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1,133 results for “wetlands”
Table 3 in Temperate grassy wetlands of South Africa: Description, classification and explanatory environmental factors
<p><b>Table 3</b> Indicator species for the broad clusters of temperate grassy wetlands, indicating the Indicator Values and p-values. Only species where the p-value is smaller than 0.05 and the Indicator Value larger than 20 are listed. Alien species are marked with an asterisk.</p><table><tbody><tr><th>Number</th><th>No. of plots</th><th>Dominants</th><th>Where</th><th>Indicator species</th><th>Indicator value</th><th>p - Value</th></tr></tbody><tbody><tr><th>1</th><td>242</td><td>Eleocharis dregeana, Leersia dregeana</td><td>Throughout the country</td><td>Eleocharis dregeana</td><td>47.7</td><td>0.001</td></tr><tr><th>2</th><td>53</td><td><i>Carex acutiformis</i></td><td>Highveld, Kwazulu-Natal</td><td>Carex acutiformis</td><td>75</td><td>0.001</td></tr><tr><th>3</th><td>36</td><td>Aristida junciformis, Helichrysum aureonitens</td><td>Highveld, Kwazulu-Natal</td><td>Fuirena pubescens</td><td>40</td><td>0.001</td></tr><tr><td>Aristida junciformis</td><td>32.7</td><td>0.001</td></tr><tr><td></td><td>Helichrysum aureonitens</td><td>24.3</td><td>0.001</td></tr><tr><th>4</th><td>162</td><td>Cyperus denudatus, Schoenoplectus brachyceras,</td><td>Highveld</td><td><i>Eragrostis curvula</i></td><td>46.7</td><td>0.001</td></tr><tr><td><i>Juncus effusus</i></td><td><i>Hyparrhenia hirta</i></td><td>50.3</td><td>0.001</td></tr><tr><td>Schoenoplectus brachyceras</td><td>88.8</td><td>0.001</td></tr><tr><td>Juncus effusus</td><td>63.8</td><td>0.001</td></tr><tr><td>Cyperus denudatus</td><td>62.3</td><td>0.001</td></tr><tr><th>5</th><td>31</td><td>Eragrostis planiculmis</td><td>Highveld</td><td>Eragrostis planiculmis</td><td>56.7</td><td>0.001</td></tr><tr><th>6</th><td>63</td><td>Arundinella nepalensis, Leucosidea sericea</td><td>Highveld, particularly Drakensberg</td><td>Arundinella nepalensis</td><td>33.7</td><td>0.001</td></tr><tr><td>Leucosidea sericea</td><td>79.7</td><td>0.001</td></tr><tr><td>Searsia dentata</td><td>52.8</td><td>0.001</td></tr><tr><td>Cliffortia nitidula</td><td>36.9</td><td>0.001</td></tr><tr><td>Euclea crispa</td><td>29.2</td><td>0.001</td></tr><tr><th>7</th><td>114</td><td><i>Hemarthria altissima</i>, Cyperus marginatus,</td><td>Mostly Highveld</td><td>Hemarthria altissima</td><td>37.6</td><td>0.001</td></tr><tr><td><i>Paspalum dilatatum</i></td><td>Cyperus marginatus</td><td>63.8</td><td>0.001</td></tr><tr><td><i>Cynodon dactylon</i></td><td>30.6</td><td>0.001</td></tr><tr><td><i>Plantago lanceolata</i></td><td>29.7</td><td>0.001</td></tr><tr><td>Paspalum dilatatum</td><td>26.4</td><td>0.001</td></tr><tr><td><i>Trifolium repens</i></td><td>26.2</td><td>0.001</td></tr><tr><th>8</th><td>65</td><td><i>Themeda triandra</i></td><td>Highveld</td><td>Themeda triandra</td><td>52.4</td><td>0.001</td></tr><tr><th>9</th><td>77</td><td>Cyperus fastigiatus</td><td>Throughout the country</td><td>Cyperus fastigiatus</td><td>62.8</td><td>0.001</td></tr><tr><th>10</th><td>136</td><td><i>Imperata cylindrica</i></td><td>Throughout the country</td><td>Imperata cylindrica</td><td>41.1</td><td>0.001</td></tr><tr><td>Senecio achilleifolius</td><td>54.2</td><td>0.001</td></tr><tr><td>Pulicaria scabra</td><td>47.3</td><td>0.001</td></tr><tr><td>Andropogon eucomus</td><td>42.2</td><td>0.001</td></tr><tr><td><i>Fimbristylis ferruginea</i></td><td>41.6</td><td>0.001</td></tr><tr><td><i>Paspalum urvillei</i></td><td>34.9</td><td>0.001</td></tr><tr><td>Pycreus betschuanus</td><td>26.8</td><td>0.001</td></tr><tr><td>Chamaecrista stricta</td><td>26.4</td><td>0.001</td></tr><tr><td>Kyllinga alba</td><td>31.8</td><td>0.001</td></tr><tr><td>Miscanthus junceus</td><td>28.9</td><td>0.001</td></tr><tr><td>Phymaspermum athanasoides</td><td>26.6</td><td>0.001</td></tr><tr><td>Wahlenbergia undulata</td><td>26.4</td><td>0.001</td></tr><tr><th>11</th><td>138</td><td><i>Eragrostis plana</i></td><td>Throughout the country</td><td>Eragrostis plana</td><td>29.8</td><td>0.001</td></tr><tr><th>12</th><td>107</td><td>Typha capensis</td><td>Throughout the country</td><td>Typha capensis</td><td>51.9</td><td>0.001</td></tr><tr><th>13</th><td>90</td><td><i>Phragmites australis</i></td><td>Throughout the country</td><td>Phragmites australis</td><td>39.5</td><td>0.001</td></tr></tbody></table>
FIG. 2 in Factors Influencing Anuran Wetland Occupancy in an Agricultural Landscape
FIG. 2.—Amphibian occupancy by species and life stage in Iowa during 2015 (light gray) and 2016 (dark gray). A. americanus ¼ Anaxŋrus americanus (American Toads); Hŋla spp. ¼ Hŋla Ʋersicolor and Hŋla chrŋsocelis (Gray Treefrogs and Cope̕s Gray Treefrogs, respectively); L. pipiens ¼ Lithobates pipiens (Northern Leopard Frogs); and P. maculata ¼ Pseudacris maculata (Boreal Chorus Frogs). Error bars represent 95% confidence intervals. Estimates are from the model with the most support (see Table 3).
Remote sensing spectral vegetation indices for 2011 NWCA wetland sites
Open the record for dataset details and reuse information.
Using Gene Expression to Assess the Status of Fish from Anthropogenically Influenced Estuarine Wetlands
GEO Series GSE28695. Gillichthys mirabilis. 60 samples. Type: Expression profiling by array.
The grain size endmembers of Tengchongbeihai wetland sediments over the past 46 ka
<p> Here, we present a grain size end-member analysis for Tengchongbeihai wetland sediments from southwestern China to investigate the paleo-hydroclimate changes since the late MIS3. The overall low fine silt (EM2) content before ~16.5 cal ka BP resulted from weak catchment erosion indicating weak ISM during cold glacial while the increasing trend thereafter indicates the ISM strengthened during the last deglaciation and Holocene. Such an orbital ISM evolution resembles to the insolation gradient between 25°N and 25°S during the boreal summer periods, which implies the transequatorial insolation difference could be an alternative explanation for the orbital scale low latitude hydroclimate changes. The striking peaks of coarse component (EM3) around ~12, 16, 24, 29, 32 and 39 cal ka BP were related to significant water level descending indicating the millennial ISM collapse corresponding to the YD and Heinrich events. However, the absence of sawtooth feature as the NGRIP δ18O and the well correspondence to the Indian Ocean sea surface temperatures (SSTs) of the ISM collapses evidence the complementary role of low latitude climate for the North Atlantic climate on the millennial scale hydroclimate variabilities.</p>
FIGURE 30 in Shallow-water Demospongiae (Porifera) from Sodwana Bay, iSimangaliso Wetland Park, South Africa
FIGURE 30. Psammocinia alba sp. nov. A. In situ; B & C. Skeletal architecture (B, x5; C, x10)
ESM Chapter 2 - Drivers of vegetation development, biomass production and the initiation of peat formation in a newly constructed wetland
<p>Electronic supplementary material to Chapter 2 "Drivers of vegetation development, biomass production and the initiation of peat formation in a newly constructed wetland" of PhD thesis from Ciska Overbeek, "Peat formation on a former landfill - Production and decomposition of aquatic pioneer vegetation". </p>
Linking functional diversity, trait composition, invasion, and environmental drivers in boreal wetland plant assemblages
<p>These datasets contain information for the the species occurrence, trait, and wetland site characteristics used in this manuscript.</p>
The refined annual 10-m wetland maps of Dongting Lake wetland during 2015~2021
<p>The wetland maps include 8 wetland classes and 5 non-wetland classes, with a spatial resolution of 10m.</p>
Data from: The Restoration of Wetlands Dominated by Habitat Modifiers
<p>Unpublished data to chapters 3 till 7 from:</p> <p>Temmink, R.J.M. 2020. The Restoration of Wetlands Dominated by Habitat Modifiers. PhD thesis, Radboud Universiteit, Nijmegen, the Netherlands.</p> <p> </p>
A water-table-dependent net warming effect of global wetlands from potent greenhouse gases
<p>A database of the annual greenhouse gase fluxes across global wetlands. In total, the database comprised 2,455 observations of annual net ecosystem exchange of CO<sub>2 </sub>(NEE; net gaseous CO<sub>2</sub> exchange between land and atmosphere), 2,342 observations of annual CH<sub>4 </sub>fluxes and 850 observations of annual N<sub>2</sub>O fluxes.</p>
Success of coastal wetlands restoration is driven by sediment availability
<p>Shorelines and their ecosystems are endangered by sea-level rise. Nature-based coastal protection is becoming a global strategy to enhance coastal resilience through the cost-effective creation, restoration and sustainable use of coastal wetlands. However, the resilience to sea-level rise of coastal wetlands created under Nature-based solution has been assessed largely on a regional scale. Here we assess, using a meta-analysis, the difference in accretion, elevation, and sediment deposition rates between natural and restored coastal wetlands across the world. Our results show that restored coastal wetlands can trap more sediment and that the effectiveness of these restoration projects is primarily driven by sediment availability, not by wetland elevation, tidal range, local rates of sea-level rise, and significant wave height. Our results suggest that Nature-based Solutions can mitigate coastal wetland vulnerability to sea-level rise, but are effective only in coastal locations where abundant sediment supply is available.</p>
Movement and competition ecology of African lions in semi-arid and wetland ecosystems
<p>GPS dataset of lion tracking data.</p>
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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