Title: Palaemonetes
1Palaemonetes glass shrimp
2Boundary Habitats
3Questions
- What are estuaries?
- Physical parameters
- Biological classification
- What are patterns of mixing in estuaries?
- What are the challenges of estuaries?
- How are estuaries and ocean systems linked?
4Estuary refers to a physical condition
- A partially enclosed coastal area where fresh and
sea water mix - Mixing creates high variability in salinity
- Variable salinity is unusual in most other ocean
systems - Definition excludes inland, saline waters
- Geological derivation leads to finer
classification of estuaries
5Drowned river valleys(Coastal plain estuaries)
- Formed after the last ice age to 3000 years bp
(before present) - Usually in temperate zone, with low sediment
loads - Process of sedimentation is slower than
inundation (otherwise one finds deltas)
6A drowned river valley estuary
7coastal plain estuary
8Bar-build Estuaries
- Shallow basins, with barrier islands inlets
- Sedimentation
- inundation
- May be shallow with extensive lagoons, marshes
9Fjords
- Once covered by ice sheets
- Glaciers cut typical U shaped valleys rock
sills at mouths - Norway, Canada, Chile, New Zealand
10Tectonic estuaries
- Created by faulting and land subsidence
11Patterns of mixing for fresh and sea water
- Mechanisms influencing pattern
- Fresh water has lower density floats on sea
water if turbulence is low - River flow is out, tidal flux is both out and in
- Mixing patterns are sensitive to flow rates
- Salinity can be highly variable in space and time
12Fresh and salt water mixing regimes
13Positive or Salt-wedge estuaries
- High flow of fresh water from river
- Fresh water flows outward, over deeper salt water
- Wedge of salt water changes position with tides
- Moderately stratified
- Also called river-dominated estuaries
14Marine-dominated estuaries
- Very low flow of fresh water
- Promotes more complete vertical mixing
- Tidal flux, winds, and shape of basin influence
mixing
15Negative/evaporite estuaries
- In hot climates, high evaporation is combined
with low fresh-water flow - Creates hypersaline estuaries (higher salinity
than surrounding sea water)
16(No Transcript)
17(No Transcript)
18(No Transcript)
19(No Transcript)
20(No Transcript)
21Fluctuations in salinity in the water column are
buffered in sediments
22Other important physical parameters
- Turbidity
- Sediment load delivered by river
- Dynamics of settling and resuspension
- Temperature, which can be highly variable in
shallow water - Oxygen levels, also more variable than in typical
ocean habitats
23Interactions among physical parameters
24Characteristics of biological communities Marsh
habitats
- Generally, high density but low diversity
- Physiological stresses
- Low topographic substrate variability
- But very high potential for productivity due to
nutrient input
25Components
- Macrophytes (seagrasses, sedges, rushes,
cordgrasses) - Epiphytic algae (macro- and micro-)
- Benthic macroalgae and microalgae
- Phytoplankton
26Estuary edge zonation in marshes