Thesis (M.S.)--University of North Carolina Wilmington, 2008. / Title from PDF title page (viewed September 22, 2008) Includes bibliographical references (p. 60-62)

Thesis (Ph. D.)--Florida State University, 2005. / Advisor: Dr. Joel Kostka, Florida State University, College of Arts and Sciences, Dept. of Oceanography. Title and description from dissertation home page (viewed June 22, 2005). Document formatted into pages; contains xi, 108 pages. Includes bibliographical references.

No description available.

The capacity of the world’s coastal ecosystems to sequester carbon dioxide (CO2), termed “Blue Carbon,” has been a major focus of research in recent decades due to its potential to mitigate climate change. Vegetated coastal ecosystems such as mangroves, seagrass beds, and salt marshes represent a global area that is one to two orders of magnitude smaller than that of terrestrial forests, yet their contribution to long-term carbon sequestration is much greater per unit-area, in part because of their high productivity and efficiency in trapping suspended matter and associated organic carbon. Despite the value that Blue Carbon (BC) systems offer in sequestering carbon, as well as providing numerous other goods and services, these habitats are being lost at critical rates and require urgent action in order to prevent further degradation and loss. Recognition of the carbon sequestration value of vegetated coastal ecosystems provides a strong argument for their protection and restoration, and global efforts are now underway to include BC ecosystems into global carbon offset budgets, focusing on their optimal management to optimize CO2 sequestration and minimize CO2 emissions. Here, BC was investigated in the Cowichan Estuary in relation to habitat type (salt marsh, eelgrass meadow, non-vegetated mudflats, and oyster shell beds), and habitat degradation. Stored organic carbon (OC) and inorganic carbon (IC) were quantified in the top 20 cm depth of sediment cores, as well as in eelgrass and salt marsh vegetation, and then extrapolated to the areal extent of each habitat type based on a high resolution 1:12,000 scale base map of the estuary. Rates of sedimentation and carbon sequestration were quantified in each habitat type using 210Pb radiometric dating, and organic matter (OM) sources and quality were assessed in each habitat type using δ13C, C/N ratios and photopigment content in the sediments. A particular focus on the lower intertidal zone allowed us to examine the potential impact of industrial activity (log transport and storage) on the estuary’s capacity for carbon storage, as a result of a reduction of suitable habitat for eelgrass and microphytobenthos (MPB). Additionally, IC was quantified in aboveground oyster shell beds and buried oyster shell to assess inorganic storage. Finally, potential valuation of Blue Carbon in the Cowichan Estuary was investigated by comparing carbon sequestration to provincial greenhouse gas (GHG) emission equivalents as well as carbon sequestration in B.C. forests. We found that the salt marsh was the most important carbon reservoir, with a mean per-hectare sediment organic carbon (SOC) stock of 49.1 ± 19.9 Mg C ha-1, total ecosystem carbon stock (TECS) of 5443.75 Mg C, and carbon accumulation rate of 74 ± 23 g C m-2 yr-1. In the other habitats, we found SOC stocks and TECS respectively 19.1 ± 3.78 Mg C ha-1 and 3651.6 ± 72.3 Mg C in the upper mudflats, 16.9 ± 4.36 Mg C ha-1 and 1058.85 Mg C in the lower mudflats, 17.9 ± 1.21 Mg C ha−1 and 324.57 Mg C in the eelgrass meadow, and 9.43 ± 1.50 Mg C ha-1 and 59.4 Mg C in the oyster beds. The eelgrass meadow had a carbon accumulation rate of 38 ± 26 g C m-2 yr-1, while the mudflats could not successfully be dated due to erosion and/or mixing. Furthermore, the salt marsh contained the highest proportion of recalcitrant, terrestrial-derived root material which was more protected from hydrodynamic forces compared to other habitats. No pattern differences were observed between the carbon reservoirs or bulk properties of the log boom area (lower mudflat) compared to the upper mudflat, and thus there was no evidence that the log booms significantly decrease carbon sequestration in the areas where they make frequent contact with the seafloor. However, decreased chlorophyll a (chl a) concentrations in the lower mudflat sediment suggests a possible detrimental impact on microphytobenthos in addition to preventing the recolonization of the seagrass Zostera marina (Z. marina). Carbon stocks in the eelgrass meadow were similar to those of the mudflats. These carbon stocks were lower than global averages but consistent with those recently reported in low Z. marina meadows in the Pacific Northwest. Evidence of significant eelgrass vegetation outwelling necessitates further investigation to elucidate the degree to which these primary products are being decomposed or buried elsewhere in the estuary or open ocean. Since approximately half of the historical salt marsh habitat is currently reclaimed for agricultural and industrial use, consideration should be given to the role of the marsh system as a carbon reservoir in future land-use policy in the Cowichan Estuary. / Graduate / 2022-04-30

Understanding the maintenance of sexual systems is of great interest to evolutionary and ecological biologists because plant systems are extremely varied. Plant sexual systems have evolved to include not only complete plants with both male and female reproduction occurring on one plant (i.e., monoecious and hermaphroditic) but also plants with male and female function on separate plants (dioecious). The dioecious reproductive system can be used to test theories on niche differentiation given that having separate plants potentially allows for the exploitation of a broader niche. This increase in the realized niche is due to the ability for separate sexes to occupy different niches, which may occur in different physical habitats. Some dioecious plants have been shown to occur in areas biased to nearly 100% male or nearly 100% female, called spatial segregation of the sexes (SSS). Occupying a broader niche could increase fitness in some species when the separation is used for one sex to gain access to resources that increase reproductive success and/or if the separation inhibits deleterious competition. These two mechanisms have been previously proposed for the evolution of SSS in dioecious plants. The first mechanism suggests that males and females have evolved to occupy different niches due to differences in reproduction (sexual specialization). The hypothesis for the sexual specialization mechanism is that females should have higher fitness in female-majority sites and males should have higher fitness in male-majority sites. The second mechanism states that males and females occupy different niches due to competition between the sexes (niche partitioning). The hypothesis for niche partitioning states that inter-sexual competition should decrease fitness more than intra-sexual competition. These mechanisms are not mutually exclusive. In our research we use the salt-marsh grass Distichlis spicata as our study species because this plant is dioecious and because molecular markers have been developed to determine the sex of juvenile plants. These molecular markers are important for testing the niche partitioning hypothesis for SSS in juveniles. Furthermore, previous work in California has shown that plants occur in areas nearly 100% female and nearly 100% male called spatial segregation of the sexes (SSS). The previous research also showed that female-majority sites were higher in soil phosphorus than male-majority sites. We conduct all research, presented in the proceeding chapters, on Distichlis spicata in the Sand Lake estuary near Pacific City, Oregon and in the laboratory at Portland State University. In Chapter 1 we used field data to answer two questions: (1) Does Distichlis spicata exhibit SSS in Oregon, and (2) If SSS is occurring, do differences occur in plant form and function (sexual specialization) in reproductive female and male plants in female-majority and male-majority sites? We used a sex ratio survey and collected field data on reproductive males and females. Our results show that there are female-majority and male-majority areas and SSS is occurring in the Sand Lake Estuary. Results from our native plant data suggest that reproductive females perform better in female-majority sites compared to male-majority sites which could suggest that sexual specialization is occurring in females. We currently have a long term field reciprocal transplant experiment in place to further address this hypothesis. In Chapter 2 we use field dada to address the following questions: (1) Does site-specific soil nutrient content occur in August, when females have set seed? (2) Does sex-specific mycorrhizal colonization occur in reproductively mature plants? (3) Does sex-specific mycorrhizal colonization vary seasonally in natural populations? Inside the roots of D. spicata a symbiotic relationship is formed between plant and arbuscular mycorrhizal fungus (AM). The AM- plant relationship has been shown to thrive in phosphorus limited areas because the mycorrhizal fungus increases nutrient access to the plant. We analyzed the results of the field soil nutrient content and mycorrhizal colonization in roots of native Distichlis spicata from male-majority and female-majority sites. The root colonization included staining roots with trypan blue and viewing sections of the roots under the microscope. Our results show that female- majority sites are higher in phosphorus and are found to have higher AM colonization than male- majority sites in the field. In Chapter 3 we then reciprocally transplanted D. spicata plants in the field to address the following questions: (1) Does niche partitioning occur in D. spicata, and (2) If niche partitioning is occurring, which plants are competing more? Our reciprocal transplant experiment included seeds grown in intra-sexual, inter-sexual and no competition in cones, planted directly into the field, and allowed to grow for 15 months. After the 15 months was over we measured survival, dry weight and root/shoot ratio. The design of the experiment was to determine the effects of competition (intra-sexual and inter-sexual) and no competition on (single male and female) on survival, biomass and root/shoot ratios. Our results show that niche partitioning is occurring and plants in inter-sexual competition have significantly less biomass then intra-sexual competitors. In, Chapter 4, we conduct a laboratory experiment to address the following questions: (1) Do plants show plasticity in their response to root exudates of the competing plant in regards to the sexual phenotype of the competitor? (2) Do plants show plasticity in their response to root exudates of the competing plant with respect to the relatedness of the competitor? We use sterile seeds grown in 24-well plates containing liquid media. For each competing plant, we picked plants up out of the wells and into the competing plants wells so that plants only experienced media that the competing plant had grown. At no time do roots ever come into contact with one another. We measured primary root length, number of lateral roots, the number of root hairs, root/shoot ratio and total dry weight. We analyzed the study two different ways, one for sexual type competition (inter-sexual, intra-sexual, none) and for plant relationship (KIN, STRANGER and OWN). The results for the sexual type competition found that inter-sexual competition was greater for root/shoot ratio and dry weight. The results for plant relationship competition found that kin plants had a significantly greater number of lateral roots and a significantly longer primary root. The last chapter, Chapter 5, includes a summary of our conclusions. Our study found SSS occurring in the Sand Lake Estuary in Oregon with female-majority sites higher in phosphorus and root colonization higher in percent colonization of arbuscular mycorrhizal fungi compared to male-majority sites. Based on the sexual specialization hypothesis as a mechanism for SSS, we found that females had greater fitness in female-majority sites compared to male-majority sites, suggesting that sexual specialization is occurring in reproductive females. We then tested the niche partitioning hypothesis for SSS, and we found consistent lab and field results suggesting that niche partitioning due to inter-sexual competition is an explanation for why females and males D. spicata plants spatially segregate themselves at the juvenile life history stage. Furthermore, we found that plants that have the same mother had a significantly greater number of lateral roots and a significantly longer primary root. These results suggest that KIN plants respond differently to one another compared to plants paired with a plant not from the same mother (STRANGER) or when the plant is alone (OWN).

Biogeography provides a window into the evolutionary history of populations, and helps explain the diversity and distribution of life through time. Viewed from a systematic perspective, biogeographic studies generate convincing arguments to explain the relationships among organisms and categorize them into useful taxonomies. When taxonomies do not reflect evolutionary histories, inaccurate representations of biodiversity confound future studies and conservation efforts. Two thamnophiine snakes, Nerodia clarkii and Nerodia fasciata, harbor unique morphological and ecological adaptations that obscured natural groupings, leading to controversial taxonomic delimitations. Additionally, population declines documented in N. clarkii compressicauda and N. clarkii taeniata led managers to list N. clarkii taeniata as threatened in 1977. I generated a baseline for continued biogeographic and systematic study of the Nerodia clarkii/fasciata clade. I used mitochondrial DNA to build a parsimony-based haplotype network, infer the phylogenetic relationships between the two species and their thamnophiine relatives, and estimate the divergence times of major N. clarkii/fasciata clades. With these data, I tested biogeographic and systematic hypotheses about the origin and distribution of diversity in this clade. I used principal components analyses to summarize morphological data and discuss ecological observations in search of characters that may unite genetic or taxonomic units. The analyses revealed a peninsular and a panhandle clade in Florida that appeared to iv diverge as a result of Pleistocene glacial fluctuations. I found no support genetically, morphologically, or ecologically for the current taxonomy, indicating a need for range-wide research to generate revised nomenclature. My results do not support the protection status of N. clarkii taeniata

Soil organic carbon (SOC) is concentrated in coastal wetlands, and its permanence maintains a livable climate, yet dynamics that govern microbial activity and SOC persistence are not fully characterized in coastal wetlands. Though microbial activity is conventionally thought to facilitate SOC loss, soil microbes simultaneously direct SOC formation. In fact, microbially-processed materials constitute up to half of the terrestrial soil organic carbon pool. Environmental conditions can affect whether microbes yield a net gain or loss of SOC, yet there is little consensus on microbial drivers of soil carbon longevity in coastal ecosystems. I sought to identify which drivers of microbial activity have the greatest impact on SOC in salt marsh soils. To address this question, I conducted a meta-analysis using the PRISMA method. Based on an initial survey of 2,835 studies, numeric data on soil and ecosystem characteristics were collected across 50 studies on over 60 salt marshes located around the world. Integrative data analyses, including structural equation modeling (SEM), were applied to synthesized data to identify environmental drivers of SOC in salt marsh ecosystems. Across a wide range of study sites, analysis of over 20 variables shows that soil characteristics are tightly linked. Salinity, pH, nitrogen, and phosphorus are associated with increased microbial biomass and soil organic carbon. Correlations between microbial biomass carbon and SOC are strengthened by soil salinity and nitrogen, and they are weakened by moisture. Correlations were dependent on the means by which variables were measured, yet findings were consistent across study sites. These results suggest that soil carbon content is affected by drivers of microbial activity. Observational findings set the stage for experimental strategies that parcel causal effects of microbial activity on SOC from confounding effects of covariant environmental conditions. I identified that nitrogen, phosphorus, salinity, pH, and moisture influence microbial contributions to SOC. These environmental drivers, as well as microbial biomass and greenhouse gas flux, should be considered key indicators of soil health when assessing the sustainability of coastal SOC. Identification of environmental drivers of microbial function enables design of land management strategies that promote conditions conducive to coastal soil carbon longevity.

Salt marshes are important habitats that provide many ecosystem services, but they are susceptible to the impacts of sea level rise (SLR), often resulting in emergent vegetation loss. In areas with enough sediment input, marshes can keep pace with SLR by gaining elevation or through upland migration. However, salt marshes in areas with limited sediment input, such as the Grand Bay National Estuarine Research Reserve, often cannot keep pace with sea level rise. Additionally, the rate of SLR is increasing making it more difficult for marshes to keep pace. To assess the short-term response of marsh vegetation to sea level rise, percent cover, stem density, and elevation, data from 2016 to 2020 in four different marsh elevation zones were analyzed in this study. Results demonstrated that the four marsh elevation zones are responding disparately to SLR. These findings indicate that it is imperative to implement restoration plans to account for site variability to conserve these vital habitats.

No description available.

The effect of cattle grazing on the abundance and distribution of vegetation, burrowing crabs (Uca rapax, Uca pugnax, and Sesarma cinereum), marsh periwinkles (Littoraria irrorata), horn snails (Cerithidea pliculosa), and salt marsh snails (Melampus bidentatus) was evaluated over four seasons (summer 2000, fall 2000, winter 2001, and spring 2001) in grazed and ungrazed treatments. A Galveston Island salt marsh adjacent to Snake Island Cove was sampled at five elevations, from the water's edge to the high tidal flats. Data were analyzed for statistical differences using a two-way ANOVA in SAS. Cattle grazing may affect the vegetation and macroinvertebrate communities in salt marshes through trampling and herbivory. Vegetation resources available to other herbivores are decreased by the direct consumption of plant material by cattle. Spartina alterniflora and Salicornia virginica heights were significantly greater in ungrazed treatments than grazed for every season in the edge, upper, and middle elevation zones. Total aerial vegetative cover was also reduced significantly in grazed treatments, with the greatest impact in the edge and upper marsh. In the ungrazed treatments, S. alterniflora stem density was significantly greater in edge elevations, while both S. virginica percent cover and stem density in the edge elevation was greater. Burrowing crab populations were greater in the upper marsh and edge habitat of ungrazed treatments, while significantly greater in most of the middle marsh habitats of the grazed treatment. Size of burrowing crabs was generally significantly greater in ungrazed treatments. Cerithidea pliculosa size decreased in grazed treatments, but population had an overall increase in grazed treatments. Littoraria irrorata had very few differences between treatments, although few specimens were found. Melampus bidentatus populations were too small to evaluate thoroughly. Macroinvertebrate populations could be used to assess the overall health of grazed salt marshes.