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Marsh Dieback: History, Potential Causes,

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Title: Marsh Dieback: History, Potential Causes,


1
Marsh Die-back History, Potential Causes,
Current Evidence
  • Karen L. McKee
  • U. S. Geological Survey
  • Irving A. Mendelssohn
  • Louisiana State University
  • Michael D. Materne
  • Natural Resources Conservation Service

2
Historical Perspective
Die-back of Spartina marshes has been
recognized since 1968
Coastal Studies Bulletin No. 5 / Special Sea
Grant Issue /February 1970 SPARTINA DIE-BACK
IN LOUISIANA MARSHLANDS W. G. Smith Coastal
Studies Institute Louisiana State University
Spartina alterniflora marshlands in Louisiana
frequently have large areas of standing dead
stubble. These killed areas were first noted by
the author in the Grand Isle area on November
10, 1968 As of December 31, 1969, no recovery
was evident (Smith 1970)
3
Salt Marsh Die-back in Louisiana
Since the 1970s more research concerning salt
marsh die-back has been conducted in Louisiana
than probably anywhere else in the world
4
Historical Spartina alterniflora Die-back
- Typical die-back of Spartina occurs in the
marsh interior
- These areas cannot maintain their elevation
relative to sea-level rise
- Our research has shown that this historical
die-back has occurred because excessive
submergence leads to sulfide accumulation, which
in turn causes reduced growth and eventually
plant death.
5
Current Marsh Dieback
6
Potential Causes of Die-back
  • Background Statement
  • Evidence
  • Data collected
  • Literature

7
Biotic Factors
8
Pathogens
  • Background Bacterial, fungal, or viral
    pathogens or insect outbreaks can cause
    widespread mortality of plants.
  • Evidence for Pathogens
  • In Texas Florida, a fungal involvement has been
    identified in connection with Spartina die-back,
    but infection usually opportunistic on stressed
    vegetation.
  • Evidence against Pathogens
  • Examination of Spartina culms from LA by
    pathologists has so far revealed no obvious
    pathogens.

9
Herbivory
  • Background Herbivores (nutria, waterfowl) can
    cause large eat-outs in marshes.
  • Evidence for Herbivory Some, but not all,
    die-back areas have large concentrations of
    snails that are eating the dead vegetation.

10
Herbivory
  • Evidence against Herbivory -Not all die-back
    areas have high densities of snails or evidence
    of snail feeding on live tissue.

11
Herbivory
  • Evidence against Insects
  • No evidence of insect outbreaks or insect damage
    out of the ordinary.

12
Low Genetic Diversity
  • Background Generally, the higher the genetic
    diversity the broader the ecological amplitude of
    a species. Changes in the environment that lead
    to a substructuring of populations may render a
    marsh more vulnerable to sudden extremes that
    exceed the genetic capacity of the population to
    adjust.

13
Low Genetic Diversity
Evidence European research shows two genetic
groups of Phragmites australis (deep water reed
and land reed), each of which may be
completely eliminated from an area by
manipulations favoring the other genotype and
preventing the establishment of new populations
after old ones have been destroyed. The
surviving population is more likely to
experience die-back.
14
Abiotic Factors
15
Chemical Spill (e.g., petroleum)
  • Background Chemical spills can kill large areas
    of marsh in a short period of time.
  • Evidence for Spills
  • There were no signs of a chemical spill in the
    die-back marshes.
  • Evidence against Spills
  • Pattern and extent of die-back is inconsistent
    with this hypothesis.

16
Buildup of Sulfide / Fermentative Products
  • Background Organic matter is generally
    accumulated in wetlands, and the anaerobic carbon
    decomposition in wetland sediments produces a
    range of fermentative products that are toxic to
    plants (organic acids and sulfide) at high enough
    concentrations. This process can also create a
    high soil oxygen demand that can stress plants by
    competing for their internal oxygen.

17
Buildup of Sulfide /Fermentative Products
  • Evidence for Phytotoxins
  • Historical die-back of Spartina alterniflora has
    been linked to sulfide accumulation in Louisiana
    marshes.
  • Current die-back areas exhibit elevated
    concentrations of sulfide. However, death of
    plants will generate these compounds a cause and
    effect relationship cannot be assumed.

18
Buildup of Sulfide / Fermentative Products
  • Evidence against Phytotoxins Unaffected species
    are not more tolerant of sulfide, e.g., Avicennia
    germinans.

19
High Salinity
  • Background The recent severe drought, combined
    with low river flow, may have increased salinity
    in die-back marshes.
  • Evidence for Salinity
  • Surface salinities did increase in the past year,
    according to records examined thus far.
  • Porewater salinity is slightly elevated in some
    of the dead marshes.

20
High Salinity
  • Evidence for Salinity More salt-tolerant
    species (Avicennia and Batis) have survived
    alongside the dead Spartina.

21
High Salinity
  • Evidence against Salinity
  • Measured salinities (lt40 ppt) do not exceed
    tolerance limits of S. alterniflora.

Upper Limit of Ecological Range 45-50
ppt Lethal Salinity 83-100 ppt From Hester,
Mendelssohn, McKee (1996)
22
High Salinity
  • Evidence against Salinity
  • Less salt tolerant species such as Juncus
    roemerianus have survived in die-back areas.

23
High Water Levels
  • Background Spartina alterniflora is very flood
    tolerant, but there are limits to its tolerance.
    When oxygen is cut off from the plant roots for
    24 hours, the meristems (growing tips) will begin
    to die and the entire plant can succumb within a
    few days.

24
High Water Levels
  • Evidence for High Water Levels
  • Pattern of die-back shows that lower elevation
    areas (interior marsh) are experiencing extensive
    mortality.

25
High Water Levels
  • Evidence against High Water Levels
  • Other species that are equally or less flood
    tolerant than Spartina have survived.

26
Low Water Levels
  • Evidence for low water levels Records indicate
    low water levels at some locations during early
    part of year.

27
Low Water Levels
  • Evidence against low water levels Low elevation
    sites appear to be more affected than high
    elevation sites.

28
Interacting Environmental Biotic Factors
  • Background Several factors may be interacting
    to cause die-back. A pre-existing stress
    condition may have made the plants more
    vulnerable to a second stress factor or a
    pathogen that alone would not have caused
    mortality.
  • Evidence
  • In Louisiana, natural subsidence, sea-level rise,
    and sediment deficiency have been implicated in
    historical die-back of interior marshes.
  • In Europe, Phragmites die-back has been linked to
    a combination of eutrophication, artificially
    stable water-levels (stagnation), and disturbance
    (harvesting, fire).

29
Summary
  • Factors least likely to be involved a chemical
    spill, herbivory
  • Factors possibly involved, but with little or no
    data from a broad survey of current die-back
    sites pathogens, low genetic diversity
  • Factors possibly involved, with some evidence
    from several sites water level extremes,
    salinity, natural toxins (e.g., sulfide)
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