cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.20714392.v2
title: Supplementary Table S3-S5 new manuscript

description: This datasheet contains the Supplementary Tables listed below, which are separate sheets of a single excel file named Supplementary Table S3-S5 new manuscript to complement the data and analyses of the manuscript entitled: Multiple approaches define the bacterial ancestry of mitochondria. <br> <strong>Supplementary Table S3.</strong> Tabulation of 20 aerobic traits (Box1) and their cumulative score in 15 alphaproteobacterial lineages plus 20 aerobic mitochondria from eukaryotes. The rightmost column shows the sum values for the 2-oxoacid:ferredoxin oxidoreductases (OFORs) considered as traits of anaerobic metabolism. <strong>Supplementary Table S3B.</strong> Statistical results of the T test on the lineage-specific scores of aerobic traits listed in Table S3. Lineages displaying high levels of P values (&gt;0.1) indicating no significant difference with respect to aerobic mitochondria are highlighted in pale purple. <strong>Supplementary Table S4. </strong>Distribution of <em>spt</em> (the gene for serine-palmitoyl transferases) and allied genes for ceramide biosynthesis, as well as of <em>kynU</em> (gene for kynureninase) and allied genes of the kynurenine pathway among 15 lineages of alphaproteobacteria. When the <em>kynA</em> gene for tryptophan di-oxygenase gene lies in the same genomic region of <em>kynU</em> it is annotated as 1. <strong>Supplementary Table S5</strong>. Distribution of four enzymes for cardiolipin metabolism along the alphaproteobacterial lineages, cf. Fig. 3E. Taxa with both types of cardiolipin synthase are highlighted in pale green. <br> We add to the above Tables the separate MEGAX file named Contig829 with the DNA sequence of the re-assembled metagenomic DNA sequence for Alphaproteobacteria J134 from Ward et al (2019) DOI: 10.1264/jsme2.ME19017 . <br> <br>
DOI: 10.6084/m9.figshare.20714392.v1
title: Supplementary Table S3-S5 new manuscript

description: This datasheet contains the Supplementary Tables listed below, which are separate sheets of a single excel file named Supplementary Table S3-S5 new manuscript to complement the data and analyses of the manuscript entitled: Multiple approaches define the bacterial ancestry of mitochondria. <br> <strong>Supplementary Table S3.</strong> Tabulation of 20 aerobic traits (Box1) and their cumulative score in 15 alphaproteobacterial lineages plus 20 aerobic mitochondria from eukaryotes. The rightmost column shows the sum values for the 2-oxoacid:ferredoxin oxidoreductases (OFORs) considered as traits of anaerobic metabolism. <strong>Supplementary Table S3B.</strong> Statistical results of the T test on the lineage-specific scores of aerobic traits listed in Table S3. Lineages displaying high levels of P values (&gt;0.1) indicating no significant difference with respect to aerobic mitochondria are highlighted in pale purple. <strong>Supplementary Table S4. </strong>Distribution of <em>spt</em> (the gene for serine-palmitoyl transferases) and allied genes for ceramide biosynthesis, as well as of <em>kynU</em> (gene for kynureninase) and allied genes of the kynurenine pathway among 15 lineages of alphaproteobacteria. When the <em>kynA</em> gene for tryptophan di-oxygenase gene lies in the same genomic region of <em>kynU</em> it is annotated as 1. <strong>Supplementary Table S5</strong>. Distribution of four enzymes for cardiolipin metabolism along the alphaproteobacterial lineages, cf. Fig. 3E. Taxa with both types of cardiolipin synthase are highlighted in pale green. <br>
DOI: 10.6084/m9.figshare.16545644
title: 4D volcanic geology of Hachijo-jima islet, Izu-Bonin arc

description: This study combines detailed geologic mapping, tephrochronology, U-Pb zircon dating, and published drill core data to evaluate the time transgressive 3-dimensional (thus 4-dimensional) structure and evolution of the two volcanoes on Hachijo-jima of the juvenile Izu-Bonin intra oceanic arc. The regional Ata-Torihama tephra (Ata-Th; 0.24 Ma) and Kikai-Tozurahara tephra (K-Tz; 0.095 Ma) from Kyushu are intercalated within the voluminous proximal volcanic products. The silicic tuff cover of some supra-subduction zone ophiolites, that formed in a nascent arc setting, may be ancient analogs of the regional tephra derived from the adjacent but mature volcanic arc. The volcanic succession comprises submarine volcanic basement, marine volcaniclastic rocks, and terrestrial tuff intercalated with tholeiitic basalt and the exotic calc-alkaline tephra layers. The undissected Hachijo-Fuji stratovolcano (tholeiitic basalt) overlies marine volcaniclastics abutting the northwestern paleo sea cliffs of the older dissected volcano, Mihara-yama. Newly-described folding and normal faulting of the marine and overlying terrestrial volcaniclastic rocks record NW-SE shortening that may be associated with the collision of the Izu-Bonin arc with the Honshu arc, analogous to the NNE-SSW shortening observed for the Troodos ophiolite. The proto Hachijo-jima volcano emerged above the sea &gt;0.24 Ma, and this date can be applied as a molecular biological calibration date for organisms on this island.
DOI: 10.6084/m9.figshare.16545644.v3
title: 4D volcanic geology of Hachijo-jima islet, Izu-Bonin arc

description: This study combines detailed geologic mapping, tephrochronology, U-Pb zircon dating, and published drill core data to evaluate the time transgressive 3-dimensional (thus 4-dimensional) structure and evolution of the two volcanoes on Hachijo-jima of the juvenile Izu-Bonin intra oceanic arc. The regional Ata-Torihama tephra (Ata-Th; 0.24 Ma) and Kikai-Tozurahara tephra (K-Tz; 0.095 Ma) from Kyushu are intercalated within the voluminous proximal volcanic products. The silicic tuff cover of some supra-subduction zone ophiolites, that formed in a nascent arc setting, may be ancient analogs of the regional tephra derived from the adjacent but mature volcanic arc. The volcanic succession comprises submarine volcanic basement, marine volcaniclastic rocks, and terrestrial tuff intercalated with tholeiitic basalt and the exotic calc-alkaline tephra layers. The undissected Hachijo-Fuji stratovolcano (tholeiitic basalt) overlies marine volcaniclastics abutting the northwestern paleo sea cliffs of the older dissected volcano, Mihara-yama. Newly-described folding and normal faulting of the marine and overlying terrestrial volcaniclastic rocks record NW-SE shortening that may be associated with the collision of the Izu-Bonin arc with the Honshu arc, analogous to the NNE-SSW shortening observed for the Troodos ophiolite. The proto Hachijo-jima volcano emerged above the sea &gt;0.24 Ma, and this date can be applied as a molecular biological calibration date for organisms on this island.
DOI: 10.6084/m9.figshare.16571366
title: Ordovician crustal thickening and syn-collisional magmatism of Iran: Gondwanan basement along the north of the Yazd Block (Central Iran)

description: This study investigates relicts of some granitic Gondwanan basement unexpectedly outcropping in the northwest of Central-East Iranian Microcontinent (CEIM) and incorporated into an ophiolitic mélange. Based on petrographical (e.g. high modal content of muscovite (~10 vol.%), absence of hornblende, inherited zircons (&gt;541 Ma)), geochemical (peraluminous and calc-alkaline S-type affinity, high silica, high ‘light rare earth element (LREE)/heavy rare earth element (HREE)’ ratios, negative Nb and Ti anomalies), and geochronological (magmatic zircon age ~448 Ma) results, it is an Ordovician anatectic granite formed from a sedimentary source during crustal thickening in a syn-collisional setting. It shows some signatures of metamorphic deformation (cataclastic fabric, quartz bulging recrystallization, and foliation) likely developed in the Devonian (~410 Ma). The U-Pb zircon ages from this granite are analogous to the other Ordovician collision-related magmatic events in the CEIM (Chahak to Airekan, Balvard). Our results confirm that Cadomian subduction and closure of the Proto-Tethys Ocean to the north of the Gondwana supercontinent resulted in crustal thickening during Ordovician collision-related magmatism and Devonian-Carboniferous regional metamorphism in the CEIM.
DOI: 10.6084/m9.figshare.16571366.v2
title: Ordovician crustal thickening and syn-collisional magmatism of Iran: Gondwanan basement along the north of the Yazd Block (Central Iran)

description: This study investigates relicts of some granitic Gondwanan basement unexpectedly outcropping in the northwest of Central-East Iranian Microcontinent (CEIM) and incorporated into an ophiolitic mélange. Based on petrographical (e.g. high modal content of muscovite (~10 vol.%), absence of hornblende, inherited zircons (&gt;541 Ma)), geochemical (peraluminous and calc-alkaline S-type affinity, high silica, high ‘light rare earth element (LREE)/heavy rare earth element (HREE)’ ratios, negative Nb and Ti anomalies), and geochronological (magmatic zircon age ~448 Ma) results, it is an Ordovician anatectic granite formed from a sedimentary source during crustal thickening in a syn-collisional setting. It shows some signatures of metamorphic deformation (cataclastic fabric, quartz bulging recrystallization, and foliation) likely developed in the Devonian (~410 Ma). The U-Pb zircon ages from this granite are analogous to the other Ordovician collision-related magmatic events in the CEIM (Chahak to Airekan, Balvard). Our results confirm that Cadomian subduction and closure of the Proto-Tethys Ocean to the north of the Gondwana supercontinent resulted in crustal thickening during Ordovician collision-related magmatism and Devonian-Carboniferous regional metamorphism in the CEIM.
DOI: 10.6084/m9.figshare.16545644.v2
title: 4D volcanic geology of Hachijo-jima islet, Izu-Bonin arc

description: This study combines detailed geologic mapping, tephrochronology, U-Pb zircon dating, and published drill core data to evaluate the time transgressive 3-dimensional (thus 4-dimensional) structure and evolution of the two volcanoes on Hachijo-jima of the juvenile Izu-Bonin intra oceanic arc. The regional Ata-Torihama tephra (Ata-Th; 0.24 Ma) and Kikai-Tozurahara tephra (K-Tz; 0.095 Ma) from Kyushu are intercalated within the voluminous proximal volcanic products. The silicic tuff cover of some supra-subduction zone ophiolites, that formed in a nascent arc setting, may be ancient analogs of the regional tephra derived from the adjacent but mature volcanic arc. The volcanic succession comprises submarine volcanic basement, marine volcaniclastic rocks, and terrestrial tuff intercalated with tholeiitic basalt and the exotic calc-alkaline tephra layers. The undissected Hachijo-Fuji stratovolcano (tholeiitic basalt) overlies marine volcaniclastics abutting the northwestern paleo sea cliffs of the older dissected volcano, Mihara-yama. Newly-described folding and normal faulting of the marine and overlying terrestrial volcaniclastic rocks record NW-SE shortening that may be associated with the collision of the Izu-Bonin arc with the Honshu arc, analogous to the NNE-SSW shortening observed for the Troodos ophiolite. The proto Hachijo-jima volcano emerged above the sea &gt;0.24 Ma, and this date can be applied as a molecular biological calibration date for organisms on this island.
DOI: 10.6084/m9.figshare.16553048
title: Ordovician supra-subduction, oceanic and within-plate ocean island complexes in the Tekturmas ophiolite zone (Central Kazakhstan): age, geochemistry and tectonic implications

description: The Junggar-Balkhash region in the west of the Central Asian orogenic belt comprises Palaeozoic flysch, dismembered ophiolites, chert, basalt, and olistostrome within its accretionary wedges. The Tekturmas ophiolite zone in the north of the Junggar-Balkhash region hosts Ordovician to Early Silurian complexes, mostly formed with a convergent margin in front of the Baydaulet-Akbastau magmatic arc. The northern part of the Tekturmas zone comprises Middle to Late Ordovician (465–455 Ма) Bazarbai supra-subduction (SSZ) ophiolites, which were formed in the fore-arc settings. At the south of the Tekturmas zone Early Ordovician (~470 Ма) Tortaul SSZ ophiolites, Middle Ordovician Karamurun oceanic island basalts (OIB) and Middle to Late Ordovician Tekturmas deep water cherts are present. There are also concurrent Middle Ordovician (~460 Ma) high-temperature granulites, related to a partial melting of the subducted metasedimentary complexes. Since the second half of the Late Ordovician until the Early Silurian, the stratigraphic data constrain in front of the Baydaulet-Akbastau island arc the emergence of the Nura fore-arc trough. In the north of the Tekturmas zone, it is represented by the chert-tuffaceous Bazarbai Formation; southward, the zone can be interpreted as a concurrent accretionary wedge made up by the fragments of the Bazarbai and Tortaul ophiolites, Karamurun OIB basalts, and Tekturmas deep water cherts, accompanied by chaotic olistostrome. In the Early Silurian, growth of the accretionary wedge migrated to the south into the Uspenskу zone. We propose that while subduction was steadily directed underneath the Baydaulet-Akbastau island arc, the near-surface thrusting OIB and deep water cherts was also directed northward onto the fore-arc in the Late Ordovician to the earliest Silurian, whereas from the middle Llandovery it reversed southwards. In the end of the Palaeozoic to the Mesozoic, the Tekturmas ophiolite zone was offset into a number of segments by the sinistral strike-slip faults.
DOI: 10.6084/m9.figshare.16553048.v2
title: Ordovician supra-subduction, oceanic and within-plate ocean island complexes in the Tekturmas ophiolite zone (Central Kazakhstan): age, geochemistry and tectonic implications

description: The Junggar-Balkhash region in the west of the Central Asian orogenic belt comprises Palaeozoic flysch, dismembered ophiolites, chert, basalt, and olistostrome within its accretionary wedges. The Tekturmas ophiolite zone in the north of the Junggar-Balkhash region hosts Ordovician to Early Silurian complexes, mostly formed with a convergent margin in front of the Baydaulet-Akbastau magmatic arc. The northern part of the Tekturmas zone comprises Middle to Late Ordovician (465–455 Ма) Bazarbai supra-subduction (SSZ) ophiolites, which were formed in the fore-arc settings. At the south of the Tekturmas zone Early Ordovician (~470 Ма) Tortaul SSZ ophiolites, Middle Ordovician Karamurun oceanic island basalts (OIB) and Middle to Late Ordovician Tekturmas deep water cherts are present. There are also concurrent Middle Ordovician (~460 Ma) high-temperature granulites, related to a partial melting of the subducted metasedimentary complexes. Since the second half of the Late Ordovician until the Early Silurian, the stratigraphic data constrain in front of the Baydaulet-Akbastau island arc the emergence of the Nura fore-arc trough. In the north of the Tekturmas zone, it is represented by the chert-tuffaceous Bazarbai Formation; southward, the zone can be interpreted as a concurrent accretionary wedge made up by the fragments of the Bazarbai and Tortaul ophiolites, Karamurun OIB basalts, and Tekturmas deep water cherts, accompanied by chaotic olistostrome. In the Early Silurian, growth of the accretionary wedge migrated to the south into the Uspenskу zone. We propose that while subduction was steadily directed underneath the Baydaulet-Akbastau island arc, the near-surface thrusting OIB and deep water cherts was also directed northward onto the fore-arc in the Late Ordovician to the earliest Silurian, whereas from the middle Llandovery it reversed southwards. In the end of the Palaeozoic to the Mesozoic, the Tekturmas ophiolite zone was offset into a number of segments by the sinistral strike-slip faults.
DOI: 10.6084/m9.figshare.16571366.v1
title: Ordovician crustal thickening and syn-collisional magmatism of Iran: Gondwanan basement along the north of the Yazd Block (Central Iran)

description: This study investigates relicts of some granitic Gondwanan basement unexpectedly outcropping in the northwest of Central-East Iranian Microcontinent (CEIM) and incorporated into an ophiolitic mélange. Based on petrographical (e.g. high modal content of muscovite (~10 vol.%), absence of hornblende, inherited zircons (&gt;541 Ma)), geochemical (peraluminous and calc-alkaline S-type affinity, high silica, high ‘light rare earth element (LREE)/heavy rare earth element (HREE)’ ratios, negative Nb and Ti anomalies), and geochronological (magmatic zircon age ~448 Ma) results, it is an Ordovician anatectic granite formed from a sedimentary source during crustal thickening in a syn-collisional setting. It shows some signatures of metamorphic deformation (cataclastic fabric, quartz bulging recrystallization, and foliation) likely developed in the Devonian (~410 Ma). The U-Pb zircon ages from this granite are analogous to the other Ordovician collision-related magmatic events in the CEIM (Chahak to Airekan, Balvard). Our results confirm that Cadomian subduction and closure of the Proto-Tethys Ocean to the north of the Gondwana supercontinent resulted in crustal thickening during Ordovician collision-related magmatism and Devonian-Carboniferous regional metamorphism in the CEIM.
DOI: 10.6084/m9.figshare.16553048.v1
title: Ordovician supra-subduction, oceanic and within-plate ocean island complexes in the Tekturmas ophiolite zone (Central Kazakhstan): age, geochemistry and tectonic implications

description: The Junggar-Balkhash region in the west of the Central Asian orogenic belt comprises Palaeozoic flysch, dismembered ophiolites, chert, basalt, and olistostrome within its accretionary wedges. The Tekturmas ophiolite zone in the north of the Junggar-Balkhash region hosts Ordovician to Early Silurian complexes, mostly formed with a convergent margin in front of the Baydaulet-Akbastau magmatic arc. The northern part of the Tekturmas zone comprises Middle to Late Ordovician (465–455 Ма) Bazarbai supra-subduction (SSZ) ophiolites, which were formed in the fore-arc settings. At the south of the Tekturmas zone Early Ordovician (~470 Ма) Tortaul SSZ ophiolites, Middle Ordovician Karamurun oceanic island basalts (OIB) and Middle to Late Ordovician Tekturmas deep water cherts are present. There are also concurrent Middle Ordovician (~460 Ma) high-temperature granulites, related to a partial melting of the subducted metasedimentary complexes. Since the second half of the Late Ordovician until the Early Silurian, the stratigraphic data constrain in front of the Baydaulet-Akbastau island arc the emergence of the Nura fore-arc trough. In the north of the Tekturmas zone, it is represented by the chert-tuffaceous Bazarbai Formation; southward, the zone can be interpreted as a concurrent accretionary wedge made up by the fragments of the Bazarbai and Tortaul ophiolites, Karamurun OIB basalts, and Tekturmas deep water cherts, accompanied by chaotic olistostrome. In the Early Silurian, growth of the accretionary wedge migrated to the south into the Uspenskу zone. We propose that while subduction was steadily directed underneath the Baydaulet-Akbastau island arc, the near-surface thrusting OIB and deep water cherts was also directed northward onto the fore-arc in the Late Ordovician to the earliest Silurian, whereas from the middle Llandovery it reversed southwards. In the end of the Palaeozoic to the Mesozoic, the Tekturmas ophiolite zone was offset into a number of segments by the sinistral strike-slip faults.
DOI: 10.57745/cpztew/rmb1fl
title: Commercial acerola-based food supplements.pdf

description: Description of commercial acerola-based food supplements (label) - NMR stackplot
DOI: 10.57745/cpztew/jx3gmy
title: Commercial acerola-based food supplement - NMR spectra_D.S.product.zip

description: 1D 1H NMR spectra of commercial acerola-based food supplements
DOI: 10.57745/cpztew/n5sx50
title: Ascorbic acid Chemical shift pH dependence in acerola powder.pdf

description: Description and NMR stackplot of Ascorbic acid Chemical shift pH dependence in acerola powder
DOI: 10.57745/cpztew/mg8xqm
title: Ascorbic acid NMR and pH.zip

description: 1D 1H NMR spectra of 9 solutions of acerola reference powder with pH adjusted to 1.0, 1.5, 2.0, 2.5, 3.0, 3.5, 4.0, 4.5 and 5.0
DOI: 10.57745/cpztew/4vbsqg
title: Acerola powder .pdf

description: description of samples prepared from acerola powders for 1D 1H-NMR
DOI: 10.57745/cpztew/oavkvq
title: 8 NMR spectra from acerola powder solutions .zip

description: 1D 1H NMR spectra file of a selection of 8 samples prepared from acerola powders
DOI: 10.57745/cpztew/hxj6ow
title: NMR of Acerola juice concentrate .pdf

description: Description of samples of acerola juice concentrates for 1D 1H NMR. Stackplot. • (Ascorbic Acid area/Choline area) ratio
DOI: 10.57745/cpztew/lpjqdx
title: Acerola juice concentrate NMR spectra .zip

description: 1D 1H NMR spectra of a selection of 10 samples prepared from acerola concentrate juice.
DOI: 10.57745/cpztew/gymrsq
title: 1D and 2D NMR of acerola juice concentrate for annotation.pdf

description: Material and Method of the 1D 1H-NMR and 2D NMR spectra of acerola juice concentrate for annotation
DOI: 10.57745/cpztew/dcl1i8
title: Acerola juice concentrate 1D and 2D NMR experiments for annotation .zip

description: 1D NMR Stackplot; Annotation table; 1D 1H-NMR and 2D NMR spectra file description of acerola juice concentrate for annotation.
DOI: 10.5281/zenodo.7032251
title: MPS19 seismic hazard model of Italy results

description: <em>The MPS19 model is the result of the activities performed by the Seismic Hazard Center at INGV (Centro Pericolosità Sismica - CPS) in the framework of the 2015-2019 DPC-INGV B1 agreements. The documentation of the whole work is presented in Meletti et al. (2021). Details on the earthquake rupture forecasts are reported in Visini et al. (2021). Details on the ground motion models are reported in Lanzano et al. (2020).</em> <em>Data are free for the users, by reporting the following citation: <strong>Meletti C., Marzocchi W., D'Amico V., Lanzano G., Luzi L., Martinelli F., Pace B., Rovida A., Taroni M., Visini F. & the MPS19 Working Group, 2022. MPS19 seismic hazard model of Italy results. DOI: 10.5281/zenodo.7032251</strong></em> <em>In each file, the different sheets list the mean values and the values corresponding to 84th, 16th, 97.5th and 2.5th percentiles for the spectral acceleration, contained in the filename. Values are computed for 10 probabilities of exceedance in 50 years (as reported in the column name) and for rocky soil (class A of the Eurocode 8). Values represent the geometric mean of the horizontal components of the shaking. Values are computed on a regular grid 0.05 degrees spaced, covering the Italian territory.</em>
DOI: 10.5281/zenodo.7032250
title: MPS19 seismic hazard model of Italy results

description: <em>The MPS19 model is the result of the activities performed by the Seismic Hazard Center at INGV (Centro Pericolosità Sismica - CPS) in the framework of the 2015-2019 DPC-INGV B1 agreements. The documentation of the whole work is presented in Meletti et al. (2021). Details on the earthquake rupture forecasts are reported in Visini et al. (2021). Details on the ground motion models are reported in Lanzano et al. (2020).</em> <em>Data are free for the users, by reporting the following citation: <strong>Meletti C., Marzocchi W., D'Amico V., Lanzano G., Luzi L., Martinelli F., Pace B., Rovida A., Taroni M., Visini F. & the MPS19 Working Group, 2022. MPS19 seismic hazard model of Italy results. DOI: 10.5281/zenodo.7032251</strong></em> <em>In each file, the different sheets list the mean values and the values corresponding to 84th, 16th, 97.5th and 2.5th percentiles for the spectral acceleration, contained in the filename. Values are computed for 10 probabilities of exceedance in 50 years (as reported in the column name) and for rocky soil (class A of the Eurocode 8). Values represent the geometric mean of the horizontal components of the shaking. Values are computed on a regular grid 0.05 degrees spaced, covering the Italian territory.</em>