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Eponyms of Dale Russell. Available to Purchase

Published: 07 December 2020
Table B1. Eponyms of Dale Russell.
Journal Article

Gender in mineral names Available to Purchase

Christopher Emproto, Gabriela A. Farfan, Tyler L. Spano, Marko Bermanec, Mike S. Rumsey, Barbara L. Dutrow, Raquel Alonso-Perez, Jessica Riaño, Adam C. Simon
Published: 01 February 2025
American Mineralogist (2025) 110 (2): 181–188.
DOI: https://doi.org/10.2138/am-2024-9327
... database. The compiled information yields diverse insights into the intersection of science and culture and could also be used to project future trends. In this study, we used the name database to investigate gender diversity among mineral eponyms. More than half (ca. 54%) of all mineral species are named...
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Includes: Supplemental Content
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Occurrence of eponymous species of the two previously proposed biozonation ... Available to Purchase

Published: 01 November 2024
Table 4. Occurrence of eponymous species of the two previously proposed biozonation schemes for the Doushantuo Formation in South China. Abbreviations for biozones: A1 =  Tianzhushania spinosa zone of Liu et al. ( 2013 , 2014a ) and Xiao et al. ( 2014 ), corresponding to Member II
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Taxonomic ordination plots based on NMDS analysis of taxonomically updated occurrence data from 82 collections of Doushantuo acanthomorphs in South China (see Supplemental Materials for data). (1) NMDS scatter plots and convex hulls differentiated by depositional facies. (2) NMDS scatter plots and convex hulls differentiated by depositional facies and stratigraphic intervals. (3) Species loading diagram. Note that some species are not labeled because of the limited space; see Supplemental Materials for loading data. Red and green circled points represent eponymous species of the lower and upper biozones of the Doushantuo Formation (Liu et al., 2013, 2014b; Xiao et al., 2014), respectively. Blue filled points represent eponymous species of the biozones of Liu and Moczydłowska (2019). See Figure 42 for abbreviations.

Taxonomic ordination plots based on NMDS analysis of taxonomically updated ... Available to Purchase

Published: 01 November 2024
scatter plots and convex hulls differentiated by depositional facies and stratigraphic intervals. ( 3 ) Species loading diagram. Note that some species are not labeled because of the limited space; see Supplemental Materials for loading data. Red and green circled points represent eponymous species
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Visual comparison of the three FCM ‘centres’. This shows the percentages of each taxon in each centre. Only the nominate taxa from the three FCM centres are labelled. R. australoclavatidites dominates its eponymous centre, making up almost 40% of the flora. Its occurrence in the other centres rapidly decreases. P. equiexinus dominates its eponymous centre, making up 15% of the flora, and decreases sequentially in abundance through the transitional and R. australoclavatidites centres.

Visual comparison of the three FCM ‘centres’. This shows the percentages of... Available to Purchase

Published: 01 February 2013
Fig. 7. Visual comparison of the three FCM ‘centres’. This shows the percentages of each taxon in each centre. Only the nominate taxa from the three FCM centres are labelled. R. australoclavatidites dominates its eponymous centre, making up almost 40% of the flora. Its occurrence in the other
Journal Article

THE 29.07.2022 M L = 6.2 TSAGAN-SHIBETU EARTHQUAKE AND SPATIAL POSITION OF THE FOCAL AREA IN THE WESTERN MOUNTAIN FRAMING OF THE TUVA BASIN Available to Purchase

A.F. Emanov, A.A. Emanov, E.V. Shevkunova, E.A. Gladyshev
Published: 01 June 2025
Russ. Geol. Geophys. (2025) 66 (6): 769–776.
DOI: https://doi.org/10.2113/RGG20254796
...A.F. Emanov; A.A. Emanov; E.V. Shevkunova; E.A. Gladyshev The 29.07.2022 (UTC time 13:01:10.1) Tsagan-Shibetu earthquake with M L = 6.2, M W = 5.5 occurred in the eponymous mountain range in the eastern Altai Mountains (Gorny Altai), in proximity to the Tuva Basin (50.51º N, 90.69º E). The Tsagan...
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View PDF for article title, THE 29.07.2022 M L = 6.2 TSAGAN-SHIBETU EARTHQUAKE AND SPATIAL POSITION OF THE FOCAL AREA IN THE WESTERN MOUNTAIN FRAMING OF THE TUVA BASIN
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The small workings of the eponymous Wortupa mine, where few primary sulfides (aside from scattered pyrite) and no telluride mineralised zones remain. (a) Author JB surveys a former tailings pile. (b) Mine entrance surrounded by non-mineralised pebbles. Photos taken in November 2017.

The small workings of the eponymous Wortupa mine, where few primary sulfide... Open Access

Published: 24 August 2023
Figure 1. The small workings of the eponymous Wortupa mine, where few primary sulfides (aside from scattered pyrite) and no telluride mineralised zones remain. (a) Author JB surveys a former tailings pile. (b) Mine entrance surrounded by non-mineralised pebbles. Photos taken in November 2017.
Journal Article

Recommended nomenclature of epidote-group minerals Open Access

Thomas ARMBRUSTER, Paola BONAZZI, Masahide AKASAKA, Vladimir BERMANEC, Christian CHOPIN, Reto GIERÉ, Soraya HEUSS-ASSBICHLER, Axel LIEBSCHER, Silvio MENCHETTI, Yuanming PAN, Marco PASERO
Published: 01 September 2006
European Journal of Mineralogy (2006) 18 (5): 551–567.
DOI: https://doi.org/10.1127/0935-1221/2006/0018-0551
... be maintained. (2) Members of the allanite subgroup are REE-rich minerals typified by the eponymous mineral “allanite”. This subgroup may be derived from clinozoisite by homovalent substitutions and one coupled heterovalent substitution of the type A2 (REE) 3+ + M3 M 2+ → A2 Ca 2+ + M3 M 3+ . Thus the valences...
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Journal Article

PHYLOGENETIC ANALYSIS OF SOME BASAL EARLY CAMBRIAN TRILOBITES, THE BIOGEOGRAPHIC ORIGINS OF THE EUTRILOBITA, AND THE TIMING OF THE CAMBRIAN RADIATION Available to Purchase

BRUCE S. LIEBERMAN
Published: 01 July 2002
Journal of Paleontology (2002) 76 (4): 692–708.
DOI: https://doi.org/10.1666/0022-3360(2002)076<0692:PAOSBE>2.0.CO;2
... of “fallotaspidoids” distributed in the White-Inyo Range of California that have been previously illustrated but not described. These species had been referred to Fallotaspis Hupé, 1953 , and used to define the occurrence of the eponymous Fallotaspis Zone in southwestern Laurentia. However, these two new species...
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View PDF for article title, PHYLOGENETIC ANALYSIS OF SOME BASAL EARLY CAMBRIAN TRILOBITES, THE BIOGEOGRAPHIC ORIGINS OF THE EUTRILOBITA, AND THE TIMING OF THE CAMBRIAN RADIATION
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Figure 13.

View to the SE of Quebrada Retamito, where the eponymous lineament raised t... Available to Purchase

Published: 06 June 2016
Figure 13. View to the SE of Quebrada Retamito, where the eponymous lineament raised the granite block of Cerro Los Gigantes (right in the picture silhouetted against the horizon). Cataclastic rocks occur along this lineament.
Journal Article

Ordovician chitinozoans of the Miaopo Formation at Zhenjin, Upper Yangtze Platform, South China Available to Purchase

Yan Liang, Jaak Nõlvak, Olle Hints
Journal: Palynology
Published: 08 April 2024
Palynology (2024) 48 (2): 2271086.
DOI: https://doi.org/10.1080/01916122.2023.2271086
... , is documented in the lowermost part of the formation. This is the first report of this species in South China. The L. striata Biozone is suggested for the basal part of the formation due to the presence of the eponymous species. The index species of the Laufeldochitina stentor Biozone, the Armoricochitina...
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View PDF for article title, Ordovician chitinozoans of the Miaopo Formation at Zhenjin, Upper Yangtze Platform, South China
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A) Differentiation of the various channel-related environments based on spatial distribution of key ichnofacies associations (see text). Eponymous ichnogenera: B)Scolicia, C)Nereites, D)Ophiomorpha, E)Tisoa, F) phycospiphoniforms, G)Scolicia.

A) Differentiation of the various channel-related environments based on sp... Available to Purchase

Published: 14 January 2020
Fig. 12.— A) Differentiation of the various channel-related environments based on spatial distribution of key ichnofacies associations (see text). Eponymous ichnogenera: B) Scolicia , C) Nereites , D) Ophiomorpha , E) Tisoa , F) phycospiphoniforms, G) Scolicia .
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Effects of fault creep along the hidden section of the S. Gregorio fault, in the eastern part of the eponymous village. The house is located right on the fault trace (footwall on the right); it was progressively damaged, abandoned and finally completely destroyed.

Effects of fault creep along the hidden section of the S. Gregorio fault, i... Available to Purchase

Published: 01 February 2012
Fig. 3 Effects of fault creep along the hidden section of the S. Gregorio fault, in the eastern part of the eponymous village. The house is located right on the fault trace (footwall on the right); it was progressively damaged, abandoned and finally completely destroyed.
Journal Article

A new species of Hirnantia (Orthida, Brachiopoda) and its implications for the Hirnantian age of the Ellis Bay Formation, Anticosti Island, eastern Canada Open Access

Joshua B. Zimmt, Jisuo Jin
Published: 01 January 2023
Journal of Paleontology (2023) 97 (1): 47–62.
DOI: https://doi.org/10.1017/jpa.2022.83
... Ordovician stage, the Hirnantian, has been difficult to identify on Anticosti due to the lack of a traditional Hirnantia fauna within the Upper Ordovician Ellis Bay Formation. Previously, the eponymous taxon of the Hirnantia fauna, and type species of the genus Hirnantia , H. sagittifera (M'Coy, 1851 ) has...
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View PDF for article title, A new species of Hirnantia (Orthida, Brachiopoda) and its implications for the Hirnantian age of the Ellis Bay Formation, Anticosti Island, eastern Canada
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Journal Article

Warm-water Tcherskidium fauna (Brachiopoda) in the Late Ordovician Northern Hemisphere of Laurentia and peri-Laurentia Available to Purchase

Jisuo Jin, Robert B. Blodgett, David A.T. Harper, Christian M.Ø. Rasmussen
Published: 01 November 2022
Journal of Paleontology (2022) 96 (6): 1461–1478.
DOI: https://doi.org/10.1017/jpa.2022.58
..., Siberia, Kazakh and adjacent terranes, and South China. In Laurentia, the eponymous genus Tcherskidium was predominant in regions north of the paleoequator and, in sharp contrast, was absent south of the paleoequator. In this study, Tcherskidium lonei n. sp. and Proconchidium schleyi n. sp. are described...
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View PDF for article title, Warm-water Tcherskidium fauna (Brachiopoda) in the Late Ordovician Northern Hemisphere of Laurentia and peri-Laurentia
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Membership curves for (a) R. australoclavatidites and (b) P. equiexinus plotted against the three named FCM cluster ‘centres’. Percentage occurrences of the named taxon in each ‘centre’ are shown by the solid circle symbol; occurrences in the remaining ‘centres’ are shown in the open circle symbol. R. australoclavatidites has high membership to its eponymous ‘centre’ and low to the P. equiexinus ‘centre’. Its relationship in the transitional ‘centre’ is clear but also shows an overlap in its association outside that ‘centre’ (two-branched dashed line), which clearly shows that its parent plant was present at all times but waxed and waned in abundance with occasionally high abundances outside its eponymous ‘centre’. The relationship of P. equiexinus is less distinct between the three ‘centres’ with the differences being less marked than for R. australoclavatidites. This is may not be so much of a surprise given that the parent plant is a liana and so associated with many other plants, rather than R. australoclavatidites which is from a fern that would be widespread.

Membership curves for ( a ) R. australoclavatidites and ( b ) P. equiexi... Available to Purchase

Published: 01 February 2013
in the open circle symbol. R. australoclavatidites has high membership to its eponymous ‘centre’ and low to the P. equiexinus ‘centre’. Its relationship in the transitional ‘centre’ is clear but also shows an overlap in its association outside that ‘centre’ (two-branched dashed line), which clearly shows
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Field examples of waterfalls lying very close to the fan apex: in Death Valley’s Black Mountains: (A) Badwater and (B) South Badwater 4; in Panamint Valley’s eponymous mountains: (C) South Park Canyon. See Figure 4 for locations.

Field examples of waterfalls lying very close to the fan apex: in Death Val... Available to Purchase

Published: 10 October 2017
Figure 1. Field examples of waterfalls lying very close to the fan apex: in Death Valley’s Black Mountains: (A) Badwater and (B) South Badwater 4; in Panamint Valley’s eponymous mountains: (C) South Park Canyon. See Figure 4 for locations.
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Stratigraphic framework diagram showing the context of the Indian Cave Sandstone at Echo Cliff, NE Kansas. Note that the stratigraphic position of the (presumed) incised body is slightly lower than that of the Indian Cave Sandstone at the eponymous type locality in Nebraska (Fischbein et al. 2009).

Stratigraphic framework diagram showing the context of the Indian Cave Sand... Available to Purchase

Published: 01 February 2015
Fig. 1.— Stratigraphic framework diagram showing the context of the Indian Cave Sandstone at Echo Cliff, NE Kansas. Note that the stratigraphic position of the (presumed) incised body is slightly lower than that of the Indian Cave Sandstone at the eponymous type locality in Nebraska ( Fischbein
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Logistic regression (R2 = 0.98) of a 20-year moving average for the year-on-year percentage of women among new mineral namesakes for 1954–2022. The most recent year with zero women among new mineral namesakes was 2006 when 30 new eponyms honoring men were introduced. Additional moving averages for all data are visualized in Online Materials3 Figure S3, and the same moving averages are visualized for only American namesakes in Online Materials3 Figure S4. (Color online.)

Logistic regression (R 2  = 0.98) of a 20-year moving average for the year-... Available to Purchase

Published: 01 February 2025
Figure 5. Logistic regression (R 2  = 0.98) of a 20-year moving average for the year-on-year percentage of women among new mineral namesakes for 1954–2022. The most recent year with zero women among new mineral namesakes was 2006 when 30 new eponyms honoring men were introduced. Additional moving
Journal Article

First results of GPS measurements on the Ulaanbaatar geodynamic testing area Available to Purchase

A.I. Miroshnichenko, N.A. Radziminovich, A.V. Lukhnev, F.L. Zuev, S. Demberel, D. Erdenezul, M. Ulziibat
Published: 01 August 2018
Russ. Geol. Geophys. (2018) 59 (8): 1049–1059.
DOI: https://doi.org/10.1016/j.rgg.2018.07.023
... × 10 –8 yr –1 ) form an extended area in the center of the testing ground, which is elongated in the northeastern direction, conformably with the strike of the major geologic structures. The strain distribution pattern of the Emeelt network located within the eponymous seismogenic structures...
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