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The ecological consequences of the reduction of species diversity : experimental approachesAllison, Gary William 16 January 1997 (has links)
The influence of loss of diversity on community dynamics and ecosystem
functioning has recently received considerable attention. Although study of biodiversity
has a long history within ecology, empirical investigations exploring consequences of
loss have been rare. Because many factors confound diversity comparisons, experimental
manipulations of diversity offer the most direct way of attributing cause to diversity loss.
The effects of reduction in number of species will depend on the strength and sign
of species interactions affected by loss of diversity. An experiment performed on a high
zone, rocky intertidal community in which macroalgal diversity was manipulated
demonstrated that effects of diversity loss will be highly dependent on which species are
removed. However, effects of diversity reductions were strongest at the harsh end of a
stress gradient where interactions were more positive. Thus, factors that affect the
strength and sign of species interactions such as the degree of physical stress may serve
as a rough guide to where the effects of diversity loss will be most severe.
An assessment of the influence of diversity on community response to a strong
physical perturbation was performed using an experimentally-induced thermal stress.
Higher diversity treatments were most strongly affected directly by the stress because
such treatments had higher abundance and therefore more biomass to lose. However,
those same treatments recovered more quickly from the stress. Community recovery of
initially low diversity treatments was slowed by persistence of non-typical states or slow
recovery of dominant species.
A simulation study was performed to assess the ability of different experimental
designs to detect biodiversity effects. Our ability to predict consequences of changes in
diversity will be dependent on our ability to distinguish the most influential biodiversity
"components" within a system. This study uncovered a phenomenon that will be
common in biodiversity studies: misidentification of one biodiversity component (e. g.,
an effect of a keystone species) as a different component (e. g., an effect of the number of
species). I call this phenomenon "aliasing." Because of the complexity of biodiversity,
experiments and observational studies will be highly susceptible to aliasing and, thus,
results will require careful interpretation. / Graduation date: 1997
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Macroscale to local scale variation in rocky intertidal community structure and dynamics in relation to coastal upwellingFreidenburg, Tess L. 24 May 2002 (has links)
Understanding how large-scale processes (>100 kms) influence ecological
communities is currently a major focus in ecology. In marine systems, coastal
upwelling, a large-scale oceanographic process in which surface water pushed
offshore by winds is replaced by cold, nutrient-rich water from depth, appears to
cause variation in rocky intertidal communities. Along the central Oregon coast
upwelling occurs intermittently during the summer while on the southern coast it
begins earlier in the spring and is less variable throughout the summer.
Coastal upwelling can affect rocky intertidal communities by altering the
delivery of nutrients, larvae, and phytoplankton. I conducted three studies on both
the southern and central Oregon coast to understand how differences in upwelling
affect rocky intertidal community structure and dynamics. In the first study, I
examined the recruitment and growth rates of sessile invertebrates (mussels and
barnacles). Recruitment of both mussels and barnacles, and growth of mussels were
consistently higher on the central Oregon coast than the southern coast.
Upwelled water is nutrient-rich, so differences in upwelling are likely to
affect growth rates of macroalgae. In the second study, I tested this hypothesis by
monitoring the growth of two species of intertidal kelp at both central and southern
coast sites. During El Ni��o years, when upwelling is sharply reduced on the central
Oregon coast, algae may fare better at sites on the southern coast where upwelling
is less affected. However, during years when upwelling is strong all along the
coast, nutrient limitation does not appear to differentially affect macroalgal growth
rates.
Finally, in the third study, I examined the influence of upwelling on the
interactions between microalgal primary producers and herbivorous limpets. I
conclude that this interaction is complex and varies both within and between
upwelling regions.
My research suggests that a transition in upwelling from weak and sporadic
on the central Oregon coast to stronger and more persistent on the southern Oregon
coast drives the striking differences in rocky intertidal community structure and
dynamics between these areas. / Graduation date: 2003
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The effects of biomechanical and ecological factors on population and community structure of wave-exposed, intertidal macroalgaeBlanchette, Carol A. 29 August 1994 (has links)
I examined the biomechanical factors that influence the sizes of
intertidal macroalgae by studying a population of Fucus gardneri at Fogarty
Creek Point, OR. I constructed a mathematical model to predict optimal
sizes and probabilities of survival for Fucus under conditions of high and
low wave exposure. Predicted optimal sizes of Fucus closely matched the
mean observed sizes of plants collected from wave-exposed and protected
locations. To test this hypothesis in the field, I reciprocally transplanted
Fucus between wave-exposed and wave-protected sites and found that the
degree of wave exposure did not affect survival, but did influence size.
Large Fucus were tattered by waves at exposed sites, and small Fucus grew
at protected sites. These results support the hypothesis that wave forces
can set mechanical limits to size in Fucus.
I experimentally examined the relative influences of wave-induced
disturbance, competition and predation on the sea palm, Postelsia
palmaeformis and its understory community at a wave-exposed site at
Depoe Bay, OR. Postelsia recruitment was affected by seasonal variations in disturbance and was greatest in areas disturbed in winter. Postelsia were most abundant at mid-zone, wave-exposed sites, and their restriction to wave-exposed sites seems to be due both to; 1) the occurrence of predictable winter disturbances at these sites which remove mussels, thereby stimulating sea palm growth from the underlying rock, and 2) high water motion which enhances sea palm growth by increasing nutrient exchange and photosynthesis and preventing desiccation at low tide.
Competition, disturbance and grazing were all important factors in structuring the Postelsia understory community. Postelsia were dominant competitors and their holdfasts overgrew low-lying plants which were torn loose with Postelsia when this kelp was dislodged by winter storm surf. In the absence of this predictable, seasonal disturbance, competitive understory species, such as Corallina dominated primary space.
Intermediate levels of disturbance allowed for the highest understory
species diversity. Limpets played a keystone role by grazing Postelsia, the
competitive dominant during most of the year, and maintained high
levels of species diversity in the algal understory. / Graduation date: 1995
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The effects upon the macrofaunal community of a dominant burrowing deposit feeder, C̲a̲ḻḻi̲a̲ṉa̲s̲s̲a̲ c̦a̲ḻi̲f̲o̲ṟṉi̲e̲ṉs̲i̲s̲, and the role of predation in determining its intertidal distributionPosey, Martin Harold January 1985 (has links)
ix, 119 leaves : ill., maps ; 28 cm
Notes Typescript
Thesis (Ph. D.)--University of Oregon, 1985
Includes vita and abstract
Bibliography: leaves 108-119
Another copy on microfilm is located in Archives
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Sandy beach surf zones : what is their role in the early life history of Chinook salmon?Marin Jarrin, Jose R., 1980- 05 October 2012 (has links)
Early life stages of many marine and diadromous fish species use sandy beach surf zones, which occur along >50% of the world's marine coastlines. This extensive habitat can provide juvenile fishes with an abundant supply of potential prey and the ability to hide from predators in its shallow turbid waters. Chinook salmon is an anadromous species that migrates to the ocean during their first (subyearlings) or second (yearlings) year of life. The majority of subyearlings reside in estuaries during their first summer season; however, a small number of juveniles also use surf zones. Early marine residence is considered a critical period for Chinook salmon due to high mortality rates; however the role of surf zones in Chinook salmon life history is unclear. Therefore, I determined the distribution of juvenile Chinook salmon on beaches of the eastern North Pacific, compared the migration and growth patterns observed in surf zones and estuaries, identified the factors that accounted for variation in juvenile surf zone catch, explored the factors
that influence growth rate variation in surf zones and estuaries, and modeled how growth rates in these coastal habitats may vary in the near future with predicted changes in climate.
The majority (94%) of juveniles were caught in surf zones adjacent to estuaries with trough areas, which are beach sections where sand moved by currents and waves produce a trench-like shape. Surf zone fish were collected in significantly lower numbers than estuarine juveniles but entered brackish/ocean waters at similar sizes. Juveniles in surf zones consumed similar organisms (gammarid amphipods, crustacean larvae and insects) as in estuaries. Furthermore, stomach fullness indices (average = 2% of body weight) and growth rates (average = 0.4 mm day�����) were similar in surf zones and estuaries. At one surf zone, juvenile catch was positively correlated to short-term specific growth rates (14 days prior to capture). A bioenergetics modeling approach indicated that given current conditions, consumption rates accounted for more of the variation in growth than prey energetic content and temperature. Climate models predict future increases in fresh water temperature (1.5 to 5.8��C), sea surface temperature (1.2��C) and wave height (0.75 m) that could influence estuarine and surf zone use. Therefore, I developed a local mixing model based on these predictions to estimate future surf zone and estuarine water temperatures in two of the watersheds studied. Based on these temperature projections and the bioenergetics model, I predicted how juvenile specific growth rates would vary in both habitats. I determined that increases in water temperature in both habitats would reduce specific growth rates by 9 to 40% in surf zones and
estuaries if diet composition and consumption rates remain similar to present conditions. To compensate for the decline in growth, juveniles may increase their consumption rates or consume more energetically rich prey, if available. If they are not able to compensate, their size at the end of the season may be reduced, which could reduce their overall survival. These results confirm that a small number of suyearling Chinook salmon use sandy beach surf zones, mostly adjacent to estuary mouths, where they experience growth conditions comparable to estuaries. My findings indicate that, in certain situations, juvenile Chinook salmon surf zone use can be influenced by surf zone growth conditions, while variation in growth rates are themselves most strongly influenced by variation in consumption rates in surf zones and estuaries. Predicted changes in coastal western North American climate will likely modify juvenile growth conditions in the next 50 years, and potentially reduce overall survival. Additional insights into the potential impacts of climate change on juvenile salmon will require estimates of changes in the composition, energetic quality and abundance of prey communities inhabiting coastal environments. / Graduation date: 2013
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