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Between the Tides Chapter 11
Copyright © 2016 McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education.
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Intertidal Zone The intertidal zone is the area between the mean low tide and mean high tide By contrast, the subtidal zone is the area that is always submerged The intertidal zone will be exposed during low tide
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Intertidal Substrates
Substrate - type of bottom Intertidal zone substrate can be rocky or soft bottom Soft bottoms can vary from sand to silt or a mixture (mud) Rocky substrate can vary as to the type of rock and the slope angle
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Intertidal Zone Organisms
Epifauna – organisms that live on the surface of the substrate (ex: mud snails on soft bottoms, barnacles on hard substrates) Infauna – organisms that live in the substrate (ex: clams burrowing in soft bottoms) Meiofauna – organisms that are so small that they live between the grains of soft substrate These organisms can be sessile or motile
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Challenges Associated with the Intertidal
Due to the exposure to air, organisms face a variety of challenges, including: Desiccation (water loss) Temperature changes (can be extreme) Salinity changes (can be extreme) Interrupted feeding Wave action and tides Oxygen availability and build-up of CO2 at low tide Limited space
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Desiccation When exposed, organisms must deal with potential water loss Water loss is more pronounced on hot, dry, or windy days Organisms can deal with the potential water loss by hiding or “clamming up”
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Desiccation Hiding may involve moving to a tide pool or an area with more moisture (motile organisms) Hiding may also mean that some organisms only live in areas where moisture will remain when the tide is out (such as crevices in rocks or shallow spots in soft bottoms)
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Desiccation “Clamming up” consists of closing shells or otherwise walling yourself off from the environment to conserve moisture + moisture can be conserved - no exchange of gases or feeding occurs
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Temperature The wide range of temperatures that must be tolerated by organisms in the intertidal can be severe Some organisms have mechanisms to help stay cool
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Animals hide under algal mats
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White shells reflect radiation back away from animals
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Changing Salinity Salinity can change dramatically due to temperatures or weather. Normal ocean salinity is ~ ppt. Estuarine salinity normally varies between 5 ppt and 30 ppt. Organisms in the intertidal are normally euryhaline (eury = broad; haline = salt) subtidal organisms are normally stenohaline (steno = narrow)
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Changing Salinity Salinity may begin at /00 and climb dramatically during the day due to water loss when the intertidal is exposed. Salinity may also drop during the day due to a sudden influx of freshwater provided by a passing thunderstorm. A salinity change of possibly 20 0/00 or more combined with a temperature change of 40 degrees or more may occur
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Interrupted Feeding If an organisms “clams up,” feeding will stop
Feeding will also cease for filter feeders when exposed to air A few organisms such as snails can still feed during low tide by scraping algae off surfaces For communities with semidiurnal tides, an animal could spend nearly half of their day un-submerged and not feeding.
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Wave Action Wave exposure can be a problem for intertidal organisms
Rocky shores are often exposed to significant wave action
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Oxygen Availability Oxygen can be exhausted if an organism “clams up” during low tide It can also be exhausted in tide pools if high density of organism, particularly algae at night (no photosynthesis) Carbon dioxide can also build up Some organisms have evolved the ability to exchange gases in both air and water This is infauna, but O2 related
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Limited Space In some intertidal communities, space may be limited
This is particularly true in the rocky intertidal, where surface area is limited Space can also be limited in soft bottomed communities, where many organisms select hard substrates such as oyster reefs to prevent being washed away
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Zonation in the Intertidal
Zonation in the intertidal consists of upper intertidal (most exposed) to middle and lower intertidal (least exposed).
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Zonation in the Intertidal
Competition will be greater in the lower intertidal because it is the least extreme of the zones: exposed to a lesser degree than the upper intertidal The lower intertidal always has more species for the same reason (although species will vary greatly by location)
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Competition Some species are better competitors than others and will exclude others if the community is left undisturbed If a habitat is disturbed, organisms move in and are excluded in a predictable pattern known as ecological succession The climax community (end result) will eventually form when the community is undisturbed for a long period of time
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Predation Predation by keystone predators such as sea stars strongly affect occurrence and density of animals in the middle intertidal (use of removal and caging experiments: see Box 11.1: Transplantation, Removal, and Caging Experiments)
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Competition Research Predator exclusion cage experiments
on New England rocky intertidal – Work by Dr. Griffin, U of So Carolina Researching barnacle competition in New Zealand. - work by Rahul Demello, Victoria University of Wellington
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Zonation Biological interactions (competition for space, predation, grazing) are often important factors in determining lower limit of rocky intertidal organisms; physical factors (desiccation) for determining upper limit
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Substrate in the Soft Bottom Intertidal
Sediment size can vary between sand, silt, clay, or a mixture (mud) The smaller the sediment size, the less oxygen in the water filling spaces
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Substrate in the Soft Bottomed Intertidal
The sediment size can be small so that all except the top few inches is anoxic (without oxygen). Infauna must maintain a connection with the oxygenated zone via tubes, siphons, or extended burrows if they are located in the anoxic zone Anaerobic bacteria that break down organic matter thrive in the anoxic zone Most animals are infauna: adaptations to dig or burrow (see Figs and 11.30) Poor epifauna
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Soft Bottom Intertidal Organisms
The diagram to the right shows the diversity of infauna and epifauna that may be found in this community.
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Soft Bottom Food Webs Detritus (broken down organic particles) and producers such as photoautotrophs and chemoautotrophs form the basis for the food web in this community.
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Rocky Intertidal Food Webs
The food web in the rocky intertidal is based on autotrophs such as seagrasses, algae and diatoms. Top carnivores in any community that have the ability to change community composition significantly are known as keystone predators.
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