introduction to wetlands...yash p. abrol and keith t. ingram: effects of higher day and night...
TRANSCRIPT
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Introduction to Wetlands
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Quick Review!
• Early settlers;
• Population expansion;
• Functions and values;
• Two major types;
• Distribution in Virginia.
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Defining a Wetland
Those areas that are inundated or
saturated by surface or ground
water at a frequency and duration
sufficient to support, and that under
normal circumstances do support, a
prevalence of vegetation typically
adapted for life in saturated soil
conditions
www.usace.army.mil/Portals/2/docs/civilworks/regulatory/rw_bro.pdf
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Start by defining unique attributes
•Presence of water
•Saturated soils
•Hydrophytic vegetation
(hydrophytes)
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Water Soil
Vegetation
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Soil
Vegetation
Nutrients
(in pore water)
Support
Organics
Pore spaces
Temperature
mediation
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Water
Vegetation
Hydrogen for PS
Drawdown
Pore spaces
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Water Soil
Saturation/inundation
Erosion
Some cohesion
Stores water
Provides microb habitat
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pH (~5 to 8);
Minerals and nutrients
– Macronutrients (C HOPKNS
CaFe Mg)
– Cation exchange capacity;
What else is Necessary for Plant
Growth?
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All plants rely on soil microbes, microbes need an electron accepter;
In the absence of O2, bacteria use other oxidized elemental forms as terminal electron acceptors;
Two other things needed for this to occur:
1. Sugars;
2. Water.
Chemical Reduction in Wetlands
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Element Oxidized Form Reduced Form Eh (mV)
Oxygen O2 H2O 400 to 600
Nitrogen NO3- (nitrate)
N2O, N2, NH4+ (nitrous
oxide, nitrogen gas, and
ammonium)
250
ManganeseMn+4
(manganic)Mn+2 (manganous) 225
Iron Fe+3 (ferric) Fe+2 (ferrous) 120
Sulfur SO4-2 (sulfate) S-2 (sulfide) -75 to -150
CarbonCO2 (carbon
dioxide)CH4 (methane) -250 to -350
The Redox “Hierarchy”
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O
A
B
C
Root-
ing
depth
Soil Horizons
– O-horizon: organic
materials
(undecomposed or
partially decomposed
litter)
– A-horizon: mineral
soil with some
organic enrichment
(“topsoil”)
– E-horizon: zone of
“eluviation”
(materials leached
out)
– B-horizon: zone of
“illuviation”
(accumulation of
materials leached
from above)
– C-horizon:
undifferentiated
subsoil (resembles
parent material)
– R-horizon: bedrock
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Reducing Fe3+ = Fe2+
Fe3+ (ferric) is not water
soluble, reflects red light.
Fe2+ (ferrous) is not water
soluble, neutral color
(absorbs most light).
Fe3+ is used in plant
metabolism.
Fe2+ , on the other hand,
is toxic to plants.
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Soil Color: upland soils are
yellow-brown-red, wetland soils
are usually gray
How can you use soil color to
indicate a wetland soil?
Wetland (hydric) soil:...saturation, flooding, or ponding...during the growing season...anaerobic conditions in the upper part
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Coating of Fe2O3
Mineral grain (gray)
Remove Fe if
reducedRed Soil
CoatingsGray Soil
Upland Soil Wetland Soil
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Upland Soil Wetland Soil
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Wetland Plants and Stress
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What is stress?
An aberrant change in physiological processes
brought about by one or a combination of
environmental and biological factors. Stress
leads to injury and/or reduced growth. (The
Physiology of Plants Under Stress, Hale and Orcutt 1987).
Physical Chemical Biotic
Drought Air Pollution Competition
Temperature Allelochemicals
(organic)
Allelopathy
Radiation Nutrients (inorganic) Lack of Sybiosis
Flooding Pesticides Human activities
Mechanical Toxins Diseases
Wind Salts Insects
Electrical pH of Soil Solution
Magnetic
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Homeostasis is the property of a
system in which variables are
regulated so that internal conditions
remain stable and relatively
constant.
Examples of homeostasis include
the regulation of temperature and
salinity, and the balance between
acidity and alkalinity (pH).
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Biotic Response to Stress
Osmoconformers: the capacity of a plant (or
animal) to survive and grow even though
subjected to an unfavorable environment: i.e.
it can sustain the effects of stress without
dying or suffering irreparable damage. Plants
will reach a thermodynamic equilibrium
(acclimation).
Spartina alterniflora: stores organic compounds and excess salts in cells that allows diffusion gradient where water moves into plant. Also has hollow stems for oxygen diffusion to roots.
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Osmoregulator: plant does not come to
thermodynamic equilibrium with the stress
or can exclude the stress by means of a
physical or metabolic barrier.
Spartina patens: under salt conditions (and
water stress) S. patens rolls leaves (involute
margins) to cover stomata. Moisture regime
in rolled leaf moist. Can only be sustained
for short period of time.
Biotic Response to Stress
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There are adaptations for both types of strategies.
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Summary:
Osmoconformers must find way to
reach isostasis (hyper- or isohaline
conditions) using inorganic or organic
salts.
Osmoregulators must leave area or
find way to avoid stress.
In both cases Homeostasis is
the goal!
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Oh no,
not
more!
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Anoxia
Wetland Stressors
Temperature
Nutrient
Irradiation
Salt
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• High amounts of salt can result in
a drought-like environment
for plants.
• Plants will exhibit drought or root
damage injuries.
What Effect does Salt have on Plants?
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SALT STRESS
Cell Level: Osmotic Homeostasis
Most plants live in an “isotonic” environment
where [salt] = cell [salt] (isostatic osmotic
potential).
+
+
+
+
+
+
+
+
Permeable membrane
Plant cellSalt Water
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SALT STRESS
Cell Level: Osmotic Shock
Salt: Plants that grow with root systems in soil
of high salt content have low osmotic potentials
as a result an increased [] of solutes and are salt
tolerant. High salt [] can cause both osmotic stress
and toxicity.
+
+
+
+
+
+
+
+
+
+
+
+
Permeable membrane
Plant cellSalt Water
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SALT STRESS
Cell Level: Osmotic Shock
Salt: Plants that grow with root systems in soil
of high salt content have low osmotic potentials
as a result an increased [] of solutes and are salt
tolerant. High salt [] can cause both osmotic stress
and toxicity.
+
+
+
+
+
+
+
+
+
+
+
+
Water flow
Permeable membrane
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Cell Level: Coping with Salt
Single cell organisms increase
internal salinity
Halophiles: increase inorganic molecules
Specifically K+ (actually decrease Na+)
Halophyte: increase organic molecules
WHY?
(e.g. Glycerol and/or arabitol)
These do NOT interfere w/
enzyme activity
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Organism Level: Coping with Salt II
Higher Plants
1) Increase inorganic molecules and organic
compounds (K+, arabitol, glycol, glycerol);
2) Structural complexity
Salinity within intercellular space of leaves
of black mangrove is 50-70% NaCl, rest is
organic composition
a. Barriers (endodermis)
Other species (Bidens) had only
10%NaCl and 90% organic.
b. Excrete salts (Spartina alterniflora)
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Anoxia
Anoxia in a wetland is defined as the point where
all the available oxygen in the soil and pore water
has been depleted, usually through respiration of
micro-organisms.
Anaerobic respiration: plants respond by
increasing the rate of glycolysis (break down of
glucose to pyruvate and lactic acids) and
fermentation.
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From Anderson and Perry 1996
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Glycolysis (O2 present)
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Glycolysis (Fermentation)
Glucose
No external O2 to act as
electron acceptor
Fermentation
Pyruvate
decarboxilation
Acetaldehyde
Ethanol
ADP
ATP
NADox
NADred
(Malate)
(Fatty Acids)
Uses an endogenous
electron acceptor,
which is usually an
organic compound
(C4)
(toxic)
(toxic)
(toxic)
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Alternate Electron Accceptors
Nitrogen
Manganese
Iron
Sulfur
Carbon
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Anaerobic Respiration
All byproducts of aerobic respiration are non-toxic!
H2O, ATP, NADox
Most byproducts of anaerobic respiration are toxic!
Acetaldehyde, Ethanol,
NADred
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Morphological (structural)
Plant response to inundation and/or
saturation stress can be divided into
three categories:
Physiological
Reproductive
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Morphological (structural)
Adaptations
Aerenchyma
Buttressed tree trunks
Pneumatophores
Adventitious roots
Hypertrophied lenticels
Pressurized gas flow
Shallow roots
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What happens when a plant is flooded?
Decrease in PS
% C
ausa
lity
Stomata Closing
Inhibitory Effects
Inhibitory Effects = Ribisco, ethanol, acetaldehyde
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Aerenchyma
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Aerenchyma
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Aerenchyma
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Aerenchyma
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Aerenchyma & Passive
Diffusion
O2
O2
CO2
CH4
CO2
CH4
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Herbaceous wetland: tidal salt marsh
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Air
Air
Old Stems New Stems
Rhizome
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Increased Air
Air
Old Stems New Stems
Rhizome
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Pressurized ventilation (mass flow, bulk
flow, or convective though flow)
Air
Air
Rhizome
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Buttressed Trunks
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Pneumatophores
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Black Mangrove (Avecinia germinans)
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Gaseous Exchange
Air CO2
CO2
CO2
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Adventitious roots
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Red Mangrove (Rhizophora mangle)
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Hypertrophied lenticels
Hypertrophied lenticels
An exaggerated (oversized) pore on the stem of woody plants through which
gases are exchanged between the plant and the atmosphere, serves to increase
oxygen to plant roots during periods of inundation or soil saturation.
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Reproductive Strategies
Delayed or accelerated flowering
Buoyant seeds
Vivipary
Large persistent seed banks
Production of tubers, roots, and seeds that can
survive long periods of submergence
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Temperature/Irradiation
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Temperature
High temperatures cause increased respiration and R>P
1) Loss of water;
2) thermal tolerance in relation to membrane
stability;
3) induced thermotolerance through gradual
temperature increase vis-a-vis production of heat
shock proteins; and
4) decreased photosynthesis and productivity during
high temperature stress.
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Temperature/Irradiation
Increased temperatures force plant into photorespiration.
Normal range 0o to 40o C
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YASH P. ABROL and KEITH T. INGRAM: Effects of higher day and night temperatures on growth and yields of some crop plants
Seasonal foliage temperatures of wheat (cv. Kanking) and cotton (cv.
Paymaster 145) grown at Lubbock, Texas. The vertical lines represent
the temperature range that comprises the species-specific thermal
kinetic window (where Michaelis-Menten constant for CO2 (Km) is
minimal and stable) as determined from the changes in the apparent
Kmof purified enzymes with temperature.
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1) Induces rapid transpiration and water loss;
2) The guard cells lose turgor, the stomates partially or
completely close, and the rate of diffusion of carbon
dioxide into the leaves slows down;
Increase in Temperature of Leaves
3) Rate of photosynthesis decreases while respiration
continues, resulting to low availability of
carbohydrates for growth and development
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1) Chlorophyll content is
reduced. This reduces the rate
of light absorption and the rate
of photosynthesis;
2) Increase in temperature of
leaves which in turn induces
rapid transpiration and water
loss;
3) High leaf temperature
inactivates the enzyme system
that changes sugars to starch.
From Edmond et al. (1978)
High Light Intensity
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Granular (stacked chlorophyll-found in leaf blade of all plants)
Agranular (only found surrounding bundle
sheath of veins of C4 plants)
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Glycolysis (Fermentation)
Glucose
No O2
Fermentation
Pyruvate
Decarboxilation
C3
Acetaldehyde
Ethanol
ADP
ATP
NADox
NADred
Malate
C4
ADP
ATP
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C4 v. C3 Plants
20 to 50%
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Atriplex patula (C4) v. C3 A. rosea (C3)
Light Intensity Leaf Temperature [CO2] w/i intercellular spaces
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C4 v. C3 Plants
C4 plants have a competitive advantage over plants
possessing the more common C3 carbon fixation
pathway under conditions of drought, high
temperatures and nitrogen or carbon dioxide limitation.
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That’s
all,
Folks!
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Tidal River/
Lagoon
Ebb
Flood
Sa
lin
ity (
no
te:
tid
e ra
ng
e re
ma
ins
con
sta
nt)
Dec
rea
seEstuary/River
ProfileTidal Freshwater Marshes
Polyhaline Saltmarshes
Ocean
Headwater System
Spatial Diversity
Oligohaline Saltmarshes
Mesohaline Saltmarshes