The Diel Dynamics of Ciliate Community in a Tide-Pool
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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). -
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. -
Dam Effects on Low-Tide Channel Pools and Fish Use of Estuarine Habitat
Beaver in Tidal Marshes: Dam Effects on Low-Tide Channel Pools and Fish Use of Estuarine Habitat W. Gregory Hood Wetlands Official Scholarly Journal of the Society of Wetland Scientists ISSN 0277-5212 Wetlands DOI 10.1007/s13157-012-0294-8 1 23 Your article is protected by copyright and all rights are held exclusively by Society of Wetland Scientists. This e-offprint is for personal use only and shall not be self- archived in electronic repositories. If you wish to self-archive your work, please use the accepted author’s version for posting to your own website or your institution’s repository. You may further deposit the accepted author’s version on a funder’s repository at a funder’s request, provided it is not made publicly available until 12 months after publication. 1 23 Author's personal copy Wetlands DOI 10.1007/s13157-012-0294-8 ARTICLE Beaver in Tidal Marshes: Dam Effects on Low-Tide Channel Pools and Fish Use of Estuarine Habitat W. Gregory Hood Received: 31 August 2011 /Accepted: 16 February 2012 # Society of Wetland Scientists 2012 Abstract Beaver (Castor spp.) are considered a riverine or can have multi-decadal or longer effects on river channel form, lacustrine animal, but surveys of tidal channels in the Skagit riverine and floodplain wetlands, riparian vegetation, nutrient Delta (Washington, USA) found beaver dams and lodges in the spiraling, benthic community structure, and the abundance and tidal shrub zone at densities equal or greater than in non-tidal productivity of fish and wildlife (Jenkins and Busher 1979; rivers. Dams were typically flooded by a meter or more during Naiman et al. -
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. -
Spatial and Temporal Patterns of Salinity and Temperature at an Intertidal Groundwater Seep
Estuarine, Coastal and Shelf Science 72 (2007) 283e298 www.elsevier.com/locate/ecss Spatial and temporal patterns of salinity and temperature at an intertidal groundwater seep Ryan K. Dale*, Douglas C. Miller University of Delaware, College of Marine and Earth Studies, 700 Pilottown Road, Lewes, DE 19958, USA Received 9 June 2006; accepted 31 October 2006 Available online 22 December 2006 Abstract Spatial and temporal patterns at an intertidal groundwater seep at Cape Henlopen, Delaware, were characterized using a combination of pore water salinity and sediment temperature measurements. Pore water salinity maps, both on a small scale (resolution of 0.1 m over a 1.25 m2 area) and large scale (1e5 m over a 1710 m2 area) showed reduced pore water salinities to as low as one-sixth seawater strength in a region 0e6m from the intertidal beach slope break. In this region, there was substantial spatial variability in pore water salinity at all measured scales (0.1e 90 m) alongshore. At À10 cm sediment depth, pore water salinity ranged from 6 to 24 in less than 1 m horizontally. To further characterize spatial patterns in discharge, we used novel temperature probes during summer low tides and found temperatures were much lower in a ground- water seep than the nearby sediment, as much as 8e9 C cooler at À30 cm sediment depth. Measurements over time using temperature loggers showed that despite strong tidal and diel forcing on surficial sediment temperatures, thermal anomalies due to groundwater discharge persisted over several-day sampling periods and were strongest at À20 and À30 cm depth. -
Okeanos Explorer Rov Dive Summary
OKEANOS EXPLORER ROV DIVE SUMMARY Site Name GB907 Expedition Kelley Elliott/ Coordinator/ Brian Bingham ROV Lead Stephanie Farrington (Biology) Science Team Leads Jamie Austin (Geology) General Area Gulf of Mexico Descriptor Cruise Season Leg Dive Number ROV Dive Name EX1402 3 DIVE02 ROV: Deep Discoverer Equipment Deployed Camera Platform: Seirios CTD Depth Altitude Scanning Sonar USBL Position Heading ROV Measurements Pitch Roll HD Camera 1 HD Camera 2 Low Res Cam 1 Low Res Cam 2 Low Res Cam 3 Low Res Cam 4 Low Res Cam 2 Equipment N/A Malfunctions Dive Summary: EX1402L3_DIVE02 ^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^ In Water at: 2014-04-13T13:45:38.439000 27°, 05.899' N ; 092°, 37.310' W Out Water at: 2014-04-13T19:12:34.841000 27°, 05.096' N ; 092°, 36.588' W ROV Dive Summary Off Bottom at: 2014-04-13T18:24:04.035000 (From processed ROV 27°, 05.455' N ; 092°, 36.956' W data) On Bottom at: 2014-04-13T14:31:16.507000 27°, 05.519' N ; 092°, 37.099' W Dive duration: 5:26:56 Bottom Time: 3:52:47 Max. depth: 1266.7 m Special Notes Primary Jamie Austin, EX, UT Austin, [email protected] Stephanie Farrington, EX, HBOI/FAU, [email protected] Andrea Quattrini, Temple, Temple, [email protected] Scientists Involved Bernie Ball, Duke, Duke, [email protected] (please provide name / Brian Kinlan, NOAA NMFS, [email protected] location / affiliation / email) Carolyn Ruppel, Woods Hole, USGS, [email protected] Erik Cordes, Temple, Temple, [email protected] Larry Mayer, UNH, UNH CCOM, [email protected] Michael Vecchione, -
A Guide to the Side of the Sea Lessons: Pre-Trip Activities Underwater Viewers Students Can Make Underwater Viewers for Studying Intertidal Life
Lessons The following lessons are grouped into three categories: pre-trip, during the trip, and post-trip. If you do pre-trip lessons, plan how to refer to them while on the trip. If you plan to do any of the post-trip lessons, be aware of ways to prepare the students while on the trip by making observations or asking questions. Each category is further divided into Hands-On Activities and Other Activities of various types. California State Content Standards that can easily be addressed through the lessons are referenced by subject and number. See pages 143–146 for abbreviated summaries of the standards. Some of the hands-on activities are intended to be discovery activities (experiments) in which the students don’t know the answers ahead of time. The teacher should try to facilitate the students’ discoveries rather than telling them what to expect. Whenever possible, be a guide on the side! Also . it is HIGHLY recommended that the teacher: • Try out all experiments before having students do them. • Enlist the help of parent volunteers before, during, and after experiments. • Feel free to adapt, expand, or alter experiments to suit your needs, student needs, and resources. Hands-on or “lab” type activities are presented in a detailed lesson plan format. A few “other” activities are given as examples, but the resources in the curriculum of the resources section (p. 158) give many additional worthwhile activities. Many of the lessons begin before the field trip and continue with activities to be done while at the coast. Others that are listed as pre-trip can also be done after the trip. -
Explore a Tide Pool Lesson Plan
Waldo County 4-H Program 992 Waterville Rd, Waldo, ME 04915 (207) 342-5971 Ext (800) 287-1426 toll free in Maine (800) 287-8957 TDD [email protected] [email protected] Putting knowledge to work with the people of Maine Explore a Tide Pool Purpose of activity: The purpose of this activity is to explore tide pools along the intertidal coastline. In this activity, youth will explore what a tide pool is and what type of plants and animals live there. What is a tide pool? Tide pools are rocky pools on the seashore that are filled with seawater when the ocean tide goes out, creating low tide. Tide pools often have plants and animals living in the pool that have to adapt to environmental extremes like the hot sun on a summer day and predators such as seagulls. Plants that grow in tide pools include seaweed, algae, and sea grass. Animals that live in tide pools might be periwinkles, crabs, starfish, barnacles, and more. Materials: An interactive On-line Tide Pool experience • Green Crab discovery with Tidepool Tim, of your choice. Gulf of Maine Inc • PBS Interactivities: Exploring Tide Pools • Intertidal snails with Tidepool Tim, Gulf • What is a Tide Pool? of Maine Inc • Tide Pool Ocean Adventure Children or • Tidal Pool Scavenger Hunt Handout Kids Activity • Ecosystem of California: Intertidal Instructions: 1. Take an adventure and explore tide pools. Choose one interactive on-line resource to view or take your family on an adventure to the nearest coastline and look for tidepools. If you and your family are preparing for a beach trip, make sure you bring appropriate beach clothes, shows with non-slip tread, and sun protection. -
Diversity of Intertidal Macroalgae Increases with Nitrogen Loading by Invertebrates
UC Davis UC Davis Previously Published Works Title Diversity of intertidal macroalgae increases with nitrogen loading by invertebrates Permalink https://escholarship.org/uc/item/47t5n0vn Journal Ecology, 85(10) ISSN 0012-9658 Authors Bracken, Matthew E S Nielsen, K J Publication Date 2004-10-01 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Ecology, 85(10), 2004, pp. 2828±2836 q 2004 by the Ecological Society of America DIVERSITY OF INTERTIDAL MACROALGAE INCREASES WITH NITROGEN LOADING BY INVERTEBRATES MATTHEW E. S. BRACKEN1,3 AND KARINA J. NIELSEN2 1Department of Zoology, Oregon State University, Corvallis, Oregon 97331-2914 USA 2Sonoma State University, Department of Biology, Rohnert Park, California 94928 USA Abstract. Many ecological phenomena are characterized by context dependency, and the relationship between diversity and productivity is no exception. We examined the re- lationship between macroalgal diversity and nutrient availability by evaluating the effects of reduced nutrients and their subsequent replacement via local-scale nutrient loading in tide pools. Macroalgae in Oregon coast high-intertidal pools have evolved in a nitrate-rich upwelling ecosystem, but instead of settling on low-intertidal reefs (where algae are often immersed in nutrient-rich nearshore waters) these individuals have colonized high-zone pools, where they are isolated from the ocean for extended periods of time and are subjected to extended periods of nitrate depletion. In some pools, this nutrient stress was ameliorated by a positive interaction: the excretion of ammonium by invertebrates. We conducted ex- perimental manipulations to quantify invertebrate-mediated ammonium loading and ma- croalgal ammonium uptake in high-intertidal pools. -
Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds
Appendix 5.4, Page 1 Appendix 5.4 Marine and Coastline Habitats Featured Species-associated Intertidal Habitats: Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds A swath of intertidal habitat occurs wherever the ocean meets the shore. At 44,000 miles, Alaska’s shoreline is more than double the shoreline for the entire Lower 48 states (ACMP 2005). This extensive shoreline creates an impressive abundance and diversity of habitats. Five physical factors predominantly control the distribution and abundance of biota in the intertidal zone: wave energy, bottom type (substrate), tidal exposure, temperature, and most important, salinity (Dethier and Schoch 2000; Ricketts and Calvin 1968). The distribution of many commercially important fishes and crustaceans with particular salinity regimes has led to the description of “salinity zones,” which can be used as a basis for mapping these resources (Bulger et al. 1993; Christensen et al. 1997). A new methodology called SCALE (Shoreline Classification and Landscape Extrapolation) has the ability to separate the roles of sediment type, salinity, wave action, and other factors controlling estuarine community distribution and abundance. This section of Alaska’s CWCS focuses on 3 main types of intertidal habitat: rocky intertidal, mudflats and beaches, and eelgrass beds. Tidal marshes, which are also intertidal habitats, are discussed in the Wetlands section, Appendix 5.3, of the CWCS. Rocky intertidal habitats can be categorized into 3 main types: (1) exposed, rocky shores composed of steeply dipping, vertical bedrock that experience high-to- moderate wave energy; (2) exposed, wave-cut platforms consisting of wave-cut or low-lying bedrock that experience high-to-moderate wave energy; and (3) sheltered, rocky shores composed of vertical rock walls, bedrock outcrops, wide rock platforms, and boulder-strewn ledges and usually found along sheltered bays or along the inside of bays and coves. -
Topographic Complexity and Landscape Temperature Patterns Create a Dynamic Habitat Structure on a Rocky Intertidal Shore
Vol. 428: 1–12, 2011 MARINE ECOLOGY PROGRESS SERIES Published May 3 doi: 10.3354/meps09124 Mar Ecol Prog Ser OPENPEN ACCESSCCESS FEATURE ARTICLE Topographic complexity and landscape temperature patterns create a dynamic habitat structure on a rocky intertidal shore Justin J. Meager*, Thomas A. Schlacher, Mahdi Green Faculty of Science, Health and Education, University of the Sunshine Coast, Maroochydore DC, Queensland 4558, Australia ABSTRACT: Habitat complexity is a fundamental dri- ver of ecosystem structure and function. Rocky inter- tidal shores are the classic model system for investi - gating theoretical and mechanistic models of habitat complexity, because the structural topography is largely biologically independent and stable over time. In the present study, we investigate how static (topographic complexity and heterogeneity) and dynamic (tempera- ture landscape) components of habitat structure influ- ence the abundance and body-size distribution of in - vertebrates on a rocky shore. Using a novel approach that included high-resolution 3D fractal surface and temperature measurements, we show that topographic complexity, temperature landscape and habitat hetero- geneity had largely independent effects on species Dynamic and static habitat traits determine associations of abundance and body size. Invertebrate abundance was invertebrates on a rocky shore: limpets Cellana tramoserica associated with temperature landscape in 7 of 11 spe- under a ledge. cies, while variation in body-size was mostly driven by Photo: J. Meager fractal topography in 7 of 10 species. Overall, the body size−abundance relationship was not influenced by habitat structure, indicating that the effects of habitat and conservation planning (e.g. Banks & Skilleter structure on body size and abundance were largely 2007, McArthur et al. -
Overview of the Rocky Intertidal Systems of Southern California Mark M
Overview of the Rocky Intertidal Systems of Southern California Mark M. Littler Department of Ecology and Evolutionary Biology, University of California, Irvine, California 92717 INTRODUCTION The Southern California Bight (Fig. 1) has been defined (SCCWRP 1973) as the open embayment of the Pacific Ocean bounded on the east by the North American coastline extending from Point Conception, California, to Cabo Colnett, Baja California, Mexico, and on the west by the California Current. The climate of the Southern California Bight has been amply studied in quantitative terms and is relatively well known (for physical, air, and seawater data, see Kimura 1974). Wind conditions are extremely important in that major reversals occur predominantly throughout late fall and winter. This results in strong, hot, and dry "Santa Ana" winds from the inland desert regions at the time of low tides during the daylight hours, thereby causing extreme heating, desiccation, and insolation stress to intertidal organisms. Another important ecological factor is the protection of certain mainland shores and the mainland sides of islands from open ocean swell and storm waves. This leads to a higher wave-energy regime on the unprotected outer island shores with marked effects on their biological communities. Nearly all of the southern California mainland coastline is protected to some degree by the outlying islands (Ricketts, Calvin, and Hedgpeth 1968). The only mainland sites receiving direct westerly swell are near the cities of Los Angeles and San Diego. A number of substrate types were present among the 10 rocky intertidal habitats studied (Fig. 1), ranging from hard, irregular flow breccia to smooth sandstone or siltstone.