Estuary Biomes: Definition and Ecology

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Questions and Answers

Which of the following factors contributes to the high level of variability in estuarine environments, making them stressful for organisms?

  • Extreme variation in salinity (correct)
  • Constant temperature
  • Stable salinity levels
  • Consistent oxygen levels

Estuaries are typically considered low-diversity environments due to their unfavorable conditions.

False (B)

What is the term for the adaptation where estuarine organisms allow their internal salinity to vary with the surrounding water?

osmoconformity

The tidal range in estuaries can be artificially enhanced by urbanization through a combination of encroachment and ______.

<p>flood defence</p> Signup and view all the answers

Match the following estuary zones with their characteristics:

<p>Freshwater Zone = Riverine zone above tidal influence Tidal Freshwater Zone = Subject to tidal influence but essentially fresh Mixing Zone = Progressive increase in salinity with distance from the river Seawater zone = Marine waters with little or no dilution</p> Signup and view all the answers

What is the primary reason estuaries are considered exceptionally new systems in geological and evolutionary terms?

<p>Successive influence by glaciation and sea-level rise (C)</p> Signup and view all the answers

Temperature variation, rather than salinity, is the primary environmental trigger for the migration and reproduction of estuarine organisms in higher latitudes.

<p>True (A)</p> Signup and view all the answers

Name one adaptation estuarine organisms have developed to tolerate low levels of dissolved oxygen.

<p>anaerobic respiration</p> Signup and view all the answers

Fine-grained mudflats in estuaries are primarily composed of soft, fine, grey silt, which gives off a distinctive ______ odour when disturbed.

<p>sulphurous</p> Signup and view all the answers

Match each estuarine habitat with its description:

<p>Mudflats = Areas of soft, muddy sediment exposed at low tide Saltmarshes = Areas of grassland flooded at high tide Mangroves = Forests of trees and shrubs that grow in saltwater Seagrass Beds = Underwater meadows of seagrass</p> Signup and view all the answers

Why are estuaries considered to have high levels of secondary production?

<p>High quantity and quality of available food (D)</p> Signup and view all the answers

The outer limit of an estuary can easily be defined by a specific level of seawater dilution.

<p>False (B)</p> Signup and view all the answers

What is the term for the longitudinal profile of dissolved oxygen levels in an estuary that shows a notable dip in the mid-estuary?

<p>DO sag</p> Signup and view all the answers

__________ are the most abundant organisms in estuaries and play an important role in the decomposition of organic matter and the cycling of nutrients.

<p>bacteria</p> Signup and view all the answers

Match the type of estuary to its formation mechanism:

<p>Coastal Plain Estuary = Flooding of river valleys following sea-level rise Fjord = Flooding results in deep-sided estuaries formed from glacial U-shaped valleys Bar-built Estuary = Offshore deposits form barriers restricting flow Tectonic Estuary = Land sinking due to tectonic activity, flooding the valley</p> Signup and view all the answers

Flashcards

What is an Estuary?

A transition zone between freshwater and marine environments, influenced by both, but with unique ecology.

Lower Estuary sector

An estuary zone with a free connection to the open sea.

Middle Estuary Sector

An estuary zone characterized by strong mixing of salt and fresh water.

Upper Estuary Sector

An estuary zone primarily freshwater, subject to daily tidal action.

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Coastal Plain Estuaries

Estuaries formed by the flooding of river valleys due to rising sea levels.

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Fjords

Estuaries often found to be very deep, formed in glacial U-shaped valleys.

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Bar-Built Estuaries

Estuaries created by offshore deposits that form barriers across bays or inlets.

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Isostatic Variation

Occurs when estuaries are created by land sinking due to tectonic activity.

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Eustatic Sea Level Change

Change in sea level due to variations in the volume of water in the ocean.

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Isostatic Sea Level Change

Change in sea level due to variations in the level of the land.

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Tidal Prism

A measure of the difference in water volume in an estuary between high and low tide.

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Estuarine Zonation

Estuaries divided into zones based on freshwater and saline water mixing.

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Osmoregulation

Adaptive process where organisms maintain a stable internal salinity despite external changes.

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Osmoconformers

Organisms that allow their internal salinity to vary with their surroundings.

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Mudflats

Areas of soft, muddy sediment exposed at low tide, serving as habitats and feeding grounds.

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Study Notes

Estuaries: The Transition Between Freshwater and Marine Biomes

  • Estuaries exhibit distinct, variable, and fascinating environments and ecologies due to the blending of fresh and saltwater.
  • They support diverse invertebrate populations and serve as crucial nursery grounds for fish and feeding areas for birds.
  • They are sometimes considered the most degraded habitat, and provide an ideal setting for studying ecology, conservation, and human impact interactions.
  • Estuarine study requires comprehensive ecosystem knowledge.

Introduction to Estuaries

  • Most view an estuary as a place where a river meets the sea
  • This interaction yields diverse systems, with an estuary being only one type.

Defining an Estuary

  • Defining an estuary has proven difficult, with over 40 definitions proposed, with varied criteria like seawater dilution, tidal regime, and geomorphology.
  • Traditional focus on salinity can overshadow other environmental and biological variables.
  • The Amazon estuary has a tidal influence reaching 735 km inland, but insignificant seawater penetration due to vast river flow; mixing occurs 1000 km seaward.
  • Defining by tidal influence differentiates deltas from estuaries.
  • Defining an estuary is an inlet of the sea reaching into a river valley up to the tidal rise limit
  • Typically divisible into three sectors: (1) lower (free connection to open sea); (2) middle (strong salt/freshwater mixing); (3) upper (freshwater with daily tidal action).
  • Defining boundaries using salinity can be difficult
  • In unmanaged estuaries, the upper boundary is that of daily tidal influence, truncated by structures in urban areas.
  • Defining outer limits is harder; large rivers create reduced salinity plumes far into the sea.
  • Estuary boundaries are usually subjectively defined by coastal morphology or management criteria.
  • Estuaries are part of a continuum from river to sea, with both biomes strongly affecting estuarine ecology.

Estuary Evolution

  • Estuaries differ from marine systems due to their geological ephemerality in temperate zones influenced by glaciation.
  • High sedimentation rates lead to infilling and ecological succession.
  • During the last glaciation (17,000 BP), sea levels were 130m lower, with a rapid rise following ice sheet retreat, flooding continental shelves and river valleys to create modern estuaries by 6000 BP.
  • Because of this, most estuaries are new systems with implications for colonization, diversity, and ecology.

Estuary Classifications

  • Estuaries vary globally in geomorphology, tidal range, and salinity, leading to various classification schemes for comparison.
  • Topography is a popular classification method that reflects formation after post-glacial sea-level rise.

Topographic Classification

  • Coastal Plain estuaries are the most common, formed by river valley flooding after eustatic sea-level rise.
  • Fjords are deep estuaries from glacial U-shaped valleys, with a shallow sill limiting seawater exchange and causing anoxic basins.
  • Bar-built estuaries form from offshore deposits that restrict seawater flow, creating diluted water bays.
  • Estuaries can also be created via isostatic variation in areas of tectonic activity: the San Francisco Bay formed from land sinking.

Change in Sea-Level

  • Change in sea-level can be either eustatic (variations in ocean volume), or isostatic (land level variations).
  • While topography is a common classification method, it has little ecological relevance except on a broad scale.
  • Fjords are typically boreal, while blind estuaries are more tropical.

Tidal Range Classification

  • Tidal range also classifies estuaries, having major dynamic and ecological impact, separating them from brackish seas.
  • Estuaries exhibit varied tidal amplitudes, from under a meter in tropical systems to over 16m in the Bay of Fundy, Canada.
  • The tidal prism (water volume difference between high and low tide) in the Bay of Fundy is ~100 billion tonnes!
  • Estuaries are categorized by tidal range: microtidal (<2 m), mesotidal (2-4 m), macrotidal (4-6m), and hypertidal (>6m).
  • Urbanization, especially encroachment and flood defenses, enhance these ranges through channel narrowing.

Tides

  • Tidal movement is a key estuarine descriptor
  • Also, it affects organism function, survival, and distribution by varying physicochemical parameters
  • Estuaries are naturally stressful aquatic systems due to environmental variability.

Important Environmental Variables in Estuaries

  • Key environmental conditions like salinity, sediment, dissolved oxygen and temperature affect estuarine life

Salinity

  • Historically, salinity was considered the dominant factor that defined estuarine survival and distribution of organisms; salinity remains an important, widely variable factor.
  • Salinity has two components: spatial/longitudinal variation (0 at river end to 34 at mouth) and temporal (tidal) variation.
  • Salinity in tropical estuaries can exceed seawater salinity due to evaporation.
  • The most significant salinity variation: conditions changing over time.
  • Salinity ranges in the mid-Ythan, Scotland can range from 3 to 29 over a tidal cycle.
  • Salinity is measured as Practical Salinity Units (PSU), represented as a number without units.
  • Salinity range decreases toward both ends of an estuary away from the mid-estuary.
  • Trapped water salinity is less variable in intertidal areas, where heavier seawater fills in and lighter freshwater flows on top of the sediment.
  • Salinity of interstitial water in subtidal sediments mirrors overlying water.
  • Seasonal variations in freshwater flow rates can influence estuaries.
  • Freshwater flow impacts current speed and saltwater interaction, plus the overall estuarine structure

Sediment

  • Intertidal mudflats, of soft grey silt, compose estuaries and are difficult to traverse, while emitting a sulphurous odor.
  • This mobile sediment makes it difficult to colonize so it has no points of macroalgae attachment/sessile organisms; organisms avoiding mechanical disturbance cannot manage the substratum.
  • Fine particles can clog feeding and respiratory structures, which makes locomotion challenging.
  • Thriving organisms need to be adapted to the sediment moreso than salinity.
  • Large mudflats form within the middle reaches of the estuary under normal conditions, and are comprised of seafloor material.
  • Sediment deposition results from the speed of tidal/river currents, but there is an excess of suspended sediment concentration towards the estuary for various reasons.
  • Sediments near estuary mouths and heads are coarser due to high tidal/river flows, preventing fine particle settlement.
  • Mudflats found in estuaries are full of material that settled out of the water column
  • Estuaries have one of the highest levels of secondary production in aquatic systems.
  • Deposit-feeding organisms can tolerate stressful mudflat conditions and have extremely high growth rates due to abundant, high-quality food.

Dissolved Oxygen

  • Low oxygen levels are uncommon in aquatic systems, so estuaries have some unique conditions that affect life.
  • Estuarine waters and sediments have high organic matter and microorganism levels, which consume dissolved oxygen.
  • Aerobic bacteria breakdown matter in estuarine waters which depletes oxygen; head/mouth of estuary have normal oxygen.
  • An oxygen sag occurs in middle estuaries.
  • Oxygen removal from interstitial water in mudflats is more severe; diffusion is prevented by sediment
  • Matter is broken down by anaerobic bacteria below the surface by oxygen removal, causing toxic by-products like methane and hydrogen sulfide.
  • The effect is black mud with a rotten egg smell (occurs in unpolluted estuaries); adds stress to organisms.
  • Low estuarine oxygen is severely impacted by human life.
  • Human settlement on estuary banks stimulates removal of oxygen via sewage disposal, organic matter supplementation, and bacterial action.
  • Estuarine waters can become oxygen-depleted, threatening ecology when urbanized.

Temperature

  • Limited temperature variables, but there are seasonal temperature patterns changing the major trigger for migration and reproduction (fish + large crustaceans).
  • Temperate change can be influential and a major ecological factor; temperature also influences the speed of microbial breakdown.
  • Bacteria process organic matter rapidly in the tropics/summer of the temperate systems.
  • During urbanized areas, oxygen depletion is more severe during the summer when temperate water occurs
  • The discharge of water can affect temperature levels
  • Thames Estuary’s water temperature increased by three degrees because of power stations.

Conditions Linking Human Influence

  • Conditions surrounding and within estuaries are directly connected to human activity impacting the water quality, fisheries, and/or alteration of the surrounding bankside environment.
  • Estuaries are the most anthropogenically degraded habitat, and that must be considered when investigating ecology.

Estuary Zonation

  • Estuaries are traditionally divided into zones reflecting overall environmental conditions apparent in the region for additional sub-classification.
  • Schemes are based on various salinity levels and are highly subjective
  • Zones are hard to spatially define in a system that's changing via tidal and seasonal cycles.
  • Pritchard's (1967) scheme is based on the mixing of saline and fresh water

Pritchard's Zonation Scheme

  • Freshwater zone is defined as the river above the tidal influences
  • Tidal freshwater zone is subject to tidally influences, but is essentially freshwater
  • Mixing zone features a steady increase in salinity, as distance from the river is gained
  • Seawater zone is defined as marine waters with little to no dilution
  • Mixing Zone includes: upper mixing (freshwater dominant), middle mixing (steady salinity increase), and lower mixing (marine influence is dominant).
  • Location varies with state and freshwater flow.

Estuarine Organisms

  • Most of them have evolved elsewhere
  • Few organisms have evolved to exclusively live there
  • Estuarine organisms are descendants of marine/freshwater and have developed mechanisms to survive

Evolution of Estuarine Organisms

  • There is complex disagreement surrounding estuarine evolution, but here are the leading theories:
    • Estuarine evolved from: marine species that tolerate low salinity
    • Estuarine species evolved from: freshwater that tolerate high salinity
  • Likely that both processes occurred

Challenges for Organisms

  • Maintain a stable internal environment in the face of salinity change
  • Known as osmoregulation
  • Osmoconformers allow their internal salinity to vary
  • This is a passive strategy
  • Osmoregulators maintain a stable internal salinity.
  • Active/energy demanding

Osmoregulation

  • Organisms are osmoregulators because it's hard for osmoconformers to maintain stable internal
  • The sediment makes organisms more stable/osmoconformers

Adaptations of Estuarine Organisms

Adaptations

  • Have developed adaptations to survive that can be divided into categories
  • Physiological Adaptations: affect organisms internal functioning
  • Behavioural Adaptations: Affect organisms behavour
  • Life History Adaptations: Affect organisms lifecycle

Physiological Adaptations

  • Most important: osmoregulation because changes in salinity makes it hard for osmoconfomers
  • Important adaption tolerate levels of disolved O2
  • Levels are low in sediment
  • This helps them extract oxygen from water and breathe
  • Has allowed them to switch to respiration when O2 levels are low

Behavioural Adaptations

  • Most important burrow, allows them escape predators and avoid currents
  • Helps escape salinity and temp
  • Ability to migrate
  • Move to new habitat/conditions that are good
  • Estuarine fish transfer between Estuaries and sea

Life-history Adaptations

  • Ability to be able to reproduce quickly
  • Reproduce likely to take advantage

Dispersal

  • Important adaptation, ability to dispersed widely
  • Organisms that dispersed are mor likely to fine habitats

Diversity of Estuarine Organisms

  • Estuaries are home to a range of organisms including algae plants invertebrates fish and birds
  • Diversity influenced by: salinity, temp, sediment type, food O2 availability

Bacteria

  • Most abundant
  • Play role in decomposition and cycling nutrients

Algae

  • Algae: abundant and have food
  • Are important primary producers use sunlight to produce food
  • Plants
  • Home to plants (mangroves) plants animals use for food

Invertebrates

  • Animals w/out backbones most diverse
  • Play role in foodweb and helpful filter wate

Fish

  • Very important habitat for fish
  • They are food for people

Birds

  • Great habitat for birds
  • Food from crustaceans/fish

Importance of Estuaries

  • Many benefits for animals and humans

Importance

  • Water filtration helps to filter H2O
  • Flood control helps absorb it
  • Fisheries: important for Fish
  • Recreation: for boating
  • Tourism: major

Global Economy

  • Worth trillions

Threats to Estuarie

Threat

  • Pollution from sewage/agriculture harm

Habitat Loss

  • Harm from development/activities

Climate Change

  • Cause sea levels to rise
  • Inundating

Invasive Species

  • Outcomplete

Estuarine Conservation

Important for benefits they contribute

Conservation

  • Recycle
  • Conserve
  • Restore
  • Impact

Estuarine Habitats

  • Variety of Habitats including

Habitats

  • Mudflaps
  • Salt marshes
  • Mangroves
  • Seagrass
  • Oyester Reefs
  • Unique community

Mud Flats

  • Common
  • Worms crab food for bids

Saltmashes

  • Birds other animals upper

Mangroves

  • Protect from the ocean
  • Fish crabs

Seagrass beds

  • Found shallow h2o
  • Fish crabs

Oyster Reefs

Currents

Estuarine food webs

  • Consists of phytoplankton, base made zooplankton they eat each oth

Consumers

  • Zooplanktoninvertebrates

Decomposers

  • Break down plant
  • Estuaries are productive one earth

PromaryProduction

  • Rate producers make organic
  • Estuaries receive nutrients

Secondary Production

  • Secondary production
  • Consumers
  • Many factors impact

Factors

Nutrient availability

  • Important availability

Light availability

  • Photosynthesis

Temp

  • Metabolic rate affect

Salinity

  • Distrubution

Pollution

  • HArm reduce productivity

Food Webs

  • Base estuarine food webs
  • Eats

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