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1,515 results for “marshes”

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Fig. 3 in Habitat Preference And Prey Selection Of Marsh Harrier (Circus Aeruginosus) In Overwintering Area Of Southeast China

Fig. 3. Abundances of passerines (), pheasant () and marsh harrier (+) of the four years in the four habitats in Shahu Nature Reserve, China, with line transects 2000 m × 200 m (A, autumn; W,

opencc-by-4.0Dec 2010View details →
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Fig. 2 in Habitat Preference And Prey Selection Of Marsh Harrier (Circus Aeruginosus) In Overwintering Area Of Southeast China

Fig. 2. Wintering marsh harrier's abundance in different habitats in Shahu Nature Reserve, China in autumn and winter of 2001, 2003, 2004 and 2006

opencc-by-4.0Dec 2010View details →
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Fig. 1 in Habitat Preference And Prey Selection Of Marsh Harrier (Circus Aeruginosus) In Overwintering Area Of Southeast China

Fig. 1. Shahu Nature Reserve (SNR, autumn and winter). The up left shows the location of SNR; HB, Hubei Province; BWH, Beiwu Lake; NWH, Nanwu Lake; DC, Daocao Lake; DJ, Dongji River; YR, Yangtze River

opencc-by-4.0Dec 2010View details →
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Fig. 4 in Physiological Responses Of Rare Coastal Salt Marsh Plant Triglochin Maritima L. To Soil Chemical Heterogeneity

Fig. 4. Time-course of Peformance Index (A) and chlorophyll concentration (B) in leaves of T. maritima plants grown in different substrates.

opencc-by-4.0Dec 2017View details →
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Fig. 7 in Physiological Responses Of Rare Coastal Salt Marsh Plant Triglochin Maritima L. To Soil Chemical Heterogeneity

Fig. 7. Correlation between summary Na + K concentration and extract EC in leaves (A) and roots (B) of T. maritima plants.

opencc-by-4.0Dec 2017View details →
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Fig. 1 in Physiological Responses Of Rare Coastal Salt Marsh Plant Triglochin Maritima L. To Soil Chemical Heterogeneity

Fig. 1. Effect of treatment type on soil electrical conductivity (A) and pH (B) after 8 weeks of cultivation.

opencc-by-4.0Dec 2017View details →
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Fig. 5 in Physiological Responses Of Rare Coastal Salt Marsh Plant Triglochin Maritima L. To Soil Chemical Heterogeneity

Fig. 5. Time-course of Na+ (A), K+ (B) and Ca2+ concentration in leaves of T. maritima plants grown in different substrates.

opencc-by-4.0Dec 2017View details →
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Fig. 6 in Physiological Responses Of Rare Coastal Salt Marsh Plant Triglochin Maritima L. To Soil Chemical Heterogeneity

Fig. 6. Effect of treatment type on Na+ (A) and K+ (B) concentration in roots of T. maritima plants after 8 weeks of cultivation.

opencc-by-4.0Dec 2017View details →
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Fig. 4 in Habitat requirements and occurrence of Crematogaster pilosa (Hymenoptera: Formicidae) ants within intertidal salt marshes

Fig. 4. Logistic regression model (P = 0.03) of the probability of Crematogaster pilosa as a function of brown leaf density between 0.61 and 1.20 m. Stars indicate plots containing ants, and open symbols indicate plots not containing ants. Vertical dashed line represents a 50% probability of ants and occurs at a brown leaf density of 2.5 m−1, which equals 1.5 brown leaves between 0.61 and 1.20 m above the marsh surface.

opencc-by-4.0Mar 2016View details →
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Fig. 2 in Habitat requirements and occurrence of Crematogaster pilosa (Hymenoptera: Formicidae) ants within intertidal salt marshes

Fig. 2. Mean vegetation heights for marsh plots containing ants (n = 8) and plots not containing ants classified by their dominant vegetation type: short (n = 7) and tall (n = 2). All plots were from Dean Creek and Odum's Marsh. Mean heights are the weighted average of all vegetation counts within plots. Letters above whiskers signify significant difference using Tukey's HSD with P <0.05.

opencc-by-4.0Mar 2016View details →
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Fig. 1 in Habitat requirements and occurrence of Crematogaster pilosa (Hymenoptera: Formicidae) ants within intertidal salt marshes

Fig. 1. Southern tip of Sapelo Island, Georgia (USA). Location of Crematogaster pilosa observations and vegetation assessments in Odum's Marsh (A) and Dean Creek (C). Presence/absence of ants along Lighthouse Creek (B) from canoe and baited trap survey. Sites containing C. pilosa were labeled "ants", those not containing ants were labeled by their vegetation (i.e., short or tall) based on maximum vegetation height.

opencc-by-4.0Mar 2016View details →
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Fig. 3 in Habitat requirements and occurrence of Crematogaster pilosa (Hymenoptera: Formicidae) ants within intertidal salt marshes

Fig. 3. Height-specific vegetation density for marsh plots with and without ants in Dean Creek and Odum's Marsh. Vegetation density is the number of vegetation features (i.e., stems and leaves) per vertical meter above an average point on the marsh surface. Integrating vertically produces the average number of vegetation features above a single point. All plots containing Crematogaster pilosa were grouped (ants); plots not containing ants were classified by the maximum vegetation height of Spartina alterniflora (i.e., tall or short). Vegetation density distributions are the means for tall (n = 2), ants (n = 8), and short (n = 7) plots.

opencc-by-4.0Mar 2016View details →
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Fig. 1. A in A comparison of two insect collection techniques in oiled and non-oiled salt marshes in Louisiana

Fig. 1. A species accumulation curve for both the sweep net (black) and the vacuum (gray) collection techniques. Dotted lines indicate the 95% confidence interval around each curve. Neither curve reached an asymptote.

opencc-by-4.0Jun 2017View details →
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Figure 2. a in Evidence of Ehrlichia chaffeensis in Argentina through molecular detection in marsh deer (Blastocerus dichotomus)

Figure 2. a_Summary of the E. chaffeensis molecular amplification of the 16SrRNA and the VLPT genes in marsh deer and tick samples at different time points. b_ Alignment of a fragment of the 16SrRNA nucleotide sequences from reference Anaplasma and Ehrlichia strains and those amplified from deer (C2, C7, D11 and C12) and a tick (tick1_C7) in the present study. The red line marks the hypervariable V1 region.

opencc-by-4.0Apr 2019View details →
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Fig. 1 in Evidence of Ehrlichia chaffeensis in Argentina through molecular detection in marsh deer (Blastocerus dichotomus)

Fig. 1. Map of the two marsh deer populations (Paraná River Delta and Ibera Wetlands) located along the alluvial plain of the Paraná River (Argentina).

opencc-by-4.0Apr 2019View details →
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"Marsh" database: characterization of the state of the necton in two depolderized zones of the Gironde estuary

<p>In the Gironde estuary, two accidentally de-polderized marshes have been the subject of biological monitoring (necton) since 2008: the Marais de Mortagne-sur-Gironde and the northern part of &Icirc;le Nouvelle. The Mortagne-sur-Gironde marsh is located in the mesohalin sector of the Gironde estuary. With an area of 191 hectares, the marsh was dammed in 1966 and cultivated for more than 30 years. Its protective dike gave way during the December 1999 storm. Ile Nouvelle is located in the Oligaline Sector of the Gironde Estuary. The northern part of the island - an area of 141 hectares - has been depolderized&nbsp;during the passage of storm Xynthia in 2010, following the opening of a breach.<br> Biological monitoring (necton) was carried out in the Gironde estuary over the period 2008-2016 to test the hypothesis that the depoldisation of the estuarine shorelines makes it possible to recreate nursery and feeding areas for fish and fish. estuarine and coastal macrocrustaceans. This work was carried out by the National Institute for Research in Science and Technology for the Environment and Agriculture (Irstea), in partnership with the Conservatoire du Littoral, the Gironde Departmental Council and the Regional Council for Natural Areas ( CREN) of Poitou-Charentes.<br> The &quot;Marsh&quot; database includes all the surveys carried out throughout the study, between 2008 and 2016, and in particular samplings carried out within the necton.</p>

opencc-by-4.0Sep 2018View details →
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Fig. 7 in Testate Amoebae as Proxy for Water Level Changes in a Brackish Tidal Marsh

Fig. 7. Graphs of observed versus estimated Elevation and Normalized elevation, predicted by the transfer function based on Jack-knifed WA-PLS (component 2) for the complete dataset, after the removing of outliers and for the partial dataset.

opencc-by-4.0Dec 2012View details →
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Fig. 1. A in Testate Amoebae as Proxy for Water Level Changes in a Brackish Tidal Marsh

Fig. 1. A – map of the Scheldt estuary with location of Groot Buitenschoor; B – map of the brackish tidal marsh Groot Buitenschoor with indication of vegetation zones and the elevation transects that are sampled; C – photos of the two sampled transects. Photo 1 – from Salix to outer edge of Phragmites australis vegetation; Photo 2 – from Phragmites australis to outer edge of Scirpus maritimus.

opencc-by-4.0Dec 2012View details →
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Fig. 6 in Testate Amoebae as Proxy for Water Level Changes in a Brackish Tidal Marsh

Fig. 6. Results of the partial RDA for both intertidal (zone B) and supratidal (zone A) bio-zones. The values in the intersection of the circle are the common variation explained by the two variables.

opencc-by-4.0Dec 2012View details →
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Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011). in Feather Palm Foliage From The Messinian Of Italy (Capo Di Fiume, Palena And Pollenzo Near Alba) Within The Framework Of Northern Mediterranean Late Miocene Flora

Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011).

opencc-by-4.0Dec 2015View details →

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