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Weaver index

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FIGURE 5—Diversity variations measured by the Shannon-Weaver Index (H) and equitability. Sequence- and small-scale cycle boundaries as in Figure 2
Published: 01 August 2001
FIGURE 5 —Diversity variations measured by the Shannon-Weaver Index (H) and equitability. Sequence- and small-scale cycle boundaries as in Figure 2
Journal Article
Published: 01 January 2012
Journal of Foraminiferal Research (2012) 42 (1): 39–55.
... were identified in 31 samples collected during an oceanographic cruise (“Bocche 2003” – P.I.C Interreg III Project) that provided new geomorphologic and sedimentologic data on the western continental shelf of the strait. Biotic parameters (species diversity, density, Fisher α index, Shannon-Weaver...
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Planktic foraminiferal percentage, planktic foraminiferal fragmentation index, species diversity (Fisher Alpha Index, α; Shannon-Weaver Index, H), and eveness (J) plotted against depth.
Published: 01 October 2006
F igure 5. Planktic foraminiferal percentage, planktic foraminiferal fragmentation index, species diversity (Fisher Alpha Index, α; Shannon-Weaver Index, H), and eveness (J) plotted against depth.
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Published: 01 January 2003
TABLE 2. Average of the diversity parameters, according to the TWINSPAN classification. H = Shannon–Weaver index, R = Richness (number of taxa), Eq = Equitability. See materials and methods for details.
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Box plot of Shannon-Weaver diversity index colored according to detrital zircon population similarities (Fig. 6). Peak and low heavy mineral grades of newly dated samples (highlighted in bold) from Table 1. Gobi background sample AD550079 excluded from the analysis. Amb = Ambrosia, Ata = Atacama, HM = heavy mineral, Trip = Tripitaka.
Published: 01 March 2022
Fig. 7. Box plot of Shannon-Weaver diversity index colored according to detrital zircon population similarities ( Fig. 6 ). Peak and low heavy mineral grades of newly dated samples (highlighted in bold) from Table 1 . Gobi background sample AD550079 excluded from the analysis. Amb = Ambrosia
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FIGURE 9—Correlation between palynocycles and TLI cycles, and comparison with diversity trends represented by the Shannon-Weaver index (Rull, in press). Diversity in bits/indiv; arrows indicate diversity minima. Only some indicative samples are labelled (see Fig. 2)
Published: 01 February 2000
FIGURE 9 —Correlation between palynocycles and TLI cycles, and comparison with diversity trends represented by the Shannon-Weaver index (Rull, in press). Diversity in bits/indiv; arrows indicate diversity minima. Only some indicative samples are labelled (see Fig. 2 )
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Published: 01 November 2012
Table 1 Shannon–Weaver diversity index ( H ) and Shannon evenness ( E ) of water depth for the distribution of facies classes “reefal frameworks” and “sediments” for the six focus areas. Low values of H mean that that one of the two classes occurs over a limited range of water depths; low
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Published: 01 July 2011
T able 3. Taxonomic unit counts, probable error, Shannon-Weaver diversity index, tests per cc, relative abundance (% A) and Standard error (2σ) for each sample analyzed from Set One (2007) and Set Two (2008).
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Published: 01 January 2004
Table 1 Shannon-Weaver diversity index ( H ) and Shannon evenness ( E ) of water depth by sedimentologic facies (A) and habitat group (B). Low values of H mean that that class occurs over a limited range of water depths; low values of E suggest that classes are not distributed by water depths
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FIGURE 4—Benthic foraminiferal calcareous-agglutinated and infaunal-epifaunal ratios, heterogeneity and diversity indices, and δ13C (in bulk sediment) and %CaCO3 values across the upper Paleocene and lower Eocene at Zumaia. H (S) = Shannon Weaver index of diversity; BEE = benthic foraminiferal extinction event; CIE = carbon isotope excursion; PDB = Pee Dee Belemnite standard
Published: 01 May 2009
FIGURE 4 —Benthic foraminiferal calcareous-agglutinated and infaunal-epifaunal ratios, heterogeneity and diversity indices, and δ 13 C (in bulk sediment) and %CaCO 3 values across the upper Paleocene and lower Eocene at Zumaia. H (S) = Shannon Weaver index of diversity; BEE = benthic foraminiferal
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Published: 01 July 2007
T able 1. Quantitative data from the four treatments. N = absolute abundance (relative abundance in parenthesis); G = generic richness; H ′ = Shannon-Weaver index; J ′ = equitability (based on H ′ ); D = McIntosh’s diversity index; E = equitability (based on D ). Underlined χ 2 values
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Plot of ostracod assemblage characteristics with depth, including total number of species’ upper and lower depth limits, diversity (measured by number of species recorded, compound diversity – number of species within recorded depth range, and Shannon–Weaver index) and total number of specimens recorded in sample. AAIW, Antarctic Intermediate Water; CDW, Circumpolar Deep Water; SAUW, Subantarctic Upper Water. Dashed lines indicate watermass boundary.
Published: 01 May 2004
Fig. 5. Plot of ostracod assemblage characteristics with depth, including total number of species’ upper and lower depth limits, diversity (measured by number of species recorded, compound diversity – number of species within recorded depth range, and Shannon–Weaver index) and total number
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1986
AAPG Bulletin (1986) 70 (1): 26–33.
... crystallinity index (CI) decreases with increasing R 0 : log (CI) = 1.01 - 0.07 (R 0 ). Plots of bitumen ratio (bitumen/total organic carbon) vs. vitrinite reflectance, Weaver’s illite sharpness ratio, and Kubler’s crystallinity index all reveal hydrocarbon generation-preservation curves that define submature...
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Journal Article
Published: 03 October 2017
Bulletin de la Société Géologique de France (2017) 188 (3): 13.
..., San Pietro Mussolino, Vestenanova, and the Bolca area (Vicenza; Verona – NE Italy). The high value of the Shannon-Weaver biodiversity index calculated for these buildups confirms the hypothesis of the existence during the Early Eocene of a large lagoon characterized by shallow water and patch reefs...
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Journal Article
Published: 01 April 1955
American Mineralogist (1955) 40 (3-4): 356–357.
... is that they are allophane or some other clay mineral with a very low index. (2) The “turbid” objects appear brownish in transmitted light and milky in reflected light, exactly like the liquid-filled vacuoles in granitic quartz or in chalcedonic quartz (Folk and Weaver, 1952). This is probably due to some complex dispersion...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1985
AAPG Bulletin (1985) 69 (2): 260.
... are influenced by the degree of thermal maturity. Weaver’s sharpness ratio for illite and Kubler’s crystallinity index are both significantly related to mean vitrinite reflectance. The log of the sharpness ratio increases while the log of the crystallinity index decreases with increasing mean vitrinite...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1973
AAPG Bulletin (1973) 57 (2): 429.
... sequence is based largely on assemblages from the Temblor Formation; the basal shale member contains Bruclarkia columbiana, an index species for the “Lincoln Stage” of Weaver. The overlying “Phacoides reef,” formerly assigned to the “Vaqueros Stage,” represents a previously unrecognized post-“Lincoln,” pre...
Journal Article
Published: 17 January 2003
Canadian Journal of Earth Sciences (2003) 40 (1): 13–25.
...., a sample taken 1 km south of the exposure of the Cathedral Escarpment on Fossil Ridge is likely to be a true distance of less than a few hundred metres normal to the paleo-cliff face). At higher grade, as the 10 Å peak becomes sharper, the error in measurement of the Weaver index becomes greater...
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Published: 01 December 2006
coefficient; p , two-tailed probability that r = 0;. H, Shannon Weaver Diversity Index; J, Shannon Weaver Evenness Index; PIE, Hurlbert's Equitability Index; Div30, standardized species (SP) and genus (GEN) diversity for n = 30 specimens; Div100, standardized species (SP) and genus (GEN) diversity for n
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—Relationship between illite sharpness ratio (Weaver, 1960) and illite crystallinity index (Kubler, 1968) for all 54 samples of Stanley, Jackfork, and Atoka shale analyzed.
Published: 01 January 1986
Figure. 7. —Relationship between illite sharpness ratio ( Weaver, 1960 ) and illite crystallinity index ( Kubler, 1968 ) for all 54 samples of Stanley, Jackfork, and Atoka shale analyzed.