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Journal articles on the topic 'Salt marsh'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Haacks, Manfred, and Dietbert Thannheiser. "The salt-marsh vegetation of New Zealand." Phytocoenologia 33, no. 2-3 (2003): 267–88. http://dx.doi.org/10.1127/0340-269x/2003/0033-0267.

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2

Silvestri, Sonia, Marco Marani, Jeff Settle, Fabio Benvenuto, and Alessandro Marani. "Salt marsh vegetation radiometry." Remote Sensing of Environment 80, no. 3 (2002): 473–82. http://dx.doi.org/10.1016/s0034-4257(01)00325-x.

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3

Broome, Stephen W., Ernest D. Seneca, and William W. Woodhouse. "Tidal salt marsh restoration." Aquatic Botany 32, no. 1-2 (1988): 1–22. http://dx.doi.org/10.1016/0304-3770(88)90085-x.

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4

Erfanzadeh, Reza, Julien Pétillon, Jean-Pierre Maelfait, and Maurice Hoffmann. "Environmental determinism versus biotic stochasticity in the appearance of plant species in salt-marsh succession." Plant Ecology and Evolution 143, no. (1) (2010): 43–50. https://doi.org/10.5091/plecevo.2010.422.

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<b>Background and aims</b> – It is generally accepted that in terrestrial ecosystems the occurrence and abundance of plant species in late successional stages can be predicted accurately from prevailing soil conditions, whereas in early succession their presence is much more influenced by chance events (e.g. propagule availability). Late successional vegetation stages would therefore be deterministically structured, while early succession would be dominated by more stochastic features. To test this hypothesis in salt marsh conditions, we compared the effect of abiotic environmental factors on

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5

Meyer, David L., and Martin H. Posey. "Influence of Salt Marsh Size and Landscape Setting on Salt Marsh Nekton Populations." Estuaries and Coasts 37, no. 3 (2013): 548–60. http://dx.doi.org/10.1007/s12237-013-9707-z.

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6

Guimond, Julia, and Joseph Tamborski. "Salt Marsh Hydrogeology: A Review." Water 13, no. 4 (2021): 543. http://dx.doi.org/10.3390/w13040543.

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Groundwater–surface water exchange in salt marsh ecosystems mediates nearshore salt, nutrient, and carbon budgets with implications for biological productivity and global climate. Despite their importance, a synthesis of salt marsh groundwater studies is lacking. In this review, we summarize drivers mediating salt marsh hydrogeology, review field and modeling techniques, and discuss patterns of exchange. New data from a Delaware seepage meter study are reported which highlight small-scale spatial variability in exchange rates. A synthesis of the salt marsh hydrogeology literature reveals a pos

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7

Gulzar, Salman, M. Ajmal Khan, and Irwin A. Ungar. "Salt Tolerance of a Coastal Salt Marsh Grass." Communications in Soil Science and Plant Analysis 34, no. 17-18 (2003): 2595–605. http://dx.doi.org/10.1081/css-120024787.

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8

Ormsby, E. "A Salt Marsh Near Truro." Literary Imagination 6, no. 1 (2004): 148. http://dx.doi.org/10.1093/litimag/6.1.148.

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9

Drake, Bert G. "Photosynthesis of salt marsh species." Aquatic Botany 34, no. 1-3 (1989): 167–80. http://dx.doi.org/10.1016/0304-3770(89)90055-7.

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10

Vernberg, F. John. "Salt-marsh processes: A Review." Environmental Toxicology and Chemistry 12, no. 12 (1993): 2167–95. http://dx.doi.org/10.1002/etc.5620121203.

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11

de Groot, Alma V., Roos M. Veeneklaas, and Jan P. Bakker. "Sand in the salt marsh: Contribution of high-energy conditions to salt-marsh accretion." Marine Geology 282, no. 3-4 (2011): 240–54. http://dx.doi.org/10.1016/j.margeo.2011.03.002.

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12

Campbell, Anthony, and Yeqiao Wang. "Assessment of Salt Marsh Change on Assateague Island National Seashore Between 1962 and 2016." Photogrammetric Engineering & Remote Sensing 86, no. 3 (2020): 187–94. http://dx.doi.org/10.14358/pers.86.3.187.

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Salt marshes provide extensive ecosystem services, including high biodiversity, denitrification, and wave attenuation. In the mid-Atlantic, sea level rise is predicted to affect salt marsh ecosystems severely. This study mapped the entirety of Assateague Island with Very High Resolution satellite imagery and object-based methods to determine an accurate salt marsh baseline for change analysis. Topobathy-metric light detection and ranging was used to map the salt marsh and model expected tidal effects. The satellite imagery, collected in 2016 and classified at two hierarchical thematic schemes,

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13

Leonardi, Nicoletta, Neil K. Ganju, and Sergio Fagherazzi. "A linear relationship between wave power and erosion determines salt-marsh resilience to violent storms and hurricanes." Proceedings of the National Academy of Sciences 113, no. 1 (2015): 64–68. http://dx.doi.org/10.1073/pnas.1510095112.

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Salt marsh losses have been documented worldwide because of land use change, wave erosion, and sea-level rise. It is still unclear how resistant salt marshes are to extreme storms and whether they can survive multiple events without collapsing. Based on a large dataset of salt marsh lateral erosion rates collected around the world, here, we determine the general response of salt marsh boundaries to wave action under normal and extreme weather conditions. As wave energy increases, salt marsh response to wind waves remains linear, and there is not a critical threshold in wave energy above which

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14

Bakker, J. P., and Y. Vries. "Germination and early establishment of lower salt-marsh species in grazed and mown salt marsh." Journal of Vegetation Science 3, no. 2 (1992): 247–52. http://dx.doi.org/10.2307/3235686.

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15

Geissel, W., H. Shellhammer, and H. T. Harvey. "The Ecology of the Salt-Marsh Harvest Mouse (Reithrodontomys raviventris) in a Diked Salt Marsh." Journal of Mammalogy 69, no. 4 (1988): 696–703. http://dx.doi.org/10.2307/1381624.

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16

Bakker, J. P., L. Gálvez Bravo, and A. M. Mouissie. "Dispersal by cattle of salt-marsh and dune species into salt-marsh and dune communities." Plant Ecology 197, no. 1 (2007): 43–54. http://dx.doi.org/10.1007/s11258-007-9358-x.

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17

Chen, Z. P., J. C. Dai, J. W. Zeng, and R. J. Li. "Application of Hydro-morphodynamic Modelling in Coastal Salt Marsh Management." Journal of Physics: Conference Series 2486, no. 1 (2023): 012037. http://dx.doi.org/10.1088/1742-6596/2486/1/012037.

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Abstract Salt marshes are widespread in estuarine coastal areas and are one of the most productive natural ecosystems in the world. More importantly, the role of salt marshes in coastal protection is of increasing interest, as salt marshes significantly reduce wave height and stabilize substrates. However, the application of hydrodynamic models for coastal salt marsh management is still uncommon. In this study, TELEMAC is used to set up a hydro-morphodynamic model to simulate the dynamic process in the study area. After that, the influence of hydrodynamic stress on the salt marshes under natur

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18

Calabon, Mark S., E. B. Gareth Jones, Itthayakorn Promputtha, and Kevin D. Hyde. "Fungal Biodiversity in Salt Marsh Ecosystems." Journal of Fungi 7, no. 8 (2021): 648. http://dx.doi.org/10.3390/jof7080648.

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This review brings together the research efforts on salt marsh fungi, including their geographical distribution and host association. A total of 486 taxa associated with different hosts in salt marsh ecosystems are listed in this review. The taxa belong to three phyla wherein Ascomycota dominates the taxa from salt marsh ecosystems accounting for 95.27% (463 taxa). The Basidiomycota and Mucoromycota constitute 19 taxa and four taxa, respectively. Dothideomycetes has the highest number of taxa, which comprises 47.12% (229 taxa), followed by Sordariomycetes with 167 taxa (34.36%). Pleosporales i

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19

Siemes, Rutger W. A., Bas W. Borsje, Roy J. Daggenvoorde, and Suzanne J. M. H. Hulscher. "Artificial Structures Steer Morphological Development of Salt Marshes: A Model Study." Journal of Marine Science and Engineering 8, no. 5 (2020): 326. http://dx.doi.org/10.3390/jmse8050326.

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Salt marshes are increasingly recognized as resilient and sustainable supplements to traditional engineering structures for protecting coasts against flooding. Nevertheless, many salt marshes face severe erosion. There is a consensus that providing structures that create sheltered conditions from high energetic conditions can improve the potential for salt marsh growth. However, little proof is provided on the explicit influence of structures to promote salt marsh growth. This paper investigates how artificial structures can be used to steer the morphological development of salt marshes. A mor

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20

Kuroda, Naoki, Katsuhide Yokoyama, and Tadaharu Ishikawa. "Development of a Practical Model for Predicting Soil Salinity in a Salt Marsh in the Arakawa River Estuary." Water 13, no. 15 (2021): 2054. http://dx.doi.org/10.3390/w13152054.

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Our group has studied the spatiotemporal variation of soil and water salinity in an artificial salt marsh along the Arakawa River estuary and developed a practical model for predicting soil salinity. The salinity of the salt marsh and the water level of a nearby channel were measured once a month for 13 consecutive months. The vertical profile of the soil salinity in the salt marsh was measured once monthly over the same period. A numerical flow simulation adopting the shallow water model faithfully reproduced the salinity variation in the salt marsh. Further, we developed a soil salinity mode

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21

Campbell, Anthony, and Yeqiao Wang. "High Spatial Resolution Remote Sensing for Salt Marsh Mapping and Change Analysis at Fire Island National Seashore." Remote Sensing 11, no. 9 (2019): 1107. http://dx.doi.org/10.3390/rs11091107.

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Salt marshes are changing due to natural and anthropogenic stressors such as sea level rise, nutrient enrichment, herbivory, storm surge, and coastal development. This study analyzes salt marsh change at Fire Island National Seashore (FIIS), a nationally protected area, using object-based image analysis (OBIA) to classify a combination of data from Worldview-2 and Worldview-3 satellites, topobathymetric Light Detection and Ranging (LiDAR), and National Agricultural Imagery Program (NAIP) aerial imageries acquired from 1994 to 2017. The salt marsh classification was trained and tested with vege

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22

Adams, Janine B., Jacqueline L. Raw, Taryn Riddin, Johan Wasserman, and Lara Van Niekerk. "Salt Marsh Restoration for the Provision of Multiple Ecosystem Services." Diversity 13, no. 12 (2021): 680. http://dx.doi.org/10.3390/d13120680.

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Restoration of salt marsh is urgent, as these ecosystems provide natural coastal protection from sea-level rise impacts, contribute towards climate change mitigation, and provide multiple ecosystem services including supporting livelihoods. This study identified potential restoration sites for intervention where agricultural and degraded land could be returned to salt marsh at a national scale in South African estuaries. Overall, successful restoration of salt marsh in some estuaries will require addressing additional pressures such as freshwater inflow reduction and deterioration of water qua

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23

Seyler, Lauren M., Lora M. McGuinness, and Lee J. Kerkhof. "Crenarchaeal heterotrophy in salt marsh sediments." ISME Journal 8, no. 7 (2014): 1534–43. http://dx.doi.org/10.1038/ismej.2014.15.

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24

Ingoldsby, Joseph Emmanuel. "Vanishing Landscapes: The Atlantic Salt Marsh." Leonardo 42, no. 2 (2009): 124–31. http://dx.doi.org/10.1162/leon.2009.42.2.124.

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The author, trained in art and landscape architecture, utilizes observation of nature and culture as a central focus in his art. The work involves research, scientific collaboration and examination, documentation, analysis and synthesis using art, science and technology for environmental advocacy. The focus for these works has been on the coastal landscape of New England, the imprint of humans on land and sea, and the impact of climate change on the marine landscape and fisheries of New England.

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25

Smith, Lora M., and John R. Reinfelder. "Mercury volatilization from salt marsh sediments." Journal of Geophysical Research: Biogeosciences 114, G2 (2009): n/a. http://dx.doi.org/10.1029/2009jg000979.

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26

Renner, Rebecca. "California salt marsh contaminates swimming beach." Environmental Science & Technology 35, no. 15 (2001): 320A—321A. http://dx.doi.org/10.1021/es0124360.

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27

Townend, Ian, Caroline Fletcher, Michiel Knappen, and Kate Rossington. "A review of salt marsh dynamics." Water and Environment Journal 25, no. 4 (2010): 477–88. http://dx.doi.org/10.1111/j.1747-6593.2010.00243.x.

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28

Knott, Jayne Fifield, William Kensett Nuttle, and Harold Field Hemond. "Hydrologic parameters of salt marsh peat." Hydrological Processes 1, no. 2 (1987): 211–20. http://dx.doi.org/10.1002/hyp.3360010208.

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29

Paul, Edward. "Modeling productivity of a salt marsh." Cell Biophysics 11, no. 1 (1987): 57–63. http://dx.doi.org/10.1007/bf02797112.

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30

Ouyang, X., and S. Y. Lee. "Updated estimates of carbon accumulation rates in coastal marsh sediments." Biogeosciences 11, no. 18 (2014): 5057–71. http://dx.doi.org/10.5194/bg-11-5057-2014.

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Abstract. Studies on carbon stock in salt marsh sediments have increased since the review by Chmura et al. (2003). However, uncertainties exist in estimating global carbon storage in these vulnerable coastal habitats, thus hindering the assessment of their importance. Combining direct data and indirect estimation, this study compiled studies involving 143 sites across the Southern and Northern hemispheres, and provides an updated estimate of the global average carbon accumulation rate (CAR) at 244.7 g C m−2 yr−1 in salt marsh sediments. Based on region-specific CAR and estimates of salt marsh

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31

Jacobson, Heather A., and George L. Jacobson Jr. "Variability of vegetation in tidal marshes of Maine, U.S.A." Canadian Journal of Botany 67, no. 1 (1989): 230–38. http://dx.doi.org/10.1139/b89-032.

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Systematic studies of vegetation on 18 salt marshes along the coast of Maine show that the vegetation is highly variable in species composition, species richness, and zonation pattern. Marshes with high species richness are found in relatively stable geologic settings, while unstable marshes at the base of erodible bluffs have low species richness. Species composition is influenced by freshwater input. Salt-marsh zonation varies greatly in both the number of zones present per marsh and the species assemblages within zones. With a few notable exceptions, the vegetation of salt marshes in southe

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32

Hinshaw, Sarra E., Corianne Tatariw, Nikaela Flournoy, et al. "Vegetation Loss Decreases Salt Marsh Denitrification Capacity: Implications for Marsh Erosion." Environmental Science & Technology 51, no. 15 (2017): 8245–53. http://dx.doi.org/10.1021/acs.est.7b00618.

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33

O’Connor, Mary I., Christy R. Violin, Andrea Anton, Laura M. Ladwig, and Michael F. Piehler. "Salt marsh stabilization affects algal primary producers at the marsh edge." Wetlands Ecology and Management 19, no. 2 (2011): 131–40. http://dx.doi.org/10.1007/s11273-010-9206-y.

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34

Forbrich, Inke, and Anne E. Giblin. "Marsh‐atmosphere CO 2 exchange in a New England salt marsh." Journal of Geophysical Research: Biogeosciences 120, no. 9 (2015): 1825–38. http://dx.doi.org/10.1002/2015jg003044.

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35

Richards, David F., Adam M. Milewski, Steffan Becker, et al. "Evaluation and Analysis of Remote Sensing-Based Approach for Salt Marsh Monitoring." Remote Sensing 16, no. 1 (2023): 2. http://dx.doi.org/10.3390/rs16010002.

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In the United States (US), salt marshes are especially vulnerable to the effects of projected sea level rise, increased storm frequency, and climatic changes. Sentinel-2 data offer the opportunity to observe the land surface at high spatial resolutions (10 m). The Sentinel-2 data, encompassing Cumberland Island National Seashore, Fort Pulaski National Monument, and Canaveral National Seashore, were analyzed to identify temporal changes in salt marsh presence from 2016 to 2020. ENVI-derived unsupervised and supervised classification algorithms were applied to determine the most appropriate proc

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36

Brooks, Helen, Iris MÃ¶ller, Tom Spencer, Kate Royse, and Simon James Price. "GEOTECHNICAL PROPERTIES OF SALT MARSH AND TIDAL FLAT SUBSTRATES AT TILLINGHAM, ESSEX, UK." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 55. http://dx.doi.org/10.9753/icce.v36.papers.55.

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Salt marshes and, to a lesser extent, tidal flats, attenuate incoming hydrodynamic energy, thus reducing flood and erosion risk in the coastal hinterland. However, marshes are declining both globally and regionally (the Northwest European region). Salt marsh resistance to incoming hydrodynamic forcing depends on marsh biological, geochemical and geotechnical properties. However, there currently exists no systematic study of marsh geotechnical properties and how these may impact both marsh edge and marsh surface erosion processes (e.g. surface removal, cliff undercutting, gravitational slumping

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37

Bertness, Mark D., Laura Gough, and Scott W. Shumway. "Salt Tolerances and The Distribution of Fugitive Salt Marsh Plants." Ecology 73, no. 5 (1992): 1842–51. http://dx.doi.org/10.2307/1940035.

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38

Partridge, T. R., and J. B. Wilson. "Salt tolerance of salt marsh plants of Otago, New Zealand." New Zealand Journal of Botany 25, no. 4 (1987): 559–66. http://dx.doi.org/10.1080/0028825x.1987.10410086.

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39

Duarte, B., J. Freitas, T. Couto, et al. "New multi-metric Salt Marsh Sediment Microbial Index (SSMI) application to salt marsh sediments ecological status assessment." Ecological Indicators 29 (June 2013): 390–97. http://dx.doi.org/10.1016/j.ecolind.2013.01.008.

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40

Dixon, Daniel. "EVALUATION OF CDC LIGHT TRAP, BG SENTINEL TRAP, AND MMX TRAP FOR THE COLLECTION OF SALT MARSH MOSQUITOES IN ANASTASIA STATE PARK, SAINT AUGUSTINE, FLORIDA." Journal of the Florida Mosquito Control Association 66, no. 1 (2021): 64–67. http://dx.doi.org/10.32473/jfmca.v66i1.127626.

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Salt marsh mosquitoes are major nuisance pests during the periods of high mosquito activity, especially after major storm events. In 2016-2017, Saint John’s County, Florida, USA was struck by two major hurricanes that resulted in multiple outbreaks of salt marsh mosquito populations. To optimize the surveillance of two salt marsh mosquitoes, (Aedes taeniorhynchus and Ae. sollicitans, three types of traps (the Centers for Disease Control (CDC) Light trap, Biogents Sentinel (BG) trap and Counter Flow Geometry Model (MMX) trap were tested for their capacity to capture the highest numbers of high

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41

Chen, M. Y., F. Luo, and J. C. Dai. "Study on the Influence of Salt Marsh Vegetation on Tidal Current and Sediment Transport in Intertidal Zone." Journal of Physics: Conference Series 2486, no. 1 (2023): 012049. http://dx.doi.org/10.1088/1742-6596/2486/1/012049.

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Abstract Due to the sensitivity of the environment and immoderate human activities, the coastal zone in China is facing resource conflicts and environmental pressures. Salt marsh vegetation is regarded as an important measure for coastal ecological restoration. Therefore, it is of practical significance to study the influence of salt marsh vegetation on hydro-sediment dynamics. Based on the measured topography and tidal sediment data, a generalized model of salt marsh vegetation is established to study its effects on the dynamics of nearshore water and sediment. The results show that salt mars

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42

Shute, Kyle E., Susan C. Loeb, and David S. Jachowski. "Seasonal Shifts in Nocturnal Habitat Use by Coastal Bat Species." Journal of Wildlife Management 85, no. 5 (2021): 964–78. https://doi.org/10.5281/zenodo.13489902.

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(Uploaded by Plazi for the Bat Literature Project) Sensitivity of bats to land use change depends on their foraging ecology, which varies among species based on ecomorphological traits. Additionally, because prey availability, vegetative clutter, and temperature change throughout the year, some species may display seasonal shifts in their nocturnal habitat use. In the Coastal Plain of South Carolina, USA, the northern long‐eared bat (Myotis septentrionalis), southeastern myotis (Myotis austroriparius), tri‐colored bat (Perimyotis subflavus), and northern yellow bat (Lasiurus intermedius) are s

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43

Shute, Kyle E., Susan C. Loeb, and David S. Jachowski. "Seasonal Shifts in Nocturnal Habitat Use by Coastal Bat Species." Journal of Wildlife Management 85, no. 5 (2021): 964–78. https://doi.org/10.5281/zenodo.13489902.

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(Uploaded by Plazi for the Bat Literature Project) Sensitivity of bats to land use change depends on their foraging ecology, which varies among species based on ecomorphological traits. Additionally, because prey availability, vegetative clutter, and temperature change throughout the year, some species may display seasonal shifts in their nocturnal habitat use. In the Coastal Plain of South Carolina, USA, the northern long‐eared bat (Myotis septentrionalis), southeastern myotis (Myotis austroriparius), tri‐colored bat (Perimyotis subflavus), and northern yellow bat (Lasiurus intermedius) are s

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44

Shute, Kyle E., Susan C. Loeb, and David S. Jachowski. "Seasonal Shifts in Nocturnal Habitat Use by Coastal Bat Species." Journal of Wildlife Management 85, no. 5 (2021): 964–78. https://doi.org/10.5281/zenodo.13489902.

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(Uploaded by Plazi for the Bat Literature Project) Sensitivity of bats to land use change depends on their foraging ecology, which varies among species based on ecomorphological traits. Additionally, because prey availability, vegetative clutter, and temperature change throughout the year, some species may display seasonal shifts in their nocturnal habitat use. In the Coastal Plain of South Carolina, USA, the northern long‐eared bat (Myotis septentrionalis), southeastern myotis (Myotis austroriparius), tri‐colored bat (Perimyotis subflavus), and northern yellow bat (Lasiurus intermedius) are s

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45

Shute, Kyle E., Susan C. Loeb, and David S. Jachowski. "Seasonal Shifts in Nocturnal Habitat Use by Coastal Bat Species." Journal of Wildlife Management 85, no. 5 (2021): 964–78. https://doi.org/10.5281/zenodo.13489902.

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(Uploaded by Plazi for the Bat Literature Project) Sensitivity of bats to land use change depends on their foraging ecology, which varies among species based on ecomorphological traits. Additionally, because prey availability, vegetative clutter, and temperature change throughout the year, some species may display seasonal shifts in their nocturnal habitat use. In the Coastal Plain of South Carolina, USA, the northern long‐eared bat (Myotis septentrionalis), southeastern myotis (Myotis austroriparius), tri‐colored bat (Perimyotis subflavus), and northern yellow bat (Lasiurus intermedius) are s

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46

Bertness, Mark D. "Interspecific Interactions among High Marsh Perennials in a New England Salt Marsh." Ecology 72, no. 1 (1991): 125–37. http://dx.doi.org/10.2307/1938908.

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47

Lawrence, D. S. L., J. R. L. Allen, and G. M. Havelock. "Salt Marsh Morphodynamics: an Investigation of Tidal Flows and Marsh Channel Equilibrium." Journal of Coastal Research 201 (January 2004): 301–16. http://dx.doi.org/10.2112/1551-5036(2004)20[301:smmaio]2.0.co;2.

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48

Valiela, Ivan, and Carol S. Rietsma. "Disturbance of salt marsh vegetation by wrack mats in Great Sippewissett Marsh." Oecologia 102, no. 1 (1995): 106–12. http://dx.doi.org/10.1007/bf00333317.

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49

Eiser, William C., and Björn Kjerfve. "Marsh topography and hypsometric characteristics of a South Carolina salt marsh basin." Estuarine, Coastal and Shelf Science 23, no. 5 (1986): 595–605. http://dx.doi.org/10.1016/0272-7714(86)90101-0.

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50

Reents, Svenja, Peter Mueller, Hao Tang, Kai Jensen, and Stefanie Nolte. "Plant genotype determines biomass response to flooding frequency in tidal wetlands." Biogeosciences 18, no. 2 (2021): 403–11. http://dx.doi.org/10.5194/bg-18-403-2021.

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Abstract. The persistence of tidal wetland ecosystems like salt marshes is threatened by human interventions and climate change. In particular, the threat of accelerated sea level rise (SLR) has increasingly gained the attention of the scientific community recently. However, studies investigating the effect of SLR on plants and vertical marsh accretion are usually restricted to the species or community level and do not consider phenotypic plasticity or genetic diversity. To investigate the response of genotypes within the same salt-marsh species to SLR, we used two known genotypes of Elymus at

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