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14 results for “wetland invertebrates”
UCSB SONGS Mitigation Monitoring: Wetland Performance Standard - Invertebrate Abundance and Richness
These data contain annual estimates of the density of wetland macroinvertebrates (all species combined) and species richness (as a species density) in six main channel and six tidal creek locations at four coastal wetlands as part of the SONGS San Dieguito Wetland Restoration monitoring program to track long-term patterns in species abundance and diversity. This study began in 2012 in the San Dieguito Wetland and Tijuana Estuary in San Diego County, CA, Carpinteria Salt Marsh in Santa Barbara County, CA, and Mugu Lagoon in Ventura County, CA. Beginning in 2024, Tijuana Estuary was replaced with Los Penasquitos Lagoon in San Diego County, CA.
UCSB SONGS Mitigation Monitoring: Wetland Survey - Invertebrate Abundance
These data describe the abundance of invertebrate species sampled in quadrats and sediment cores as part of the SONGS San Dieguito Wetland Restoration monitoring program to track long-term patterns in species abundance and diversity and assess compliance of the restoration project with conditions in the SONGS Coastal Development permit. This study began in 2012 in the San Dieguito Lagoon and Tijuana Estuary in San Diego County, CA, Carpinteria Salt Marsh in Santa Barbara County, CA, and Mugu Lagoon in Ventura County, CA. The abundance of invertebrates in quadrats and sediment cores was recorded at six main channel and six tidal creek locations at each wetland. Beginning in 2024, Tijuana Estuary was replaced with Los Penasquitos Lagoon in San Diego County, CA.
Figure 3 in Temporal dynamics of invertebrate and aquatic plant communities at three intermittent ponds in livestock grazed Patagonian wetlands
Figure 3. Seasonal variation of total taxa richness (A), mean density (A), and relative contribution of biomass (B) of most abundant groups of aquatic invertebrates at three ponds in a Patagonian wetland (Mallín Crespo) during the study period (May 2008 to April 2009). Livestock stocking period is indicated by the black bar.
Data for "Invertebrate Activities in Wetland Sediments Influence Oxygen and Nutrient Dynamics at the Sediment-Water Interface"
<p>Code and data for a project looking at how bioturbation by two benthic invertebrate taxa influence oxygen and nutrient dynamics a coastal freshwater wetland along Lake Erie, located in Ohio, USA.</p> <p>Article is titled "Invertebrate Activities in Wetland Sediments Influence Oxygen and Nutrient Dynamics at the Sediment-Water Interface" and is published in Wetlands.</p>
Data from: Effects of salinization on tropical freshwater wetland primary producers and aquatic invertebrates
Open the record for dataset details and reuse information.
Data from: Pollution-tolerant invertebrates enhance greenhouse gas flux in urban wetlands
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Figure 6. A in Temporal dynamics of invertebrate and aquatic plant communities at three intermittent ponds in livestock grazed Patagonian wetlands
Figure 6. A schematic cross-section of the study wetland (Mallín Crespo) contrasting the condition of the three studied ponds (P1, P2 and P3) during hydrological phases: isolation and connected periods. Distances between ponds, the weather station and sheep are not to scale. Volume (m3) is indicated below each pond. Environment variables are: water temperature (WT), precipitation (PP), pH, specific conductivity (C), dissolved oxygen (DO), total suspended solids (TSS), total nitrogen (TN), and total phosphorus (TP). Invertebrate attributes are: taxa richness (R) density (D), biomass (B) and dominant functional feeding groups (FFG). Dominant taxa in terms of density and frequency are listed over each pond. Bold letters are used for taxa that are also dominants in biomass. For both periods first and second dominant FFG are represented. P, predators; CG, collector–gatherers; and CF, collector–filterers.
Figure 4 in Temporal dynamics of invertebrate and aquatic plant communities at three intermittent ponds in livestock grazed Patagonian wetlands
Figure 4. Seasonal patterns of functional feeding groups (FFG), (A) by density (103 individuals m−3) and (B) by biomass [g DM m−3] at three ponds (May 2008 to April 2009) of Mallín Crespo wetland (Argentina). Sh, shredders; Sc, scrapers; P, predators; CG, collector–gatherers; CF, collector–filterers; P–H, piercers herbivores.
Figure 2 in Temporal dynamics of invertebrate and aquatic plant communities at three intermittent ponds in livestock grazed Patagonian wetlands
Figure 2. Seasonal variation of particulate organic matter (POM, dashed lines) and aquatic plant coverage (solid line) at three ponds on a Patagonian steppe wetland (Argentina) during the study period (May 2008 to April 2009). Categories of aquatic plant coverage explained in methodology. Livestock stocking period is indicated in the figure (black bar).
Figure 1 in Temporal dynamics of invertebrate and aquatic plant communities at three intermittent ponds in livestock grazed Patagonian wetlands
Figure 1. (A) Location of the sampling sites (P1, P2 and P3) at Mallín Crespo (Chubut Province, Patagonia, Argentina) during connected (June–December) and hydrologically isolated (January–May) periods. The three ponds are in the same scale. (B) Daily rain (dashed line) and mean daily air temperature (solid line), from May 2008 to April 2009. (C–E) Physicochemical variables sampled monthly and once per pond. Dashed line (D), indicates unavailable data.
Figures 5-8 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figures 5-8 - Lophopodella capensis statoblasts and organic detritus, including charcoal at right, from the sieved sediment subsample from25–26 cm stratigraphic depth, dated to 220–230 yr BP (5). A well preserved statoblast observed at 41–42 cm, dated to 670–711 (6). Pleistocene-aged statoblast from 480–481 cm, dated to 15600–15700 (7). Same specimen as Fig. 6 showing the split layers of the polar spine and recurved hooks (8).
Figure 1 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figure 1 - Location of the study site in Africa (A) and within Kenya (B). The location of the coring site (black circle) within Enapuiyapui (C). The red line represents a fire break cutline.
Figure 4 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figure 4 - BACON version 2.2 R program language script age-depth model for the Enapuiyapui stratigraphy using MCMC random walks (greyscale shading) through the probable radiocarbon dates (1σ age probability distributions represented in blue) that were calibrated using the IntCal13 curve (Table 1; Blaauw and Christenson 2011; Reimer et al. 2013; R Development Core Team 2015). The final model used the weighted average of the random walk densities (red line) and 95% CI (dotted grey lines) and parameter settings are shown at the top right (red font). Ages reported as calibrated year BP (before present, 1950 CE). ITRAX optical core face photographs and magnetic susceptibility profile (grey line) at bottom left that shows the 484–0 cm section of the 537 cm core. Zones were defined using a regime shift index of the magnetic susceptibility values (Rodionov 2004). Lophopodella capensis presence data are represented by red '+' symbols on the magnetic susceptibility profile. Abbreviations are AHP: African Humid Period, H: Holocene, Ps: Pleistocene.
Figures 2-3 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figures 2-3 - An wide angle aerial oblique photograph of Enapuiyapui wetland from the northwest facing southeast (2). Coring the center of the Cyperaceae-Poaceae wetland, April 2014 (3).
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OpenNeuro
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