Non-Native Seaweeds in the Rocky Intertidal Zone in the Little Corona
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Pelvetia Canaliculata Channel Wrack Ecology and Similar Identification Species
Ecology and Similar species identification Found slightly High shore alga higher than often forming a Fucus spiralis. clear zone on Fronds in more sheltered F.spiralis are shores. flat and twisted. Evenly forked fronds up to 15cm long that are rolled to give a channel on one side. Pelvetia canaliculata Channel Wrack Ecology and Similar identification species High shore alga Fucus often forming vesiculosus a clear zone which has below Pelvetia distinctive air on more bladders sheltered shores. Fronds in F.spiralis are flat and Fucus spiralis twisted and up Spiral Wrack to 20cm long. NO air bladders. Ecology and Similar identification species Most Fucus characteristic vesiculosus mid shore which has alga in shelter. paired circular air Leathery bladders fronds up to a metre long, no mid-rib and single egg-shaped Ascophyllum nodosum air-bladders Egg or Knotted Wrack Ecology and Similar identification species The F. spiralis characteristic and alga of the A.nodosum mid-shore in moderate exposure. The fronds have a prominent mid-rib and Fucus vesiculosus paired air Bladder Wrack bladders. Ecology and Similar identification species Can be Other Fucus abundant in species the low and lower mid- shore. Fronds have a serrated edge. Fucus serratus Serrated Wrack. Ecology and Similar species identification. This is the Laminaria commonest of hyperborea, the the kelps and can forest kelp, dominate around which has a low water. Each round cross plant may reach section to the 1.5m long. stem and stands erect at The stem has an low tide. oval cross section that causes the plant to droop over at low water. -
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. -
Appendix 1 Table A1
OIK-00806 Kordas, R. L., Dudgeon, S., Storey, S., and Harley, C. D. G. 2014. Intertidal community responses to field-based experimental warming. – Oikos doi: 10.1111/oik.00806 Appendix 1 Table A1. Thermal information for invertebrate species observed on Salt Spring Island, BC. Species name refers to the species identified in Salt Spring plots. If thermal information was unavailable for that species, information for a congeneric from same region is provided (species in parentheses). Response types were defined as; optimum - the temperature where a functional trait is maximized; critical - the mean temperature at which individuals lose some essential function (e.g. growth); lethal - temperature where a predefined percentage of individuals die after a fixed duration of exposure (e.g., LT50). Population refers to the location where individuals were collected for temperature experiments in the referenced study. Distribution and zonation information retrieved from (Invertebrates of the Salish Sea, EOL) or reference listed in entry below. Other abbreviations are: n/g - not given in paper, n/d - no data for this species (or congeneric from the same geographic region). Invertebrate species Response Type Temp. Medium Exposure Population Zone NE Pacific Distribution Reference (°C) time Amphipods n/d for NE low- many spp. worldwide (Gammaridea) Pacific spp high Balanus glandula max HSP critical 33 air 8.5 hrs Charleston, OR high N. Baja – Aleutian Is, Berger and Emlet 2007 production AK survival lethal 44 air 3 hrs Vancouver, BC Liao & Harley unpub Chthamalus dalli cirri beating optimum 28 water 1hr/ 5°C Puget Sound, WA high S. CA – S. Alaska Southward and Southward 1967 cirri beating lethal 35 water 1hr/ 5°C survival lethal 46 air 3 hrs Vancouver, BC Liao & Harley unpub Emplectonema gracile n/d low- Chile – Aleutian Islands, mid AK Littorina plena n/d high Baja – S. -
Balanus Glandula Class: Multicrustacea, Hexanauplia, Thecostraca, Cirripedia
Phylum: Arthropoda, Crustacea Balanus glandula Class: Multicrustacea, Hexanauplia, Thecostraca, Cirripedia Order: Thoracica, Sessilia, Balanomorpha Acorn barnacle Family: Balanoidea, Balanidae, Balaninae Description (the plate overlapping plate edges) and radii Size: Up to 3 cm in diameter, but usually (the plate edge marked off from the parietes less than 1.5 cm (Ricketts and Calvin 1971; by a definite change in direction of growth Kozloff 1993). lines) (Fig. 3b) (Newman 2007). The plates Color: Shell usually white, often irregular themselves include the carina, the carinola- and color varies with state of erosion. Cirri teral plates and the compound rostrum (Fig. are black and white (see Plate 11, Kozloff 3). 1993). Opercular Valves: Valves consist of General Morphology: Members of the Cirri- two pairs of movable plates inside the wall, pedia, or barnacles, can be recognized by which close the aperture: the tergum and the their feathery thoracic limbs (called cirri) that scutum (Figs. 3a, 4, 5). are used for feeding. There are six pairs of Scuta: The scuta have pits on cirri in B. glandula (Fig. 1). Sessile barna- either side of a short adductor ridge (Fig. 5), cles are surrounded by a shell that is com- fine growth ridges, and a prominent articular posed of a flat basis attached to the sub- ridge. stratum, a wall formed by several articulated Terga: The terga are the upper, plates (six in Balanus species, Fig. 3) and smaller plate pair and each tergum has a movable opercular valves including terga short spur at its base (Fig. 4), deep crests for and scuta (Newman 2007) (Figs. -
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). -
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Appendix C: An Analysis of Three Shellfish Assemblages from Tsʼishaa, Site DfSi-16 (204T), Benson Island, Pacific Rim National Park Reserve of Canada by Ian D. Sumpter Cultural Resource Services, Western Canada Service Centre, Parks Canada Agency, Victoria, B.C. Introduction column sampling, plus a second shell data collect- ing method, hand-collection/screen sampling, were This report describes and analyzes marine shellfish used to recover seven shellfish data sets for investi- recovered from three archaeological excavation gating the siteʼs invertebrate materials. The analysis units at the Tseshaht village of Tsʼishaa (DfSi-16). reported here focuses on three column assemblages The mollusc materials were collected from two collected by the researcher during the 1999 (Unit different areas investigated in 1999 and 2001. The S14–16/W25–27) and 2001 (Units S56–57/W50– source areas are located within the village proper 52, S62–64/W62–64) excavations only. and on an elevated landform positioned behind the village. The two areas contain stratified cultural Procedures and Methods of Quantification and deposits dating to the late and middle Holocene Identification periods, respectively. With an emphasis on mollusc species identifica- The primary purpose of collecting and examining tion and quantification, this preliminary analysis the Tsʼishaa shellfish remains was to sample, iden- examines discarded shellfood remains that were tify, and quantify the marine invertebrate species collected and processed by the site occupants for each major stratigraphic layer. Sets of quantita- for approximately 5,000 years. The data, when tive information were compiled through out the reviewed together with the recovered vertebrate analysis in order to accomplish these objectives. -
JMS 70 1 031-041 Eyh003 FINAL
PHYLOGENY AND HISTORICAL BIOGEOGRAPHY OF LIMPETS OF THE ORDER PATELLOGASTROPODA BASED ON MITOCHONDRIAL DNA SEQUENCES TOMOYUKI NAKANO AND TOMOWO OZAWA Department of Earth and Planetary Sciences, Nagoya University, Nagoya 464-8602,Japan (Received 29 March 2003; accepted 6June 2003) ABSTRACT Using new and previously published sequences of two mitochondrial genes (fragments of 12S and 16S ribosomal RNA; total 700 sites), we constructed a molecular phylogeny for 86 extant species, covering a major part of the order Patellogastropoda. There were 35 lottiid, one acmaeid, five nacellid and two patellid species from the western and northern Pacific; and 34 patellid, six nacellid and three lottiid species from the Atlantic, southern Africa, Antarctica and Australia. Emarginula foveolata fujitai (Fissurellidae) was used as the outgroup. In the resulting phylogenetic trees, the species fall into two major clades with high bootstrap support, designated here as (A) a clade of southern Tethyan origin consisting of superfamily Patelloidea and (B) a clade of tropical Tethyan origin consisting of the Acmaeoidea. Clades A and B were further divided into three and six subclades, respectively, which correspond with geographical distributions of species in the following genus or genera: (AÍ) north eastern Atlantic (Patella ); (A2) southern Africa and Australasia ( Scutellastra , Cymbula-and Helcion)', (A3) Antarctic, western Pacific, Australasia ( Nacella and Cellana); (BÍ) western to northwestern Pacific (.Patelloida); (B2) northern Pacific and northeastern Atlantic ( Lottia); (B3) northern Pacific (Lottia and Yayoiacmea); (B4) northwestern Pacific ( Nipponacmea); (B5) northern Pacific (Acmaea-’ânà Niveotectura) and (B6) northeastern Atlantic ( Tectura). Approximate divergence times were estimated using geo logical events and the fossil record to determine a reference date. -
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. -
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. -
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. -
Malacofauna Marina Del Parque Nacional “Los Caimanes”, Villa Clara, Cuba
Tesis de Diploma Malacofauna Marina del Parque Nacional “Los Caimanes”, Villa Clara, Cuba. Autora: Liliana Olga Quesada Pérez Junio, 2011 Universidad Central “Marta Abreu” de Las Villas Facultad Ciencias Agropecuaria TESIS DE DIPLOMA Malacofauna marina del Parque Nacional “Los Caimanes”, Villa Clara, Cuba. Autora: Liliana Olga Quesada Pérez Tutor: M. C. Ángel Quirós Espinosa Investigador Auxiliar y Profesor Auxiliar [email protected] Centro de Estudios y Servicios Ambientales, CITMA-Villa Clara Carretera Central 716, Santa Clara Consultante: Dr.C. José Espinosa Sáez Investigador Titular Instituto de Oceanología Junio, 2011 Pensamiento “La diferencia entre una mala observación y una buena, es que la primera es errónea y la segunda es incompleta.” Van Hise Dedicatoria Dedicatoria: A mis padres, a Yandy y a mi familia: por las innumerables razones que me dan para vivir, y por ser fuente de inspiración para mis metas. Agradecimientos Agradecimientos: Muchos son los que de alguna forma contribuyeron a la realización de este trabajo, todos saben cuánto les agradezco: Primero quiero agradecer a mis padres, que aunque no estén presentes sé que de una forma u otra siempre estuvieron allí para darme todo su amor y apoyo. A mi familia en general: a mi abuela, hermano, a mis tíos por toda su ayuda y comprensión. A Yandy y a su familia que han estado allí frente a mis dificultades. Agradecer a mi tutor el M.Sc. Ángel Quirós, a mi consultante el Dr.C. José Espinosa y a la Dra.C. María Elena, por su dedicación para el logro de esta tesis. A mis compañeros de grupo por estos cinco años que hemos compartidos juntos, que para mí fueron inolvidables. -
UC Berkeley UC Berkeley Previously Published Works
UC Berkeley UC Berkeley Previously Published Works Title Twelve thousand recent patellogastropods from a northeastern Pacific latitudinal gradient. Permalink https://escholarship.org/uc/item/21h48289 Authors Kahanamoku, Sara Hull, Pincelli Lindberg, David et al. Publication Date 2018-01-09 DOI 10.1038/sdata.2017.197 Peer reviewed eScholarship.org Powered by the California Digital Library University of California www.nature.com/scientificdata OPEN Data Descriptor: Twelve thousand recent patellogastropods from a northeastern Pacific latitudinal gradient 13 2017 Received: June 1 2 1 2 1 3 Sara S. Kahanamoku , , Pincelli M. Hull , David R. Lindberg , Allison Y. Hsiang , , Accepted: 17 October 2017 4 2 Erica C. Clites & Seth Finnegan Published: 9 January 2018 Body size distributions can vary widely among communities, with important implications for ecological dynamics, energetics, and evolutionary history. Here we present a dataset of body size and shape for 12,035 extant Patellogastropoda (true limpet) specimens from the collections of the University of California Museum of Paleontology, compiled using a novel high-throughput morphometric imaging method. These specimens were collected over the past 150 years at 355 localities along a latitudinal gradient ranging from Alaska to Baja California, Mexico and are presented here with individual images, 2D outline coordinates, and 2D measurements of body size and shape. This dataset provides a resource for assemblage-scale macroecological questions and documents the size and diversity of recent patellogastropods in the northeastern Pacific. Design Type(s) observation design • image analysis objective Measurement Type(s) morphology Technology Type(s) digital camera Factor Type(s) geographic location Patellogastropoda • State of California • State of Baja California • State of Sample Characteristic(s) Washington • Mexico • State of Alaska • State of Oregon • Province of British Columbia 1 2 Yale University, Department of Geology & Geophysics, New Haven, CT 06511, USA.