84 research outputs found
Benthic Biofilm Potential for Organic Carbon Accumulation in Salt Marsh Sediments
Coastal salt marshes are productive environments with high potential for carbon accumulation and storage. Even though organic carbon in salt marsh sediment is typically attributed to plant biomass, it can also be produced by benthic photosynthetic biofilms. These biofilms, generally composed of diatoms and their secretions, are known for their high primary productivity and contribution to the basal food web. The growth of biofilms and the preservation of carbon produced by biofilms depends on the amount of sedimentation; low sedimentation rates will favor decomposition, while high sedimentation rates could decrease biofilm productivity. In this study, we conducted laboratory experiments to test (1) if biofilms can potentially accumulate carbon in marsh soil and (2) how different sedimentation rates affect the amount of carbon accumulation. Containers filled with a settled mud bed were inoculated with natural biofilms collected from a marsh surface and allowed to grow with favorable light exposure, nutrient supply, and absence of grazing. Mud was added weekly in different amounts, resulting in an equivalent sedimentation rate from 12 to 189 mm/yr. After 11 weeks, the sediment columns were sampled and analyzed for chl a, organic matter via loss on ignition (LOI), and total organic carbon (TOC). Chl a accumulation rates ranged from 123 to 534 mg/cm2/yr, organic matter accumulation ranged from 86 to 456 g/m2/yr, and TOC accumulation rates ranged from 31 to 211 g/m2/yr. These values are on the same order of magnitude of marsh carbon accumulation rates measured in the field. All three metrics (chl a, organic matter, and TOC) increased with increased sedimentation rate. These results show that biofilms can potentially contribute to carbon accumulation in salt marsh soils. Furthermore, areas with high sedimentation rates have the potential for higher amounts of organic matter from biofilms in the sediment
Role of tidal wetland stability in lateral fluxes of particulate organic matter and carbon
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research-Biogeosciences 124(5), (2019): 1265-1277, doi:10.1029/2018JG004920.Tidal wetland fluxes of particulate organic matter and carbon (POM, POC) are important terms in global budgets but remain poorly constrained. Given the link between sediment fluxes and wetland stability, POM and POC fluxes should also be related to stability. We measured POM and POC fluxes in eight microtidal salt marsh channels, with net POM fluxes ranging between −121 ± 33 (export) and 102 ± 28 (import) g OM·m−2·year−1 and net POC fluxes ranging between −52 ± 14 and 43 ± 12 g C·m−2·year−1. A regression employing two measures of stability, the unvegetated‐vegetated marsh ratio (UVVR) and elevation, explained >95% of the variation in net fluxes. The regression indicates that marshes with lower elevation and UVVR import POM and POC while higher elevation marshes with high UVVR export POM and POC. We applied these relationships to marsh units within Barnegat Bay, New Jersey, USA, finding a net POM import of 2,355 ± 1,570 Mg OM/year (15 ± 10 g OM·m−2·year−1) and a net POC import of 1,263 ± 632 Mg C/year (8 ± 4 g C·m−2·year−1). The magnitude of this import was similar to an estimate of POM and POC export due to edge erosion (−2,535 Mg OM/year and − 1,291 Mg C/year), suggesting that this system may be neutral from a POM and POC perspective. In terms of a net budget, a disintegrating wetland should release organic material, while a stable wetland should trap material. This study quantifies that concept and demonstrates a linkage between POM/POC flux and geomorphic stability.Use of brand names is for identification purposes only and does not constitute endorsement by the U.S. Government. This study was supported by the USGS Coastal and Marine Geology Program, the Department of the Interior Hurricane Sandy Recovery program (GS2‐2D), and the USGS Mendenhall Post‐doctoral Research Program. Viktoria Unger and Paula Zelanko are acknowledged for field and lab assistance. Core collection was funded under NJ SeaGrant/NOAA Grant 6210‐0011. Gil Pontius provided helpful feedback on statistical measures. Kevin Kroeger and two anonymous reviewers provided constructive reviews of the manuscript. All time series and water sample data are available at the U.S. Geological Survey's Oceanographic Time‐Series Data Collection (at https://stellwagen.er.usgs.gov/).2019-10-2
Vegetation Dieback in the Mississippi River Delta Triggered by Acute Drought and Chronic Relative Sea-level Rise
Vegetation dieback and recovery may be dependent on the interplay between infrequent acute disturbances and underlying chronic stresses. Coastal wetlands are vulnerable to the chronic stress of sea-level rise, which may affect their susceptibility to acute disturbance events. Here, we show that a large-scale vegetation dieback in the Mississippi River Delta was precipitated by salt-water incursion during an extreme drought in the summer of 2012 and was most severe in areas exposed to greater flooding. Using 16 years of data (2007-2022) from a coastwide network of monitoring stations, we show that the impacts of the dieback lasted five years and that recovery was only partial in areas exposed to greater inundation. Dieback marshes experienced an increase in percent time flooded from 43% in 2007 to 75% in 2022 and a decline in vegetation cover and species richness over the same period. Thus, while drought-induced high salinities and soil saturation triggered a significant dieback event, the chronic increase in inundation is causing a longer-term decline in cover, more widespread losses, and reduced capacity to recover from acute stressors. Overall, our findings point to the importance of mitigating the underlying stresses to foster resilience to both acute and persistent causes of vegetation loss
Elevated temperature and nutrients lead to increased N2O emissions from salt marsh soils from cold and warm climates
Salt marshes can attenuate nutrient pollution and store large amounts of ‘blue carbon’ in their soils, however, the value of sequestered carbon may be partially offset by nitrous oxide (N2O) emissions. Global climate and land use changes result in higher temperatures and inputs of reactive nitrogen (Nr) into coastal zones. Here, we investigated the combined effects of elevated temperature (ambient + 5℃) and Nr (double ambient concentrations) on nitrogen processing in marsh soils from two climatic regions (Quebec, Canada and Louisiana, U.S.) with two vegetation types, Sporobolus alterniflorus (= Spartina alterniflora) and Sporobolus pumilus (= Spartina patens), using 24-h laboratory incubation experiments. Potential N2O fluxes increased from minor sinks to major sources following elevated treatments across all four marsh sites. One day of potential N2O emissions under elevated treatments (representing either long-term sea surface warming or short-term ocean heatwaves effects on coastal marsh soil temperatures alongside pulses of N loading) offset 15–60% of the potential annual ambient N2O sink, depending on marsh site and vegetation type. Rates of potential denitrification were generally higher in high latitude than in low latitude marsh soils under ambient treatments, with low ratios of N2O:N2 indicating complete denitrification in high latitude marsh soils. Under elevated temperature and Nr treatments, potential denitrification was lower in high latitude soil but higher in low latitude soil as compared to ambient conditions, with incomplete denitrification observed except in Louisiana S. pumilus. Overall, our findings suggest that a combined increase in temperature and Nr has the potential to reduce salt marsh greenhouse gas (GHG) sinks under future global change scenarios
Salinity and Simulated Herbivory Influence Spartina alterniflora Traits and Defense Strategy
Sea level rise is expected to push saline waters into previously fresher regions of estuaries, and higher salinities may expose oligohaline marshes to invertebrate herbivores typically constrained by salinity. The smooth cordgrass, Spartina alterniflora (syn. Sporobolus alterniflorus), can defend itself against herbivores in polyhaline marshes, however it is not known if S. alterniflora’s defense varies along the mesohaline to oligohaline marsh gradient in estuaries. I found that S. alterniflora from a mesohaline marsh is better defended than plants from an oligohaline marsh, supporting the optimal defense theory. Higher salinity treatments lowered carbon content, C:N, and new stem biomass production, traits associated with a tolerance strategy, suggesting that salinity may mediate the defense response of S. alterniflora. Further, simulated herbivory increased the nitrogen content and decreased C:N of S. alterniflora. This indicates that grazing may increase S. alterniflora susceptibility to future herbivory via improved forage quality. Simulated herbivory also decreased both belowground and new stem biomass production, highlighting a potential pathway in which herbivory can indirectly facilitate marsh loss, as S. alterniflora biomass is critical for vertical accretion and marsh stability under future sea level rise scenarios
Habilidades funcionais, nível de actividade, integração na comunidade e saúde em idosos institucionalizados em lar: resultados preliminares
São escassos os estudos portugueses que avaliam o nível de funcionalidade, o nível de actividade e a saúde em idosos institucionalizados em lar.
Objectivos: Estimar os meses de institucionalização dos idosos e as causas que conduziram à institucionalização em lar, bem como o número de idosos que partilha o seu quarto com outros. Estimar as Habilidades Funcionais dos idosos, o tipo de actividades relatadas, dentro e fora da instituição (Nível de Actividade e Integração na Comunidade) e o grau de saúde (objectiva e subjectiva). Analisar a relação entre estas quatro dimensões e analisar a relação destas com algumas variáveis demográficas (idade, género).
Métodos: 35 idosos institucionalizados em lar (idade média=80.20 anos; DP=6.263) completaram o Questionário de Informação Pessoal (QIP; Fernándes-Ballesteros, 1995; Maia et al., 2013). Para a análise dos dados recorremos ao SPSS 21.
Resultados: A grande generalidade dos idosos está institucionalizada há mais de 16 meses, por motivos maioritariamente de saúde (65,7%), partilha o quarto com terceiros (71.4%) e é autónoma, não necessitando de ajuda (56.7%) em actividades como o cuidado pessoal, comer, vestir/despir, andar, levantar/deitar. Quando se trata das actividades mais complexas, como a administração de dinheiro, uso do telefone ou ida às compras, o grau de dependência aumenta (27.6% dos sujeitos necessitam de muita ajuda e 35.2% de alguma ajuda). Verifica-se que 72.9% da população está inactiva, visto limitar-se a ver televisão ou a ouvir rádio e apenas 14.3% dos idosos se dedicam a actividades fora da Instituição. Os actos religiosos têm uma larga adesão (88.6%). 79.4% dos idosos reporta problemas de mobilidade e 35.3% problemas de foro psicológico. Verifica-se que 45.7% percepcionam a saúde como má, com as mulheres a percepcionarem a sua saúde mais negativamente do que os homens. Nenhum dos idosos, de ambos os géneros, percepciona a sua saúde como boa ou excelente (0%). A dimensão Nível de Actividade apresenta uma correlação positiva com a dimensão Integração na Comunidade (r=.448*). O género apresenta uma correlação significativa com a dimensão Habilidades Funcionais (rho=.383*) e com a dimensão Saúde (r=.414*). O estado civil apresentou uma correlação positiva com as Habilidades Funcionais (rho=.419*) e o grau de escolaridade apresentou uma correlação negativa e com a dimensão Saúde (r=-.446*).
Conclusões: Na nossa amostra a institucionalização é causada maioritariamente devido a problemas de saúde. A maioria dos idosos partilha o seu quarto o que pode afectar a sua intimidade e bem-estar. Apesar da maioria dos idosos ser funcionalmente autónoma, a grande generalidade apresenta uma vida pautada pela inactividade e por fracos laços com o exterior. As mulheres percepcionam a sua saúde mais negativamente do que os homens. Importa assim, desenvolver estratégias que conduzam a um envelhecimento activo destes idosos
Organic Matter and Nutrient Cycling in Coastal Wetlands and Submerged Aquatic Ecosystems in an Age of Rapid Environmental Change—The Anthropocene
Coastal ecosystems, such as marshes, mangroves, seagrasses and estuaries, are biogeochemical hotspots, receiving and transforming organic matter and nutrients from terrestrial watersheds and the coastal ocean [...
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