus alatus, Busycoarctum coarctatum, Triplofusus giganteus, Anadara transversa, Noetia ponderosa, Brachidontes exustus, Crassostrea virginica, Argopecten irradians, Argopecten gibbus, Chione cancellata, Mercenaria campechiensis, and Rangia flexuosa). -
Some Algae from Clipperton Island and the Danger Islands
Some Algae from Clipperton Island and the Danger Islands Item Type article Authors Dawson, E. Yale Download date 25/09/2021 22:34:01 Link to Item http://hdl.handle.net/1834/20635 SOME ALGAE FROM CLIPPERTON ISLAND AND THE DANGER ISLANDS By E. Yale Dawson Fig. 1. Rhizoclonium proftmdum sp. nov., from the type collection. A, Habit of a young plant attached to two filaments of older plants, shuwing rhizoids, altachment~ and branches, X 20. B, Detail of a single mature cell showing stratitied walls and reticu late chloroplast, X 75. SOME ALGAE FROM CLIPPERTON ISLAND AND THE DANGER ISLANDS By E. YALE DAwso:\, Through the cooperation of Dr. Carl L. Huhbs the writer has received through the Scripps Institution of Oceanography two interesting collection~ of tropical Paci fie benthic algae, one from remote Clipperton Island, the easternmost coral atoll in the Pacific, and one from a depth of about 200 feet at Pukapuka in the Danger Island~, l"nion Group, about 400 mile~ northea~t of Samoa. These are reported on helow in turn. I am grateful to Dr. Isabella Ahbott for reading and criticizing this paper. Clipperton Island The algal vegetation of this solitary atoll is known only from the papers of Taylor (1939) and Dawson (1957). These reports list only 17 entities, including 6 species of Cyanophyta and 3 unsatisfactorily identified species of other groups. The present collections, made principally hy Messrs. C. Limbaugh, T. Chess, A. Hambly and Miss M.·H. Sachet on the recent Scripps Institution Expedition (August.September, 1958), are more ample than any previously available, and permit us to add 30 marine species and 14 terrestrial and fresh water species, making a total of 61 known from the atoll. -
Resultados - Capítulo 2 120
Resultados - Capítulo 2 120 Resultados - Capítulo 2 121 Figure 32 – Electrophysiological screening of BcsTx1 (0.5 µM) on several cloned voltage–gated potassium channel isoforms belonging to different subfamilies. Representative traces under control and after application of 0.5 µM of BcsTx1 are shown. The asterisk indicates steady-state current traces after toxin application. The dotted line indicates the zero-current level. This screening shows that BcsTx1 selectively blocks KV1.x channels at a concentration of 0.5 µM. Resultados - Capítulo 2 122 Resultados - Capítulo 2 123 Figure 33 – Inhibitory effects of BcsTx2 (3 µM) on 12 voltage-gated potassium channels isoforms expressed in X. laevis oocytes. Representative whole-cell current traces in the absence and in the presence of 3 µM BcsTx2 are shown for each channel. The dotted line indicates the zero-current level. The * indicates steady state current traces after application of 3 µM BcsTx2. This screening carried out on a large number of KV channel isoforms belonging to different subfamilies shows that BcsTx2 selectively blocks Shaker channels subfamily. In order to characterize the potency and selectivity profile, concentration- response curves were constructed for BcsTx1. IC50 values yielded 405 ± 20.56 nanomolar (nM) for rKv1.1, 0.03 ± 0.006 nM for rKv1.2, 74.11 ± 20.24 nM for hKv1.3, 1.31 ± 0.20 nM for rKv1.6 and 247.69 ± 95.97 nM for Shaker IR (Figure 34A and Table 7). A concentration–response curve was also constructed to determine the concentration at which BcsTx2 blocked half of the channels. The IC50 values calculated are 14.42 ± 2.61 nM for rKV1.1, 80.40 ± 1.44 nM for rKV1.2, 13.12 ± 3.29 nM for hKV1.3, 7.76 ± 1.90 nM for rKV1.6, and 49.14 ± 3.44 nM for Shaker IR (Figure 34B and Table 7). -
Asexual Reproduction and Molecular Systematics of the Sea Anemone Anthopleura Krebsi (Actiniaria: Actiniidae)
Rev. Biol. Trop. 51(1): 147-154, 2003 www.ucr.ac.cr www.ots.ac.cr www.ots.duke.edu Asexual reproduction and molecular systematics of the sea anemone Anthopleura krebsi (Actiniaria: Actiniidae) Paula Braga Gomes1, Mauricio Oscar Zamponi2 and Antonio Mateo Solé-Cava3 1. LAMAMEBEN, Departamento de Zoologia-CCB, Universidade Federal de Pernambuco, Av. Prof. Moraes Rego 1235, Cidade Universitária, Recife-Pe, 50670-901, Brazil. [email protected] 2. Laboratorio de Biología de Cnidarios, Depto. Cs. Marinas, FCEyN, Funes, 3250 (7600), Mar del Plata - Argentina. CONICET Research. 3. Molecular Biodiversity Lab. Departamento de Genética, Instituto de Biologia, Bloco A, CCS, Universidade Federal do Rio de Janeiro, Ilha do Fundão, CEP 21941-590, Rio de Janeiro, RJ, Brazil and Port Erin Marine Laboratory, University of Liverpool, Isle of Man, IM9 6JA, UK. Received 26-VI-2001. Corrected 02-V-2002. Accepted 07-III-2003. Abstract: In this paper we use allozyme analyses to demonstrate that individuals in Anthopleura krebsi aggre- gates are monoclonal. Additionally, sympatric samples of the red and the green colour-morphs of A. krebsi from Pernambuco, Brazil were genetically compared and no significant differences were observed between them (gene identity= 0.992), indicating that they do not belong to different biological species. All individuals within aggregates of the green colour-morph were found to be identical over the five polymorphic loci analysed. Such results would be extremely unlikely (P<10-11) if the individuals analysed had been generated through sexual reproduction, thus confirming the presence of asexual reproduction in this species. Key words: Cnidaria, allozymes, clones, fission, molecular systematics. -
Genus Panopeus H. Milne Edwards, 1834 Key to Species [Based on Rathbun, 1930, and Williams, 1983] 1
610 Family Xanthidae Genus Panopeus H. Milne Edwards, 1834 Key to species [Based on Rathbun, 1930, and Williams, 1983] 1. Dark color of immovable finger continued more or less on palm, especially in males. 2 Dark color of immovable finger not continued on palm 7 2. (1) Outer edge of fourth lateral tooth longitudinal or nearly so. P. americanus Outer edge of fourth lateral tooth arcuate 3 3. (2) Edge of front thick, beveled, and with transverse groove P. bermudensis Edge of front if thick not transversely grooved 4 4. (3) Major chela with cusps of teeth on immovable finger not reaching above imaginary straight line drawn between tip and angle at juncture of finger with anterior margin of palm (= length immovable finger) 5 Major chela with cusps of teeth near midlength of immovable finger reaching above imaginary straight line drawn between tip and angle at juncture of finger with anterior margin of palm (= length immovable finger) 6 5. (4) Coalesced anterolateral teeth 1-2 separated by shallow rounded notch, 2 broader than but not so prominent as 1; 4 curved forward as much as 3; 5 much smaller than 4, acute and hooked forward; palm with distance between crest at base of movable finger and tip of cusp lateral to base of dactylus 0.7 or less length of immovable finger P. herbstii Coalesced anterolateral teeth 1-2 separated by deep rounded notch, adjacent slopes of 1 and 2 about equal, 2 nearly as prominent as 1; 4 not curved forward as much as 3; 5 much smaller than 4, usually projecting straight anterolaterally, sometimes slightly hooked; distance between crest of palm and tip of cusp lateral to base of movable finger 0.8 or more length of immovable finger P.