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  • 1
    ISSN: 1573-5052
    Keywords: Festuca rubra ; Grazing pattern ; Herbivore selectivity ; Micropattern ; Salt marsh ; Sheep grazing
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Micropatterns induced by sheep grazing, were studied in three consecutive years in a Festuca rubra-dominated salt marsh in a grazing trial with five different stocking rates (0, 1.5, 3, 4.5 and 10 sheep ha-1). The micropatterns were formed by a mosaic of short and tall F. rubra stands on a scale of square decimeters. Permanent transects of 2 m × 10 m were used to study the stability of these patterns, and to analyze interactions between the vegetation, the marsh elevation and the sheep. Micropatterns occurred only in the lightly to moderately grazed paddocks (1.5–4.5 sheep ha-1) with the highest spatial diversity in the 3 sheep ha-1 transect. When grazing was excluded, micropatterns did not develop; nor did they develop in the traditionally and most intensively grazed paddock (10 sheep ha-1). Detailed observations in one year showed that crude-protein content did not differ between green leaves from the short and tall stands, whereas in vitro digestibility was slightly higher in the short stands. In the same year, tiller density and length of full-grown leaves increased substantially in both stands from May to September. At the same time, sheep preference shifted from tall to short stands, which suggests an interplay between intake rate and digestibility in the sheep selectivity. Seven years after establishment of the grazing trial, the 10 sheep ha-1 transect still showed a smooth relief typical of the starting point of the other transects. These transects developed a more hummocky topography, with the highest spatial diversity occurring on the 1.5 sheep ha-1 transect. Marsh elevations were on average up to 3 cm lower in the short than in the tall stands, which indicates that the somewhat lower-elevated patches were grazed more intensively than the higher-elevated patches. In most cases, micropatterns changed from one year to the other, probably due to weather fluctuations. The incidence of tall stands was influenced by the rainfall balance. If the incidences of both the short and the tall stands were around 50%, however, the micropatterns showed a clear correlation with the marsh elevation. The rainfall balance seemed therefore a decisive factor for a possible correspondence between micropatterns in two consecutive years. Elevation differences were so subtle that greater than average sedimentation during a winter season could change the elevation pattern. Hence both rainfall balance and winter sedimentation counteracted the stability of the micropatterns. During our three-year study period, micropatterns were only stable in one out of six possible paired comparisons. This low micropattern stability contrasts with other studies in inland environments, which shows that in more dynamic environments, abiotic processes are likely to overrule summer grazing in determining vegetation patterns.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2023-03-10
    Keywords: Ameland; Caribbean Sea; Coon_Island; Dieksanderkoog; Dipper_Harbour; Dongtan; Event label; Isla_Cristobal; Isla_Popa; Isla_Solarte; Laws_Point; MULT; Multiple investigations; Noord-Friesland_Buitendijks; Patuxent_River; Rhode_River; Rimouski; Rush_Ranch; Site; Sonke-Nissen-Koog; South Atlantic Ocean; Spiekeroog; Tea bag index, decomposition rate; Tea bag index, stabilisation factor; TIDE_project; Treatment; Twin_Cays; Venice_Lagoon; Venice, Italy; Wachapreague; Zone
    Type: Dataset
    Format: text/tab-separated-values, 1928 data points
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  • 3
    Publication Date: 2023-03-10
    Keywords: Alfacs; Ameland; Area/locality; Caribbean Sea; China_Camp; Coon_Island; Dieksanderkoog; Dipper_Harbour; Dongtan; Ecosystem; Event label; Garxal; Isla_Cristobal; Isla_Popa; Isla_Solarte; LATITUDE; Laws_Point; Long_Marsh; LONGITUDE; Mar_Chiquita; Mechelinskie_Laki; MULT; Multiple investigations; Noord-Friesland_Buitendijks; Patuxent_River; Rhode_River; Rimouski; Rush_Ranch; Salinity, code; Schiermonnikoog; Soil composition; Sonke-Nissen-Koog; South Atlantic Ocean; Spiekeroog; Tea bag index, decomposition rate; Tea bag index, stabilisation factor; Temperature, soil; TIDE_project; Tide, amplitude; Twin_Cays; Venice_Lagoon; Venice, Italy; Vilacoto; Wachapreague; Zone
    Type: Dataset
    Format: text/tab-separated-values, 459 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Mueller, Peter; Schile-Beers, Lisa M; Mozdzer, Thomas J; Chmura, Gail L; Dinter, Thomas; Kuzyakov, Yakov; de Groot, Alma V; Esselink, Peter; Smit, Christian; D'Alpaos, Andrea; Ibáñez, Carles; Lazarus, Magdalena; Neumeier, Urs; Johnson, Beverly J; Baldwin, Andrew H; Yarwood, Stephanie A; Montemayor, Diana; Yang, Zaichao; Wu, Jihua; Jensen, Kai; Nolte, Stefanie (2018): Global-change effects on early-stage decomposition processes in tidal wetlands – implications from a global survey using standardized litter. Biogeosciences, 15(10), 3189-3202, https://doi.org/10.5194/bg-15-3189-2018
    Publication Date: 2023-01-13
    Description: Tidal wetlands, such as tidal marshes and mangroves, are hotspots for carbon sequestration. The preservation of organic matter (OM) is a critical process by which tidal wetlands exert influence over the global carbon cycle and at the same time gain elevation to keep pace with sea-level rise (SLR). The present study provides the first global-scale field-based experimental evidence of temperature and relative sea level effects on the decomposition rate and stabilization of OM in tidal wetlands. The study was conducted in 26 marsh and mangrove sites across four continents, utilizing commercially available standardized OM. While effects on decomposition rate per se were minor, we show unanticipated and combined negative effects of temperature and relative sea level on OM stabilization. Across study sites, OM stabilization was 29 % lower in low, more frequently flooded vs. high, less frequently flooded zones. OM stabilization declined by ~ 90 % over the studied temperature gradient from 10.9 to 28.5 °C, corresponding to a decline of ~ 5 % over a 1 °C temperature increase. Additionally, data from the long-term ecological research site in Massachusetts, US show a pronounced reduction in OM stabilization by 〉 70 % in response to simulated coastal eutrophication, confirming the high sensitivity of OM stabilization to global change. We therefore provide evidence that rising temperature, accelerated SLR, and coastal eutrophication may decrease the future capacity of tidal wetlands to sequester carbon by affecting the initial transformations of recent OM inputs to soil organic matter.
    Type: Dataset
    Format: application/zip, 2 datasets
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