cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.14672192.v1
title: <i>Ammitocyon kainos</i> gen. et sp. nov., a chimerical amphicyonid (Mammalia, Carnivora) from the late Miocene carnivore traps of Cerro de los Batallones (Madrid, Spain)

description: In the present paper, we describe the craniodental remains of three individuals of an amphicyonid previously determined as <i>Thaumastocyon</i> sp. from the late Miocene (<i>c</i>. 9.1 Ma) pseudokarstic site of Batallones-3. Dentognathic differences in relation to other Thaumastocyoninae enable a new taxon, <i>Ammitocyon kainos</i> gen. et sp. nov., to be defined; it is both the most recent and the most complete member of this subfamily known in the fossil record. The results of our phylogenetic analysis demonstrate that this new form reached the maximum degree of specialization within Thaumastocyoninae, a group that includes the most hypercarnivorous amphicyonid species of the Miocene. The masticatory apparatus of <i>A. kainos</i> is extremely derived, with the loss of the mesial premolars (P3 / P2 and p1–p3) and the third molars (M3 / m3). The robustness of the chin and muzzle is in contrast with the slender and highly sectorial postcanine dentition (p4 / m2 and P4 / M2), features that are consistent with the values provided by an analysis of the bending resistance of the mandible performed for these specimens. All the anatomical features combined, both cranial and postcranial, reveal the complexity of the body plan of <i>A. kainos</i>. This species combines a derived hypercarnivorous dentition with one of the most robust postcranial skeletons recorded for all large caniform carnivorans, outlining an enigmatic taxon that possesses unique ecological adaptations. https://zoobank.org/urn:lsid:zoobank.org:pub:ABC74B48-5A78-419D-B4ED-02B42B02B886
DOI: 10.6084/m9.figshare.14672166
title: The integrated data of local COVID-19 confirmed cases, human mobility, policy stringency and effective reproduction number

description: The data used in the paper named "Impact of physical distancing policy on reducing transmission of SARS-CoV-2 globally: Perspective from government’s response and residents’ compliance". <br>
DOI: 10.6084/m9.figshare.14672166.v2
title: The integrated data of local COVID-19 confirmed cases, human mobility, policy stringency and effective reproduction number

description: The data used in the paper named "Impact of physical distancing policy on reducing transmission of SARS-CoV-2 globally: Perspective from government’s response and residents’ compliance". <br>
DOI: 10.6084/m9.figshare.14672166.v1
title: The integrated data of local COVID-19 confirmed cases, human mobility, policy stringency and effective reproduction number

description: The data used in the paper named "Impact of physical distancing policy on reducing transmission of SARS-CoV-2 globally: Perspective from government’s response and residents’ compliance". <br>
DOI: 10.6084/m9.figshare.14672199
title: Supplementary Material for: Detectable SARS-CoV-2 RNAemia in Critically Ill Patients, but Not in Mild and Asymptomatic Infections

description: <b><i>Background:</i></b> The SARS-CoV-2 pandemic has challenged many of our current routine practices in the treatment and care of patients. Given the critical importance of blood donation and transfusion we analyzed 92 blood samples of individuals infected with SARS-CoV-2 stratified by symptoms. <b><i>Study Design and Methods:</i></b> We therefore tested blood samples for SARS-CoV-2 via RT-PCR targeting the E gene. In addition, we tested each blood sample for anti-SARS-CoV-2 IgG antibodies via ELISA and performed plaque reduction neutralization tests. <b><i>Results:</i></b> SARS-CoV-2 RNA was absent in the blood of mild to asymptomatic patients (57 individuals) and only detectable in individuals with severe COVID-19 who were admitted to the intensive care unit (35 individuals) (<i>n</i> = 6/92 [6.5%]; <i>p</i> = 0.023 Fisher’s exact test). Interestingly, anti-spike IgG antibodies were not significantly higher in intensive care unit patients compared to mild patients, but we found that their neutralizing capacity was disproportionately increased (<i>p</i> &lt; 0.001). <b><i>Conclusion:</i></b> Our observations support the hypothesis that there are no potential hazards from blood or plasma transfusion of SARS-CoV-2-positive individuals with mild flu-like symptoms and more importantly of asymptomatic individuals.
DOI: 10.6084/m9.figshare.14672199.v1
title: Supplementary Material for: Detectable SARS-CoV-2 RNAemia in Critically Ill Patients, but Not in Mild and Asymptomatic Infections

description: <b><i>Background:</i></b> The SARS-CoV-2 pandemic has challenged many of our current routine practices in the treatment and care of patients. Given the critical importance of blood donation and transfusion we analyzed 92 blood samples of individuals infected with SARS-CoV-2 stratified by symptoms. <b><i>Study Design and Methods:</i></b> We therefore tested blood samples for SARS-CoV-2 via RT-PCR targeting the E gene. In addition, we tested each blood sample for anti-SARS-CoV-2 IgG antibodies via ELISA and performed plaque reduction neutralization tests. <b><i>Results:</i></b> SARS-CoV-2 RNA was absent in the blood of mild to asymptomatic patients (57 individuals) and only detectable in individuals with severe COVID-19 who were admitted to the intensive care unit (35 individuals) (<i>n</i> = 6/92 [6.5%]; <i>p</i> = 0.023 Fisher’s exact test). Interestingly, anti-spike IgG antibodies were not significantly higher in intensive care unit patients compared to mild patients, but we found that their neutralizing capacity was disproportionately increased (<i>p</i> &lt; 0.001). <b><i>Conclusion:</i></b> Our observations support the hypothesis that there are no potential hazards from blood or plasma transfusion of SARS-CoV-2-positive individuals with mild flu-like symptoms and more importantly of asymptomatic individuals.
DOI: 10.25625/8plfns/vhppqd
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Table-1.xls

description: Table 1. Carbon (Ctot, Corg, Ccarb), total sulphur (Stot), and total nitrogen (Ntot) contents of sedimentary rocks of the Ludwigskanal section.
DOI: 10.25625/8plfns/xvtv5z
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-7-Correlation.jpg

description: Figure 7. Correlation of the investigated section Ludwigskanal/Dörlbach with sections from the northern Franconian Alb (Mistelgau: Krumbeck 1932c; Schulbert 2001a, b; Arp and Gropengießer 2015; Basis Mactra Subzone drawn with the “Dumortieria bed I”; Basis Aalensis Subzone defined by FAD of P. subcompta) and Swabian Alb (Rainau-Weiler: Etzold et al. 1989; Gross-Eislingen: Wiedemann 1966; Holzmaden: Hauff 1921; Riegraf 1985a; Urlichs 1977a), with suggested T-R cycles.
DOI: 10.25625/8plfns/pulcmw
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-11-Ammonites.jpg

description: Figure 11. 1. Harpoceras serpentinum (Schlotheim), bed 8, Elegans Subzone, Posidonienschiefer Formation. GZG.INV.70504: d = 197 mm, di = 144 mm, u = 80 mm, wh = 70 mm, wb = 40 mm, rb/2 = n.a.; (leg. Matthias Weißmüller). 2. Dactylioceras sp. forma aegra circumdata (Martin 1858) Hölder 1956, bed 8, Elegans Subzone, Posidonienschiefer Formation. GZG.INV.70505a: d = 53 mm, di = 40.5 mm, u = 22 mm, wh = 13.5 mm, wb = 15 mm, rb/2 = 30. 3. Dactylioceras anguinum (Reinecke), bed 8, Elegans Subzone, Posidonienschiefer Formation. GZG.INV.70505b: d = 40 mm, di = 30 mm, u = 14.5 mm, wh = 11 mm, wb = (11 mm), rb/2 = 31. 4. “Peronoceras” desplacei (d’Orbigny), bed 8, Elegans Subzone, Posidonienschiefer Formation. GZG.INV.70506: d = 68 mm, di = 53 mm, u = 38 mm (56%), wh = 16 mm (24%), wb = 16 mm, rb/2 = 41. 5. Phylloceras heterophyllum (Sowerby), bed 8, Elegans Subzone, Posidonienschiefer Formation. GZG.INV.70507: d = 44 mm, di = 29 mm, u = 4.5 mm, wh = 24 mm, wb = 12 mm, rb/2 = n.a. 6. Cleviceras elegans (Sowerby), bed 8, Elegans Subzone, Posidonienschiefer Formation. GZG.INV.70508: d = 86 mm, di = 53 mm, u = 15 mm, wh = 43 mm, wb = 19 mm, rb/2 = 49. 7. Dactylioceras semiannulatum Howarth, bed 8, Elegans Subzone, Posidonienschiefer Formation. GZG.INV.70509: d = 49 mm, di = 39 mm, u = 26 mm, wh = 12 mm, wb = 13 mm, rb/2 = 30.
DOI: 10.25625/8plfns/kg3hnq
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-10-Ammonites.jpg

description: Figure 10. 1. Pleuroceras solare (Phillips), reworked concretion in bed 4, basis of Hawskerense Subzone, Amaltheenton Formation. GZG.INV.70496: d = 53 mm, di = 39 mm, u = 22 mm, wh = 17 mm, wb = 15 mm, rb/2 = 15. 2. Two specimens of Pleuroceras solare var. solitarium (Simpson), together with a juvenile Amauroceras ferrugineum (Simpson), reworked concretion in bed 4, basis of Hawskerense Subzone, Amaltheenton Formation. GZG.INV.70497a: d = 54 mm, di = 39 mm, u = 21 mm, wh = 17 mm, wb = 15 mm, rb/2 = 15; GZG.INV.70497b: d = 56 mm, di = 40 mm, u = 24 mm, wh = 18 mm, wb = 14 mm, rb/2 = 15; GZG.INV.70497c: d = 11 mm, di = 7 mm, u = 3 mm, wh = 5 mm, wb = 3 mm, rb/2 = 28. 3. Pleuroceras spinatum (Bruguière), 2 m below top of bed 5, Hawskerense Subzone, Amaltheenton Formation. GZG.INV.70498: d = 54 mm, di = 37 mm, u = 23 mm, wh = 19 mm, wb = 18 mm, rb/2 = 11. 4. Pleuroceras spinatum (Bruguière), 50 cm above basis of bed 5, Hawskerense Subzone, Amaltheenton Formation. GZG.INV.70499: d = 76 mm, di = 58 mm, u = 36 mm, wh = 24 mm, wb = 24 mm, rb/2 = 14. 5. Tiltoniceras antiquum (Wright), 1–2 cm above basis of bed 7, Semicelatum Subzone, Posidonienschiefer Formation. Minor part (bright area) of the body chamber restored. GZG.INV.45641a: d = 48 mm, di = 33 mm, u = 12 mm, wh = 20 mm, wb = 12 mm, rb/2 = 22. 6. Tiltoniceras antiquum (Wright), 1–2 cm above basis of bed 7, Semicelatum Subzone, Posidonienschiefer Formation. GZG.INV.45641b: d = 38 mm, di = 26 mm, u = 9 mm, wh = 17 mm, wb = 9 mm, rb/2 = (33); GZG.INV.45641c: d = 27 mm, di = 18 mm, u = 6.5 mm, wh = 11 mm, wb = 7 mm, rb/2 = (30). 7. Lytoceras ceratophagum (Quenstedt), middle part of bed 7, Exaratum Subzone, Posidonienschiefer Formation. GZG.INV.70500: d = 29 mm, di = 18 mm, u = 9 mm, wh = 12 mm, wb = 11 mm, rb/2 = 46. 8. Hildaites murleyi (Moxon), bed 7, Exaratum Subzone, Posidonienschiefer Formation. GZG.INV.70501: d = 41 mm, di = 27 mm, u = 14 mm, wh = 16 mm, wb = 12 mm, rb/2 = 21; (leg. Arno Garbe). 9. Hildaites murleyi (Moxon), together with juvenile Cleviceras exaratum (Young and Bird), bed 7, Exaratum Subzone, Posidonienschiefer Formation. GZG.INV.70502: d = 44 mm, di = 32 mm, u = 17 mm, wh = 15.5 mm, wb = 10 mm, rb/2 = 24; (leg. Arno Garbe). 10. Cleviceras exaratum (Young and Bird), middle part of bed 7, Exaratum Subzone, Posidonienschiefer Formation.GZG.INV.70503: d = 39 mm, di = 27 mm, u = 10 mm, wh = 17 mm, wb = 8 mm, rb/2 = 24.
DOI: 10.25625/8plfns/gqkzah
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-2-Field-Images.jpg

description: Figure 2. Field images of the Ludwigskanal section and ammonites. A. Western section of the canal cutting, showing basal parts of the exposure, from the “Delta-Fossil Bed” to the basis of the Posidonienschiefer Formation. B. Eastern section of the canal cutting, showing the Amaltheenton, Posidonienschiefer, Jurensismergel, and basal parts of the Opalinuston Formation. C. Harpoceras falciferum (Sowerby), “Falciferum Shale”, bed 10, field image (specimen not recovered). D. Polished section of rock sample, from “Fucoid Bed” (bed 17), basal marl of Jurensismergel (bed 18) and “Belemnite Battlefield” (bed 19) to the “Main Phosphorite Bed” (bed 20).
DOI: 10.25625/8plfns/8wi9oa
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-8-Biostratigraphy.jpg

description: Figure 8. Ammonite zones, subzones, and horizons for the NW-European Toarcian according to different authors. 1) Dean et al. 1961; Howarth 1978. 2) Page 2003, 2004. 3) Knitter and Ohmert 1983; Riegraf et al. 1984; Riegraf 1985a; Ohmert et al. 1996; Cresta et al. 2001. 4) Gabilly 1976a; Elmi et al. 1997). Note that Pleydellia (Walkericeras) lugdunensis Elmi & Rulleau, 1997 is considered by Di Cencio and Weis (2020) as junior synonym of P. (W.) pseudolotharingicum Maubeuge, 1950, so that the subzone and horizon is termed accordingly.
DOI: 10.25625/8plfns/llqrc4
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-1-Location.jpg

description: Figure 1. Geographic and geological overview with the location of the Ludwigskanal section (49°21.238938N, 11°21.534298E) at the western margin of the Franconian Alb (S-Germany, Bavaria). Outcrop and subsurface deposits of Lower Jurassic after Freudenberger and Schwerd (1996).
DOI: 10.25625/8plfns/zju4tc
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-4-Geochemistry.jpg

description: Figure 4. Lithology and lithostratigraphy of the Ludwigskanal section (top Amaltheenton to basis Opalinuston Formation) with CaCO3 and organic carbon contents. For legend see Fig. 7.
DOI: 10.25625/8plfns/asgsxw
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-9-Sequences.jpg

description: Figure 9. Sequence stratigraphic interpretation of the Toarcian succession in the Franconian Alb (including Ludwigskanal/Dörlbach section) and adjacent areas. Sedimentary succession and ammonite biostratigraphic evidence according to Pompeckj (1901), Krumbeck (1932b, 1943), Putzer (1939), Bauberger et al. (1969), Meyer and Bauberger (1998) (Regensburg area), Brockert (1959), Fischer (1964), Wiedemann (1966), Urlichs (1977a), Riegraf et al. (1984), Riegraf (1985a), Etzold et al. (1989) (Swabian Alb), Ohmert (1976), Knitter and Ohmert (1983), Ohmert et al. (1996) (Freiburg area), T-R cycles: 1 = third order sequences N-Germany (Zimmermann et al. 2015), 2 = third order sequences France (de Graciansky et al. 1998); 3 = second order sequences Boreal standard (de Graciansky et al. 1998; Jacquin et al. 1998). Eustatic sea level and coastal onlap according to Haq (2018). Note that the definition of sequence boundaries in Haq (2018) differs from the concept of T-R-sequences, with the latter bounded by maximum regression surfaces (Embry and Johannessen 1992; see also Simmons 2012).
DOI: 10.25625/8plfns/doxy0v
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-3-Drilling-Doerlbach.jpg

description: Figure 3. Overview of the Lower Jurassic Schwarzjura Group, Drilling Dörlbach D2 (top ground surface 436 m a.s.l., 49°21.679543N, 11°21.797843E; topographic map sheet 6634 Altdorf b. Nürnberg; unpublished drilling report), ca. 750 m N of the Ludwigskanal/Dörlbach section. For legend see Fig. 7.
DOI: 10.25625/8plfns/m71eue
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-6-Posidonienschiefer-Jurensismergel.jpg

description: Figure 6. Litho- and biostratigraphy of the Posidonienschiefer, Jurensismergel, and basal Opalinuston Formation, Toarcian, exposed at the Ludwigskanal near Dörlbach. For legend see Fig. 7.
DOI: 10.25625/8plfns/xkfkkw
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-14-Ammonites.jpg

description: Figure 14. 1. Grammoceras thouarsense (d’Orbigny), 10 cm below top of bed 21, Thouarsense Subzone, Jurensismergel Formation. GZG.INV.70527: d = 72 mm, di = 50 mm, u = 25 mm, wh = 27 mm, wb = n.a., rb/2 = (25). 2. Alocolytoceras rugiferum (Pompeckj), 20–25 cm below top of bed 23, Dispansum Subzone, Jurensismergel Formation. GZG.INV.70528: d = (39 mm), di = (27 mm), u = 12 mm, wh = 16 mm, wb = n.a., rb/2 = (42). 3. Pseudolioceras cf. boulbiense (Young and Bird), 12–20 cm below top of bed 23, Dispansum Subzone, Jurensismergel Formation. GZG.INV.70529: d = 26 mm, di = 17 mm, u = 5.5 mm, wh = 13 mm, wb = n.a., rb/2 = 13. 4. Alocolytoceras rugiferum (Pompeckj), 20–25 cm below top of bed 23, Dispansum Subzone, Jurensismergel Formation. GZG.INV.70530: d = 76 mm, di = 56 mm, u = 21 mm, wh = 31 mm, wb = n.a., rb/2 = n.a. 5. Phlyseogrammoceras dispansum (Lycett), 12–20 cm below top of bed 23, Dispansum Subzone, Jurensismergel Formation. GZG.INV.70531: d = (30 mm), di = n.a., u = (9 mm), wh = 12 mm, wb = 9 mm, rb/2 = n.a. 6. Dumortieria insignisimilis (Brauns), 11 cm below top of bed 23, basis of Levesquei Subzone, Jurensismergel Formation. GZG.INV.70532: d = 22 mm, di = 17 mm, u = 12 mm, wh = 6 mm, wb = n.a., rb/2 = 20. 7. Dumortieria insignisimilis (Brauns), 11 cm below top of bed 23, basis of Levesquei Subzone, Jurensismergel Formation. GZG.INV.70533: d = 25 mm, di = 17 mm, u = 10.5 mm, wh = 8.5 mm, wb = n.a., rb/2 = 18. 8. Phlyseogrammoceras dispansum (Lycett), 20–25 cm below top of bed 23, Dispansum Subzone, Jurensismergel Formation. GZG.INV.70534: d = 83 mm, di = 61 mm, u = 27 mm, wh = 31 mm, wb = n.a., rb/2 = (45). 9. Dumortieria radiosa (Seebach), 75 cm below top of bed 24, Pseudoradiosa Subzone, Jurensismergel Formation. GZG.INV.70535: d = 73 mm, di = (54 mm), u = 30 mm, wh = 23 mm, wb = n.a., rb/2 = n.a. 10. Hammatoceras insigne (Schübler in Zieten), 15 cm below top of bed 23, Dispansum Subzone, Jurensismergel Formation. GZG.INV.70536: d = (56 mm), di = (42 mm), u = 26 mm, wh = (16 mm), wb = n.a., rb/2 = (28). 11. Dumortieria levesquei (d’Orbigny), 6 cm below top of bed 23, Levesquei Subzone, Jurensismergel Formation. GZG.INV.70537a: d = 34 mm, di = 24 mm, u = 13 mm, wh = 12 mm, wb = n.a., rb/2 = 18. 12. Hammatoceras insigne (Schübler in Zieten), 15 cm below top of bed 23, Dispansum Subzone, Jurensismergel Formation. GZG.INV.70538: d = 29 mm, di = (22 mm), u = (10 mm), wh = 10 mm, wb = 17 mm, rb/2 = (16). 13. Dumortieria levesquei (d’Orbigny), 9 cm below top of bed 23, Levesquei Subzone, Jurensismergel Formation. GZG.INV.70539: d = 32 mm, di = (23 mm), u = (13 mm), wh = 11 mm, wb = 10 mm, rb/2 = 21. 14. Dumortieria pseudoradiosa (Branco), 4 cm below top of bed 23, Levesquei Subzone, Jurensismergel Formation. GZG.INV.70537c: d = 92 mm, di = 70 mm, u = 41 mm, wh = 28 mm, wb = n.a., rb/2 = 32.
DOI: 10.25625/8plfns/ijl64j
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-13-Ammonites.jpg

description: Figure 13. 1. Lytoceras sublineatum (Oppel), 38 cm below top of bed 16, Variabilis Subzone, Posidonienschiefer Formation. The telescope-like, shallow constrictions in this juvenile specimen are reminiscent of Pleurolytoceras propehircinum Krumbeck of the Aalensis Subzone, but the high wb/wh ratio points to Lytoceras sublineatum (Oppel). GZG.INV.70518: d = 17 mm, di = 10.5 mm, u = 5 mm, wh = 7.5 mm, wb = 10 mm, rb/2 = 10. 2. Catacoeloceras raquinianum (d’Orbigny), 19 cm below top of bed 16, Variabilis Subzone, Posidonienschiefer Formation. GZG.INV.70519: d = 45 mm, di = 35 mm, u = 21 mm, wh = 12.5 mm, wb = 16 mm, rb/2 = 18. 3. Catacoeloceras raquinianum (d’Orbigny), 13 cm below top of bed 16, Variabilis Subzone, Posidonienschiefer Formation. GZG.INV.70520: d = 35 mm, di = 26 mm, u = 14 mm, wh = 11.5 mm, wb = 15 mm, rb/2 = 13. 4. Pseudogrammoceras subregale (Pinna), 4 cm below top of bed 18, Illustris Subzone, Jurensismergel Formation. GZG.INV.70521; d = 107 mm, di = 77 mm, u = 46 mm, wh = 34 mm, wb = n.a., rb/2 = (48). 5. Haugia cf. phillipsi (Simpson), 3 cm below top of bed 18, Illustris Subzone, Jurensismergel Formation. GZG.INV.70522; d = (125 mm), di = n.a., u = n.a., wh = 46 mm, wb = n.a., rb/2 = (22). 6. Catacoeloceras raquinianum (d’Orbigny), basis of bed 19, Variabilis Subzone, Posidonienschiefer Formation. GZG.INV.70523: d = 62 mm, di = 49 mm, u = 31 mm, wh = 15 mm, wb = (16 mm), rb/2 = 13. 7. Osperleioceras bicarinatum (Zieten), phosphorite nodule in bed 20, condensed transition Variabilis-Thouarsense Zone, Jurensismergel Formation. GZG.INV.70524: d = 25 mm, di = 15 mm, u = 3.5 mm, wh = 14 mm, wb = 6 mm, rb/2 = (18). 8. Lytoceras cornucopia (Young & Bird), marl matrix of bed 20, condensed transition Variabilis-Thouarsense Zone, Jurensismergel Formation. GZG.INV.70525: d = 66 mm, di = 46 mm, u = 23 mm, wh = 27 mm, wb = (28 mm), rb/2 = n.a. 9. Denckmannia rude (Simpson), phosphorite nodule in bed 20, condensed transition Variabilis-Thouarsense Zone, Jurensismergel Formation. GZG.INV.70526: d = 86 mm, di = 58 mm, u = 32 mm, wh = 32 mm, wb = (26 mm), rb/2 = n.a.
DOI: 10.25625/8plfns/9grpko
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-12-Ammonites.jpg

description: Figure 12. 1. Dactylioceras cf. commune (Sowerby), lower bedding plane of bed 12, Commune Subzone, Posidonienschiefer Formation. GZG.INV.70510a: d = 61 mm, di = 49 mm, u = 34 mm, wh = 14 mm, wb = n.a., rb/2 = (24); GZG.INV.70510b: d = 45 mm, di = 35 mm, u = 27 mm, wh = 10 mm, wb = n.a., rb/2 = (25). 2. Hildoceras cf. lusitanicum Meister, lower bedding plane of bed 12, Commune Subzone, Posidonienschiefer Formation. GZG.INV.70511: d = 92, di = (68 mm), u = 43 mm, wh = 26 mm, wb = (12 mm), rb/2 = (27). 3. Dactylioceras athleticum (Simpson), middle part of bed 12, Commune Subzone, Posidonienschiefer Formation. GZG.INV.70512: d = 64 mm, di = 51 mm, u = 38 mm, wh = 13.5 mm, wb = 13.5 mm, rb/2 = 37. 4. Hildoceras semipolitum Buckman, 18 cm below top of bed 15, Crassum Subzone, Posidonienschiefer Formation. GZG.INV.70513: d = 40 mm, di = 28 mm, u = 12 mm, wh = 16.5 mm, wb = n.a., rb/2 = (23). 5. Hildoceras semipolitum Buckman, 18 cm below top of bed 15, Crassum Subzone, Posidonienschiefer Formation. Field image: d = (30 mm), di = (23 mm), u = 11 mm, wh = 10 mm, wb = n.a., rb/2 = (24). 6. Mucrodactylites mucronatus (d’Orbigny), 43 cm below top of bed 16, Variabilis Subzone, Posidonienschiefer Formation. GZG.INV.70514: d = 20 mm, di = (15 mm), u = 9 mm, wh = 6.5 mm, wb = 8 mm, rb/2 = 17. 7. Mucrodactylites mucronatus (d’Orbigny), bed 16 ex situ, Variabilis Subzone, Posidonienschiefer Formation. leg. Volker Münzner: d = 22 mm, di = 16.5, u = 10 mm, wh = 6 mm, wb = 6 mm, rb/2 = 18. 8. Haugia variabilis (d’Orbigny), 13 cm below top of bed 16, Variabilis Subzone, Posidonienschiefer Formation. GZG.INV.45642: d = 67 mm, di = 44 mm, u = 20 mm, wh = 27 mm, wb = n.a., rb/2 = 27. 9. Haugia jugosa (Sowerby), 3 cm below top of bed 16, Variabilis Subzone, Posidonienschiefer Formation. GZG.INV.70515: d = 71 mm, di = 46 mm, u = 19 mm, wh = 30 mm, wb = n.a., rb/2 = 34. 10. Pseudolioceras compactile (Simpson), 37 cm below top of bed 16, Crassum Subzone, Posidonienschiefer Formation. GZG.INV.70516: d = 32 mm, di = 19 mm, u = 4.5 mm, wh = 17 mm, wb = 7 mm, rb/2 = 21. 11. Pseudolioceras compactile (Simpson), 32 cm below top of bed 16, Crassum Subzone, Posidonienschiefer Formation. GZG.INV.70517: d = 30 mm, di = 20 mm, u = 5 mm, wh = 15 mm, wb = n.a., rb/2 = 15.
DOI: 10.25625/8plfns/co3lte
title: Arp-et-al-2021-Toarcian-Ludwigskanal-Fig-5-Amaltheenton.jpg

description: Figure 5. Litho- and biostratigraphy of the upper Amaltheenton Formation, Upper Pliensbachian, exposed at the Ludwigskanal. For legend see Fig. 7.
DOI: 10.25625/8plfns
title: Data for publication 'Biostratigraphy and sequence stratigraphy of the Toarcian Ludwigskanal section (Franconian Alb, Southern Germany)'

description: 15 Figures (location map, sections, stratigraphic schemes, ammonites) and 1 Table of geochemical data of Lower Jurassic sedimentary rocks (Amaltheenton, Posidonienschiefer, Jurensismergel, Opalinuston) of the Ludwigskanal section (Lower Jurassic, Southern Germany).