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Fig. 6 in Tolerance of Capsicum frutescens L. (Solanales: Solanaceae) to the duration of waterlogging and impact on the post-waterlogging and recovery periods

Fig. 6 - Shoot biomass (A) and root biomass (B) after waterlogging and the end of the recovery period. Means and standard errors were based on five replications. Bars with different letters under the same category indicated a significant difference (p ≤ 0,05) with a paired t-test. C-AW: control after waterlogging, C-ER: control of the end recovery period, AW: after waterlogging, ER: the end of the recovery period. / Biomassa dei germogli (A) e delle radici (B) dopo il ristagno d'acqua e al termine del periodo di recupero. Le medie e gli errori standard si basano su cinque repliche. Le barre con lettere diverse sotto la stessa categoria indicano una differenza significativa (p ≤ 0,05) con un t-test a coppie. C-AW: controllo dopo il ristagno idrico, C-ER: controllo alla fine del periodo di recupero, AW: dopo il ristagno idrico, ER: alla fine del periodo di recupero.

Fig. 5 in Tolerance of Capsicum frutescens L. (Solanales: Solanaceae) to the duration of waterlogging and impact on the post-waterlogging and recovery periods

Fig. 5 - Relationship between shoot biomass and root biomass with waterlogging duration. Measurements were made after the flooding ended. Shoot biomass in control (A), Shoot biomass in waterlogging duration treatment (B). Root biomass in control (C), root biomass in the waterlogging duration treatment (B). / Relazione tra la biomassa dei germogli e la biomassa delle radici con la durata del ristagno idrico. Le misurazioni sono state effettuate dopo la fine dell'allagamento. Biomassa dei germogli nel controllo (A), biomassa dei germogli nel trattamento di durata crescente del ristagno idrico (B). Biomassa radicale nel controllo (C), biomassa radicale nel trattamento di durata crescente del ristagno idrico (B).

Fig. 4 in Tolerance of Capsicum frutescens L. (Solanales: Solanaceae) to the duration of waterlogging and impact on the post-waterlogging and recovery periods

Fig. 4 - The pattern of plant height (A) and number of leaves (B) during waterlogging and recovery period. Initial: before waterlogging treatment, AW-1d: after waterlogging one day, AW-3d: after waterlogging three days, AW-10d: after waterlogging ten days, R1: one-week recovery period, R2: two-week recovery period, R3: threeweek recovery period, R4: four-week recovery period, ER: end of the recovery period. / Andamento dell'altezza delle piante (A) e del numero di foglie (B) durante il periodo di ristagno idrico e di recupero. Iniziale: prima del trattamento di ristagno idrico, AW-1d: dopo un giorno di ristagno idrico, AW-3d: dopo tre giorni di ristagno idrico, AW-10d: dopo dieci giorni di ristagno idrico, R1: periodo di recupero di una settimana, R2: periodo di recupero di due settimane, R3: periodo di recupero di tre settimane, R4: periodo di recupero di quattro settimane, ER: fine del periodo di recupero.

Fig. 1 in Tolerance of Capsicum frutescens L. (Solanales: Solanaceae) to the duration of waterlogging and impact on the post-waterlogging and recovery periods

Fig. 1 - Plant response after waterlogging and the end of the recovery period. Stomata opened at the control (A), stomata closed after waterlogging AW (B), stomata opened at ER (C), there was no hypertrophic lenticels formation at the control (D), a whitish color marked the early formation of hypertrophic lenticels after waterlogging AW at the base of the stems that were flooded for three days (E), the development of hypertrophic lenticels on the seventh day of waterlogging (F), and adventitious root formation on the ninth day of waterlogging (G). The scale bars (yellow line) in D, E, F, and G are 5 cm. / Risposta delle piante dopo il ristagno d'acqua e alla fine del periodo di recupero. Gli stomi si sono aperti al controllo (A), gli stomi si sono chiusi dopo il periodo di ristagno idrico AW (B), gli stomi si sono aperti ER (C), non c'è stata formazione di lenticelle ipertrofiche al controllo (D), il colore biancastro ha indicato la formazione precoce di lenticelle ipertrofiche dopo il periodo di ristagno idrico AW alla base degli steli sommersi per tre giorni (E), lo sviluppo di lenticelle ipertrofiche al settimo giorno di ristagno idrico (F) e la formazione di radici avventizie al nono giorno di ristagno idrico (G). Le barre di scala (linea gialla) in D, E, F e G sono di 5 cm.

Fig. 3 in Tolerance of Capsicum frutescens L. (Solanales: Solanaceae) to the duration of waterlogging and impact on the post-waterlogging and recovery periods

Fig. 3 - The content of total chlorophyll (A) and carotenoids (B) after waterlogging and the end of the recovery period. Means and standard errors were based on five replications. Bars with different letters under the same category indicated a significant difference (p ≤ 0,05) with a paired t-test. C-AW: control after waterlogging, C-ER: control of the end recovery period, AW: after waterlogging, ER: the end of the recovery period. / Contenuto di clorofilla totale (A) e carotenoidi (B) dopo il ristagno idrico e al termine del periodo di recupero. Le medie e gli errori standard si basano su cinque repliche. Le barre con lettere diverse sotto la stessa categoria indicano una differenza significativa (p ≤ 0,05) con un t-test a coppie. C-AW: controllo dopo il ristagno idrico, C-ER: controllo alla fine del periodo di recupero, AW: dopo il ristagno idrico, ER: alla fine del periodo di recupero.

Fig. 2 in Tolerance of Capsicum frutescens L. (Solanales: Solanaceae) to the duration of waterlogging and impact on the post-waterlogging and recovery periods

Fig. 2 - Relationship between total chlorophyll and carotenoid content with waterlogging duration. Measurements were made after the flooding ended. Total chlorophyll in control (not waterlogging) (A), and waterlogging duration treatment (B). Carotenoid content in control (C), and the treatment with increasing waterlogging duration (D). / Relazione tra il contenuto di clorofilla totale e carotenoidi con la durata del ristagno idrico. Le misurazioni sono state effettuate dopo la fine del periodo di allagamento. Clorofilla totale nel controllo (senza ristagno d'acqua) (A) e nel trattamento con l'aumento della durata del ristagno idrico (B). Contenuto di carotenoidi nel controllo (C) e nel trattamento con l'aumento della durata del ristagno idrico (D).

opencc-by-4.0Mar 2015View details →

Fig.2. A in Evidences for the Lynx recovery in Bulgaria: the Lynx discovered in Western Rhodopes

Fig.2. A second photo of the same animal made by the camera trap an hour after the first one. The dark end of the tail is visible.

opencc-by-4.0Mar 2015View details →

Fig.1. A in Evidences for the Lynx recovery in Bulgaria: the Lynx discovered in Western Rhodopes

Fig.1. A night picture of a lynx photographed (V.P.) in August, 2014 by a camera trap in the region between Trigrad and Yagodina.

opencc-by-4.0Aug 2015View details →

Fig. 1. Samples were identified within a in Diversity of Cryptosporidium in brush-tailed rock-wallabies (Petrogale penicillata) managed within a species recovery programme

Fig. 1. Samples were identified within a phylogenetic framework with the tree constructed using neighbour-joining with bootstrap test (1,000 replicates, displayed at nodes) using the 18S rRNA locus (878 bp). KV denotes Kangaroo Valley.

opencc-by-4.0May 2018View details →

Influence of storm sequencing and beach recovery on sediment transport and beach resilience data set at CIEM large scale wave flume.

The Influence of storm sequencing and beach recovery on sediment transport and beach resilience (RESIST) experiments project proposes to study experimentally sequences of storm induced erosion and beach recovery, with a particular focus on the poorly known morphodynamic processes under low energy conditions. Series of large scale experimental tests were done to collect data on the cross-shore hydrodynamics, sediment transport and beach evolution. The main aim of this proposal is to investigate the influence of sequences of beach erosion-recovery in the overall beach profile evolution. The tested wave conditions (2 erosive and 3 Accretive bichromatic conditions) were combined to form three sequences of changing high/mild energy conditions. Each condition started from an initial beach 1/15 handmade profile. The experiments were carried out in the large scale wave flume CIEM at Universitat Politècnica de Catalunya (UPC), Barcelona within the program of Transnational Access of Hydralab+. Due to its size, the data set can not be placed on this repository and will be provided on demand. Please contact with the authors or with the data manager of the CIEM installation.

opencc-by-4.0Oct 2019View details →

Research data supporting for "Characterization of recovery onset by subgrain and grain boundary migration in experimentally deformed polycrystalline olivine"

Abstract: To apprehend plate tectonics and the dynamics of the lithosphere–asthenosphere boundary, composed principally of olivine, we need to understand the mechanisms that control plastic deformation of olivine in the relevant temperature domain. After more than 50 years of laboratory studies and investigations on natural rocks, the interplay of several key parameters (e.g. temperature, pressure, vacancy concentration, dislocation densities, grain size, strain rate) controlling polycrystalline olivine plasticity remains difficult to assess. Here, we study four olivine polycrystals, which have been deformed in axial compression under a confining pressure of 300MPa, at 1273 or 1473 K. Despite significant differences in mechanical properties (stress–strain curves), previous characterization by scanning (SEM) and transmission electron microscopy (TEM) did not reveal significant differences in dislocation microstructures which could explain these contrasted behaviours. We have undertaken automatic crystallographic orientation mapping (ACOM) analyses in TEM to increase the spatial resolution of characterization compared to previously obtained electron backscatter diffraction maps to further decipher the microstructures at nanoscale. With this novel technique applied to olivine, a noticeable difference in the onset of microstructural recovery has been identified between specimens deformed at 1273 and 1473 K. The microstructures of the olivine polycrystals deformed at 1473K exhibit numerous curved grain and subgrain boundaries, advocating for recovery by boundary migration. In contrast, the microstructures of the olivine polycrystals deformed at 1273K have significantly fewer subgrain boundaries and show more straight boundaries (i.e. closer to an equilibrium microstructure) than in the specimen deformed at 1473 K. Characterization by ACOM-TEM has permitted the identification of the onset of recovery, which is led by boundary migration even for very low macroscopic finite strains.

Fig. 17 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 17. Comprehensive model of the Spathian (Lower Triassic) Virgin Formation as recorded in south−western Utah. A. Distribution of sedimentary facies and faunal assemblages. B. Diversity gradient along the general environmental gradient.

Fig. 16 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 16. Trace fossils of the Spathian, Lower Triassic Virgin Formation. A. Thalassinoides cf. suevicus Rieth, 1932 in lower bedding plane view found at the base of beds containing sample BD−A−7, PIMUZ29586. B. Palaeophycus montanus Hall, 1847 in upper bedding plane view observed the lower calcareous unit of section HC−A. C. Spongeliomorpha isp. found at the base of grainstone which represents a lateral equivalent of BD−A−7 in the section BD−C. +

Fig. 14 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 14. Characteristics of the Protogusarella smithi Association showing frequency distribution, trophic nucleus (A) and ecological structure (B). The numbers in the pie−chart sections correspond with the species pertaining to each guild.

Fig. 15. A, B in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 15. A, B. Characteristics of the Piarorhynchella triassica Association showing frequency distribution, trophic nucleus (A) and ecological structure (B). C, D. Characteristics of the Bakevellia costata Assemblage showing frequency distribution and trophic nucleus (C) and ecological structure (D). The numbers in the pie−chart sections correspond with the species pertaining to each guild.

Fig. 13 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 13. Characteristics of the Eumorphotis ericius Association showing frequency distribution, trophic nucleus (A) and ecological structure (B).The numbers in the pie−chart sections correspond with the species pertaining to each guild.

Fig. 12 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 12. Characteristics of the Bakevellia exporrecta Association showing frequency distribution and trophic nucleus (A) and ecological structure (B). The numbers in the pie−chart sections correspond with the species pertaining to each guild.

Fig. 11. Q in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 11. Q (samples) and R−mode (species) cluster analysis using the unweighted paired group algorithm and Morisita index of similarity. Classes of abundances (circle size) represent the quintiles of absolute−abundance frequencies. Bootstrap values are shown in the white boxes within the Q−mode cluster. Dominance is given as D = 1−Simpson index. A. Bakevellia exporrecta Association. B. Eumorphotis ericius Association. C. Protogusarella smithi Association D. Piarorhynchella triassica Association. E. Bakevellia costata Assemblage. F. Main R−mode cluster incorporating the nuclei of several associations. G. Subcluster reflecting the nucleus of the Bakevellia exporrecta Association and it probably incorporates those species, which are adapted to low energy, softground conditions. H. Subcluster reflecting the nuclei of the Eumorphotis ericius Association and Protogusarella smithi Association, and it incorporates species adapted to high energy, near shore conditions.

Fig. 10 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 10. Fossil bivalves from the Spathian (Lower Triassic) Virgin Formation, Utah, USA. A. Astartidae sp. A, PIMUZ29588. B. Bakevellia exporrecta, PIMUZ29592. C. Bakevellia costata, PIMUZ29614. D. Myalinella sp. A, PIMUZ29597. E. Sementiconcha recuperator, PIMUZ29600. F. Protopis sp. A, PIMUZ29609. G. Leptochondria nuetzeli, PIMUZ29615. H. Eumorphotis virginensis, PIMUZ29616. I. Neoschizodus laevigatus, PIMUZ29599. J. Trigonodus cf. sandbergeri, PIMUZ29603. K. Trigonodus cf. orientalis, PIMUZ29604. L. Unionites cf. fassaensis, PIMUZ2960. M. Promyalina spathi, PIMUZ296102. N. Unionites cf. canalensis, PIMUZ29596. O. Promyalina putiatinensis, PIMUZ29601. P. Pernopecten sp. A., PIMUZ29590. Q. Eumorphotis ericius, PIMUZ29587. R. Eumorphotis cf. multiformis, PIMUZ29613. S. Eumorphotis cf. venetiana, PIMUZ29593. Scale bars 5 mm; except O, P, Q 10 mm.

Fig. 9 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery

Fig. 9. Fossils of the Spathian (Lower Triassic) Virgin Formation, Utah, USA. A. Natiria cf. costata, PIMUZ29595. B. Gastropod ind. A, PIMUZ29594. C. Piarorhynchella triassica, PIMUZ29589. D. Protogusarella smithi, PIMUZ29612. E. Field photograph of Holocrinus smithi, specimen not collected. Topmost limestone of Section HC−A. F. Tirolites sp. A, PIMUZ29591. G. Cypellospongia sp. A, PIMUZ29598. H. Spines of Miocidaris utahensis, PIMUZ29611. Scale bars 5 mm.