Find research datasets worth reusing

opencc-by-4.0May 2021View details →

The Midlatitude Positive Bay index

The Midlatitude Positive Bay (MPB) index measures the strength of the substorm current wedge.    Version 0.2 On some occasions, the MPB index shows sudden changes when some/one magnetometer co-rotates into/out of the nightside region. To solve this problem, a filter is designed so that the contributions from magnetometers near the dusk/dawn terminators are weighted. The weights smoothly change from 1.0 to 0.0 as the magnetometers co-rotate from nightside to dayside. The new MPB index is very close to the original MPB index, and the sudden changes disappeared. The updated MPB index and onset are calculated using magnetometers at midlatitudes in the nightside region (the method described in Chu et al. [2015]).   Version 0.1 The Original MPB index and onset are calculated using magnetometers at midlatitudes in the nightside region (the method described in Chu et al. [2015]). The MPB index starts from 1991-01-01/00:00:00 and ends on 2019-12-31/23:59:00. Therefore, it has a 1-min resolution and has a total of 15252480. The unit of the MPB index is nT^2 instead of nT. So, you may want to use sqrt(MPB) instead of the raw MPB.   A list of files: The original MPB index is in three formats:     mpb_index.mat     mpb_index.sav     mpb_index.txt. The text file has xMPB, yMPB, and MPB.      MPB = xMPB + yMPB. The xMPB and yMPB are the contributions of the H (northward) and D (eastward) components from different stations.   The original onset files:    onset.mat    onset.txt The onset file has substorm onset, peak time, end time, and MPB peak values.

opencc-by-4.0Jul 2022View details →

Light camera position detection - experiment data

Experiment data measure the accuracy of automatic light fixtures position detection using a single monocular web camera with different resolutions.

opencc-by-4.0Jul 2022View details →

Code and Data associated with "Discovery of positive and purifying selection in metagenomic time series of hypermutator microbial populations"

Code and data sufficient to reproduce analyses in "Discovery of positive and purifying selection in metagenomic time series of hypermutator microbial populations".

Global Positioning System Based on Optical Flow and Convolutional Neural Network

Two datasets used in the paper Global Positioning System Based on Optical Flow and Convolutional Neural Network, to evaluate the proposed CNN model to the task of position estimation. The datasets cover 2 different modes of motion of a drone, and were captured using Google API.

CD8+ T cells of healthy donors sorted for Dextramer positive cells

This dataset is analyzed in the study by Schneider-Hohendorf and colleagues concerning the phenotype of antigen-specific CD8+ T cells.

Weekly Standardized Counts of Influenza Positive Isolates in 4 Region in China Mainland

The data include weekly standardized counts of influenza positive isolates in 4 region in China mainland that covers 30 provinces.More details about the method of standardization and division of regions can be seen in "Characterization of influenza seasonality in China, 2010-2018: implications for seasonal influenza vaccination timing".

Dataset for "In silico Positional Analogue Scanning with Amber GPU-TI"

This repository contains the full data set and analysis scripts to reproduce all results for the manuscript "<a href="https://pubs.acs.org/doi/10.1021/acs.jcim.2c00860">In silico Positional Analogue Scanning with Amber GPU-TI, J. Chem. Inf. Model. 2022, 62, 18, 4448–4459</a>". <a href="https://doi.org/10.1021/acs.jcim.2c00860">https://doi.org/10.1021/acs.jcim.2c00860</a> The repository contains the following data: <ul> <li>20_PDB_66_MOL2_input_coordinates_for_PAS.tar.gz (7.7MB) <ul> <li>input structures of proteins (pdb format), ligands (mol2 format), experimental data and GPU-TI maps for all the 20 scans including Br-Scan, Cl-Scan, F-Scan, HO-Scan, MeO-Scan, Me-Scan, N-Scan.</li> </ul> </li> <li>AMBER18.GPUTI.scripts.tar.gz (597.2 M) <ul> <li>Scripts and example of CDK8 TI output for GPU TI ddG calculation and cycle closure correlation.</li> </ul> </li> <li>Supporting_Information_Tables_dG_ddG_small_big_change.xlsx (60kB)</li> <li>AMBER18_input_fort files, parameter and topology files, first 500 ps equilibrated restart files, amber TI input files for each TI pair calculations (total 12.9 GB) <ul> <li>AMBER-GPUTI_PAS_input.01.N-Scan.CDK8.tar.gz (736.2MB)</li> <li>AMBER-GPUTI_PAS_input.02.N-Scan.Tankyrase.tar.gz (266.1 MB)</li> <li>AMBER-GPUTI_PAS_input.03.N-Scan.HCV_NS5B_gt1b.tar.gz (722.6 MB)</li> <li>AMBER-GPUTI_PAS_input.04.F-Scan.ox1r_antagonist.tar.gz (549.4 MB)</li> <li>AMBER-GPUTI_PAS_input.05.F-Scan.ox2r_antagonist.tar.gz (768.4 MB)</li> <li>AMBER-GPUTI_PAS_input.06.F-Scan.KAT6A.tar.gz (407.9 MB)</li> <li>AMBER-GPUTI_PAS_input.07.F-Scan.PDE1B.tar.gz (470.7 MB)</li> <li>AMBER-GPUTI_PAS_input.08.F-Scan.Akt1_kinase.tar.gz (390.6 MB)</li> <li>AMBER-GPUTI_PAS_input.09.Cl-Scan.PPAR_Gama.tar.gz (412.9 MB)</li> <li>AMBER-GPUTI_PAS_input.10.Cl-Scan.erk12.tar.gz (352.4 MB)</li> <li>AMBER-GPUTI_PAS_input.11.Cl-Scan.KAT6A.tar.gz (408.2 MB)</li> <li>AMBER-GPUTI_PAS_input.12.Br-Scan.PRMT4.tar.gz (522.1 MB)</li> <li>AMBER-GPUTI_PAS_input.13.Me-Scan.BD1_scaffold_thiophene.tar.gz (187.6 MB)</li> <li>AMBER-GPUTI_PAS_input.14.Me-Scan.BD1_scaffold_furan.tar.gz (187.3 MB)</li> <li>AMBER-GPUTI_PAS_input.15.Me-Scan.HIV-1.tar.gz (740.2 MB)</li> <li>AMBER-GPUTI_PAS_input.16.Me-Scan.PPAR_Gama.tar.gz (412.8 MB)</li> <li>AMBER-GPUTI_PAS_input.17.Me-Scan.avb6.tar.gz (2.2 GB)</li> <li>AMBER-GPUTI_PAS_input.18.MeO-Scan.KAT6A.tar.gz (409.3 MB)</li> <li>AMBER-GPUTI_PAS_input.19.MeO-Scan.ox2r_agonist.tar.gz (1.1 GB)</li> <li>AMBER-GPUTI_PAS_input.20.HO-Scan.ox2r_agonist.tar.gz (1.1 GB)  </li> </ul> </li> <li>Data Structures inside each files: <ul> <li>directory_tree.20_PDB_66_MOL2_input_coordinates_for_PAS.txt (5 kB)</li> <li>directory_tree.AMBER18.GPUTI.scripts.txt (91 kB)</li> <li>directory_tree.AMBER18_input_for_PAS_GPUTI_simulations.txt (1.5 MB)</li> </ul> </li> </ul>

Text-fig. 5. SRXTM images of Miranthus elegans gen. et sp. nov.; Mira locality, Portugal. a, b: Transverse sections of flower (a, orthoslice xy0665 close to the apex of placenta; b, orthoslice xy0800 in middle part of placenta) showing remains of calyx with distinct bundles (arrows), ovary wall (ow) and numerous ovules (ov) on the central mushroom-shaped globose placenta (pl) with central column (cc). c: Transverse section of flower (orthoslice xy0620) through perianth and ovary (ow) at a level above the placenta showing ovules (ov) and cellular preservation of the sepal bundles (arrows shown for one sepal); note abaxial surface of sepals with thick-walled epidermal cells, thick cuticle, and fine pointed verrucae. d: Longitudinal section of flower (orthoslice xz0500) showing perigynous position of calyx and semi-inferior ovary (ow, ovary wall) with a central placenta (pl), central column (cc) and numerous ovules (ov); note spiny verrucae on abaxial surface of calyx lobes. Specimens, Mira 100-S153145 (a, b), Mira 100-S170155 (c, d, holotype). Scale bars = 600 µm (a–d). in Early Flowers Of Primuloid Ericales From The Late Cretaceous Of Portugal And Their Ecological And Phytogeographic Implications

Text-fig. 5. SRXTM images of Miranthus elegans gen. et sp. nov.; Mira locality, Portugal. a, b: Transverse sections of flower (a, orthoslice xy0665 close to the apex of placenta; b, orthoslice xy0800 in middle part of placenta) showing remains of calyx with distinct bundles (arrows), ovary wall (ow) and numerous ovules (ov) on the central mushroom-shaped globose placenta (pl) with central column (cc). c: Transverse section of flower (orthoslice xy0620) through perianth and ovary (ow) at a level above the placenta showing ovules (ov) and cellular preservation of the sepal bundles (arrows shown for one sepal); note abaxial surface of sepals with thick-walled epidermal cells, thick cuticle, and fine pointed verrucae. d: Longitudinal section of flower (orthoslice xz0500) showing perigynous position of calyx and semi-inferior ovary (ow, ovary wall) with a central placenta (pl), central column (cc) and numerous ovules (ov); note spiny verrucae on abaxial surface of calyx lobes. Specimens, Mira 100-S153145 (a, b), Mira 100-S170155 (c, d, holotype). Scale bars = 600 µm (a–d).

Text-fig. 7. SEM (a) and SRXTM (b–e) images of Miranthus kvacekii sp. nov.; Mira locality, Portugal. a: Lateral view of flower bud showing corolla lobes extending beyond calyx; note surface of pedicel, calyx and corolla with small equiaxial epidermal cells and indumentum of densely spaced, short stiff trichomes. b, c: Longitudinal sections through floral bud in two directions perpendicular to each other (a, orthoslice yz1024; b, orthoslice xz0950) showing corolla (co), calyx (ca), stamens (st) and semi-inferior ovary with thin ovary wall (ow) and central mushroom-shaped globose placenta (pl) bearing numerous ovules (ov). d, e: Transverse sections through floral bud above placenta (d, orthoslice xy0915; e, orthoslice xy1095) showing calyx (ca), corolla (co), ovary wall (ow) and ovules (ov); yellow outlines indicate the positions of anthers (d) and filaments (e); orange outlines indicate the position of three of the possible staminodes. Specimen, Mira 100-S170157 (a–e, holotype). Scale bars = 600 µm (a–c), 300 µm (d, e). in Early Flowers Of Primuloid Ericales From The Late Cretaceous Of Portugal And Their Ecological And Phytogeographic Implications

Text-fig. 7. SEM (a) and SRXTM (b–e) images of Miranthus kvacekii sp. nov.; Mira locality, Portugal. a: Lateral view of flower bud showing corolla lobes extending beyond calyx; note surface of pedicel, calyx and corolla with small equiaxial epidermal cells and indumentum of densely spaced, short stiff trichomes. b, c: Longitudinal sections through floral bud in two directions perpendicular to each other (a, orthoslice yz1024; b, orthoslice xz0950) showing corolla (co), calyx (ca), stamens (st) and semi-inferior ovary with thin ovary wall (ow) and central mushroom-shaped globose placenta (pl) bearing numerous ovules (ov). d, e: Transverse sections through floral bud above placenta (d, orthoslice xy0915; e, orthoslice xy1095) showing calyx (ca), corolla (co), ovary wall (ow) and ovules (ov); yellow outlines indicate the positions of anthers (d) and filaments (e); orange outlines indicate the position of three of the possible staminodes. Specimen, Mira 100-S170157 (a–e, holotype). Scale bars = 600 µm (a–c), 300 µm (d, e).

Text-fig. 2. Stratigraphic position of the Wischgrund leaf-bearing clay (arrow) on the Klettwitz Tertiary plateau. in New Leaf Species From The Upper Miocene Flora Of The Leaf-Bearing Wischgrund Clay (Lower Lusatia, Brandenburg, Germany)

Text-fig. 2. Stratigraphic position of the Wischgrund leaf-bearing clay (arrow) on the Klettwitz Tertiary plateau.

Text-fig. 4. Correlations of the strata in the Urema Graben, the Cheringoma Plateau and other parts of Mozambique proposed by various authors. The positions of fossiliferous units such as the Grudja and Cheringoma formations have been reasonably stable, whereas correlations of other rock units, especially the Mazamba Formation and the volcanics, have varied a great deal. The time scale is from Gradstein et al. (2020). in Stratigraphy, Chronology And Palaeontology Of The Tertiary Rocks Of The Cheringoma Plateau, Mozambique

Text-fig. 4. Correlations of the strata in the Urema Graben, the Cheringoma Plateau and other parts of Mozambique proposed by various authors. The positions of fossiliferous units such as the Grudja and Cheringoma formations have been reasonably stable, whereas correlations of other rock units, especially the Mazamba Formation and the volcanics, have varied a great deal. The time scale is from Gradstein et al. (2020).

Text-fig. 5. East-west cross section of the Urema Graben and Cheringoma Plateau adapted from Pfaffhuber et al. (2009). The Urema Graben is ca. 45–50 km broad. Note that in this scheme, the Eocene Limestone (i.e., the Cheringoma Fm) is overlain by Oligocene sandstone in the position mapped as Mazamba Formation by Real (1966) and by Tinley (1977). in Stratigraphy, Chronology And Palaeontology Of The Tertiary Rocks Of The Cheringoma Plateau, Mozambique

Text-fig. 5. East-west cross section of the Urema Graben and Cheringoma Plateau adapted from Pfaffhuber et al. (2009). The Urema Graben is ca. 45–50 km broad. Note that in this scheme, the Eocene Limestone (i.e., the Cheringoma Fm) is overlain by Oligocene sandstone in the position mapped as Mazamba Formation by Real (1966) and by Tinley (1977).

Text-fig. 2. Moderately dipping Oligocene layers of the Mány Member in the eastern part of the Strázsa Hill quarry, SW of Zsámbék. The claymarl and siltstone layers cover sandstone and conglomerate. The arrow indicates the position of fossiliferous layers. Photo: László Fodor. in The Late Oligocene Macroflora Of Zsámbék, Central Hungary

Text-fig. 2. Moderately dipping Oligocene layers of the Mány Member in the eastern part of the Strázsa Hill quarry, SW of Zsámbék. The claymarl and siltstone layers cover sandstone and conglomerate. The arrow indicates the position of fossiliferous layers. Photo: László Fodor.

Text-fig. 9. Portnallia. a–j: P. bognorensis M.CHANDLER. a–g: Holotype, V. 30421. a: Oblique lateral view with dorsal surface of locule cast facing towards right side. b: Basal view (original illustration from pl. 28, fig. 40 of Chandler 1961). c–g: Micro CT data. c–f: Surface renderings. c: Lateral view with interlocular septum facing forward. d: lateral view with dorsal surface of locule facing forward. e: Basal view. f: Apical view. g: Digital transverse section near equatorial position showing (c) to u-shaped locules. h: Apical view of tetralocular fruit, V. 30423 (original illustration from pl. 28, fig. 42 of Chandler 1961). i: Transverse section of specimen in (h), reflected light. j–o: P. sheppeyensis M.CHANDLER, Holotype V. 30428, here synomomized with P. bognorensis, from micro-CT data. j–m: Surface renderings. j: Lateral view with interlocular septum facing forward. k: Lateral view with dorsal surface of locule facing forward. l: Basal view. m: Apical view. n: Digital equatorial transverse section showing the three preserved locules and extensive cracking due to pyrite decomposition. o: Translucent volume rendering, apical view showing (c) to u-shaped locules. Scale bars 2 mm, bar in (a) applies also to (b), bar in (e) applies to also to (c, d), bar in (g) applies also to (f), bar in (j) applies to applies also to (k–m). in Mastixioid Fruits (Cornales) From The Early Eocene London Clay Flora: Morphology, Anatomy And Nomenclatural Revision

Text-fig. 9. Portnallia. a–j: P. bognorensis M.CHANDLER. a–g: Holotype, V. 30421. a: Oblique lateral view with dorsal surface of locule cast facing towards right side. b: Basal view (original illustration from pl. 28, fig. 40 of Chandler 1961). c–g: Micro CT data. c–f: Surface renderings. c: Lateral view with interlocular septum facing forward. d: lateral view with dorsal surface of locule facing forward. e: Basal view. f: Apical view. g: Digital transverse section near equatorial position showing (c) to u-shaped locules. h: Apical view of tetralocular fruit, V. 30423 (original illustration from pl. 28, fig. 42 of Chandler 1961). i: Transverse section of specimen in (h), reflected light. j–o: P. sheppeyensis M.CHANDLER, Holotype V. 30428, here synomomized with P. bognorensis, from micro-CT data. j–m: Surface renderings. j: Lateral view with interlocular septum facing forward. k: Lateral view with dorsal surface of locule facing forward. l: Basal view. m: Apical view. n: Digital equatorial transverse section showing the three preserved locules and extensive cracking due to pyrite decomposition. o: Translucent volume rendering, apical view showing (c) to u-shaped locules. Scale bars 2 mm, bar in (a) applies also to (b), bar in (e) applies to also to (c, d), bar in (g) applies also to (f), bar in (j) applies to applies also to (k–m).

Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils. in The Late Early Pleistocene Flora Of Oriolo, Faenza (Italy): Assembly Of The Modern Forest Biome

Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils.

Text-fig. 13. a, d–g: Acer aemilianum. b, c: Acer palmatum and A. sieboldianum modern leaves (NMNS Cleared Leaf Database). a: Oriolo MSF 661, 7-lobed leaf. b: Specimen U 1049, lobe detail showing finely serrate leaf margin. c: Specimen T 0246, 9-lobed leaf with coarsely serrate leaf margin. d: Oriolo MSF 645-1, 9-lobed leaf with two small additional lobes. e: Oriolo MSF 645. f: Oriolo MSF 660, 9-lobed specimen. g: Oriolo MSF 660-1. White arrows indicate position along lamina lobes where marginal serration starts. Scale bars 10 mm (a–c, f, g), 50 mm (d, e). in The Late Early Pleistocene Flora Of Oriolo, Faenza (Italy): Assembly Of The Modern Forest Biome

Text-fig. 13. a, d–g: Acer aemilianum. b, c: Acer palmatum and A. sieboldianum modern leaves (NMNS Cleared Leaf Database). a: Oriolo MSF 661, 7-lobed leaf. b: Specimen U 1049, lobe detail showing finely serrate leaf margin. c: Specimen T 0246, 9-lobed leaf with coarsely serrate leaf margin. d: Oriolo MSF 645-1, 9-lobed leaf with two small additional lobes. e: Oriolo MSF 645. f: Oriolo MSF 660, 9-lobed specimen. g: Oriolo MSF 660-1. White arrows indicate position along lamina lobes where marginal serration starts. Scale bars 10 mm (a–c, f, g), 50 mm (d, e).

Text-fig. 1. a: Map of France showing geographic position of Saint-Bauzile (source: http://d-maps.com/m/europa/france/france/ france09.gif). b: Overview of the active diatomite quarry at the Montagne d'Andance, photograph taken in 2017. c: SEM image of a frustule of pennate diatom (cf. Navicula sp.) from Saint-Bauzile. d) SEM image of frustules forming a colony of centric diatoms (cf. Diatoma sp.) from Saint-Bauzile. in Evidence For Wildfires During Deposition Of The Late Miocene Diatomites Of The Konservat-Lagerstätte Lake Saint-Bauzile (Ardèche, France) - Preliminary Results

Text-fig. 1. a: Map of France showing geographic position of Saint-Bauzile (source: http://d-maps.com/m/europa/france/france/ france09.gif). b: Overview of the active diatomite quarry at the Montagne d'Andance, photograph taken in 2017. c: SEM image of a frustule of pennate diatom (cf. Navicula sp.) from Saint-Bauzile. d) SEM image of frustules forming a colony of centric diatoms (cf. Diatoma sp.) from Saint-Bauzile.

Text-fig. 3. a–e: Berberis auriolensis sp. nov. a: Oriolo MSF 644, Holotype. b: Oriolo MSF 794, asterisks indicate position of teeth. c: Oriolo MSF 784. d: Oriolo MSF 789. e: Oriolo MSF 790. f–h: Modern leaves of Berberis. f: Berberis amurensis var. japonica modern leaf (NMNS Cleared Leaf Database specimen T 0454). g: Berberis koreana modern leaf (NMNS Cleared Leaf Database specimen T 1646). h: Berberis canadensis modern leaf (NMNS Cleared Leaf Database specimen T 1670). i: Epimedium cf. praeaspera Oriolo MSF 778, asterisk indicates position of tooth. j: Clematis aff. vitalba Oriolo MSF 630. Scale bars 10 mm (a–j). in The Late Early Pleistocene Flora Of Oriolo, Faenza (Italy): Assembly Of The Modern Forest Biome

Text-fig. 3. a–e: Berberis auriolensis sp. nov. a: Oriolo MSF 644, Holotype. b: Oriolo MSF 794, asterisks indicate position of teeth. c: Oriolo MSF 784. d: Oriolo MSF 789. e: Oriolo MSF 790. f–h: Modern leaves of Berberis. f: Berberis amurensis var. japonica modern leaf (NMNS Cleared Leaf Database specimen T 0454). g: Berberis koreana modern leaf (NMNS Cleared Leaf Database specimen T 1646). h: Berberis canadensis modern leaf (NMNS Cleared Leaf Database specimen T 1670). i: Epimedium cf. praeaspera Oriolo MSF 778, asterisk indicates position of tooth. j: Clematis aff. vitalba Oriolo MSF 630. Scale bars 10 mm (a–j).

Text-fig. 3. Mastixia parva E.REID et M.CHANDLER. a–g: Holotype, V. 22972. a: Ventral view (original illustration from pl. 25, fig. 13 of Reid and Chandler 1933), reflected light. b–g: from micro-CT data. b: Dorsal view of specimen in (a) now suffering from encrustation due to pyrite decay; isosurface rendering. c: Translucent volume rendering, dorsal view showing two limbs of the locule and longitudinal groove. d–g: Digital transverse sections at various positions showing c-shaped locule, longitudinal dorsal infold, endocarp wall, and degradational cracks. h, i: V. 22983(1). h: Dorsal view showing longitudinal infold. i: Physical transverse section showing c-shaped locule and longitudinal dorsal infold. Scale bars 5 mm in (a–h), applies also to (b–g), 2 mm in (i). in Mastixioid Fruits (Cornales) From The Early Eocene London Clay Flora: Morphology, Anatomy And Nomenclatural Revision

Text-fig. 3. Mastixia parva E.REID et M.CHANDLER. a–g: Holotype, V. 22972. a: Ventral view (original illustration from pl. 25, fig. 13 of Reid and Chandler 1933), reflected light. b–g: from micro-CT data. b: Dorsal view of specimen in (a) now suffering from encrustation due to pyrite decay; isosurface rendering. c: Translucent volume rendering, dorsal view showing two limbs of the locule and longitudinal groove. d–g: Digital transverse sections at various positions showing c-shaped locule, longitudinal dorsal infold, endocarp wall, and degradational cracks. h, i: V. 22983(1). h: Dorsal view showing longitudinal infold. i: Physical transverse section showing c-shaped locule and longitudinal dorsal infold. Scale bars 5 mm in (a–h), applies also to (b–g), 2 mm in (i).

Text-fig. 3. Litho- and biostratigraphic position of fossil floras treated herein, based on lithostratigraphic standard section of upper Oligocene and Miocene in central and eastern Germany (Standke et al. 2010, Escher et al. 2020); only exception from standard section: ** – Thierbach Member restricted to central Germany, replaces Branitz Member in eastern Germany; correlated to global scale of International Chronostratigraphic Chart 2022/02 (Cohen et al. 2013); maximum age ranges of sites/floras indicated by black bars; floristic complexes according to definitions by Mai and Walther 1991 for upper Oligocene, Mai 2000b, 2001b for Miocene; age range of MCO from Steinthorsdottir et al. 2021. in Assessment Of Phytogeographic Reference Regions For Cenozoic Vegetation: A Case Study On The Miocene Flora Of Wiesa (Germany)

Text-fig. 3. Litho- and biostratigraphic position of fossil floras treated herein, based on lithostratigraphic standard section of upper Oligocene and Miocene in central and eastern Germany (Standke et al. 2010, Escher et al. 2020); only exception from standard section: ** – Thierbach Member restricted to central Germany, replaces Branitz Member in eastern Germany; correlated to global scale of International Chronostratigraphic Chart 2022/02 (Cohen et al. 2013); maximum age ranges of sites/floras indicated by black bars; floristic complexes according to definitions by Mai and Walther 1991 for upper Oligocene, Mai 2000b, 2001b for Miocene; age range of MCO from Steinthorsdottir et al. 2021.