cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.rb9f3k
title: Occurrence Download

description: A dataset containing 3474779 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((4.59287 51.79737,5.17451 51.79737,5.17451 52.0326,4.59287 52.0326,4.59287 51.79737))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "Year 2015-2025"
 ]
}

 The dataset includes 3474779 records from 51 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0044259-251120083545085/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.13130/rd_unimi/epaoaq/nhy2ob
title: Giugno_1881_Pagina_028.jpg

description: Bulletin of 1881/06/07
DOI: 10.13130/rd_unimi/epaoaq/gi00jw
title: Giugno_1881_Pagina_029.jpg

description: Bulletin of 1881/06/08
DOI: 10.13130/rd_unimi/epaoaq/vyj5zy
title: Giugno_1881_Pagina_030.jpg

description: Bulletin of 1881/06/08
DOI: 10.13130/rd_unimi/epaoaq/xd4ivq
title: Giugno_1881_Pagina_031.jpg

description: Bulletin of 1881/06/08
DOI: 10.13130/rd_unimi/epaoaq/xv8jwn
title: Giugno_1881_Pagina_032.jpg

description: Bulletin of 1881/06/08
DOI: 10.13130/rd_unimi/epaoaq/hbietp
title: Giugno_1881_Pagina_033.jpg

description: Bulletin of 1881/06/09
DOI: 10.13130/rd_unimi/epaoaq/auyl7u
title: Giugno_1881_Pagina_034.jpg

description: Bulletin of 1881/06/09
DOI: 10.13130/rd_unimi/epaoaq/dplc8y
title: Giugno_1881_Pagina_035.jpg

description: Bulletin of 1881/06/09
DOI: 10.13130/rd_unimi/epaoaq/une6iu
title: Giugno_1881_Pagina_036.jpg

description: Bulletin of 1881/06/09
DOI: 10.13130/rd_unimi/epaoaq/wyvgdx
title: Giugno_1881_Pagina_037.jpg

description: Bulletin of 1881/06/10
DOI: 10.13130/rd_unimi/epaoaq/sulddl
title: Giugno_1881_Pagina_038.jpg

description: Bulletin of 1881/06/10
DOI: 10.13130/rd_unimi/epaoaq/cu2lms
title: Giugno_1881_Pagina_039.jpg

description: Bulletin of 1881/06/10
DOI: 10.13130/rd_unimi/epaoaq/ruxbk8
title: Giugno_1881_Pagina_040.jpg

description: Bulletin of 1881/06/10
DOI: 10.13130/rd_unimi/epaoaq/eplwtf
title: Giugno_1881_Pagina_041.jpg

description: Bulletin of 1881/06/11
DOI: 10.13130/rd_unimi/epaoaq/rzzyye
title: Giugno_1881_Pagina_042.jpg

description: Bulletin of 1881/06/11
DOI: 10.13130/rd_unimi/epaoaq/gpyti6
title: Giugno_1881_Pagina_043.jpg

description: Bulletin of 1881/06/11
DOI: 10.13130/rd_unimi/epaoaq/9u5kjo
title: Giugno_1881_Pagina_044.jpg

description: Bulletin of 1881/06/11
DOI: 10.13130/rd_unimi/epaoaq/sdmdhc
title: Giugno_1881_Pagina_045.jpg

description: Bulletin of 1881/06/12
DOI: 10.13130/rd_unimi/epaoaq/72vkjr
title: Giugno_1881_Pagina_046.jpg

description: Bulletin of 1881/06/12
DOI: 10.13130/rd_unimi/epaoaq/wbslz2
title: Giugno_1881_Pagina_047.jpg

description: Bulletin of 1881/06/12
DOI: 10.6084/m9.figshare.30847388
title: Data set on stability studies on antibacterial activity of cell free supernatant and crude bacteriocin of lactic acid bacteria isolates from Nigerian fermented foods

description: The increasing need for natural and safe food preservatives has triggered interest in bacteriocins (antimicrobial peptides) produced by lactic acid bacteria (LAB) as viable alternatives to chemical preservatives. This study aimed to optimize bacteriocin production from LAB isolated from Nigerian fermented foods and to evaluate its effectiveness in extending the shelf life of selected fruit juices. A total of 33 LAB strains were isolated from Nigerian local fermented foods (iru, fufu, and ogi) using MRS agar, screened for antibacterial activity against selected foodborne pathogens, and characterized using 16S rRNA sequencing. Five LAB strains were identified: <i>Lactobacillus plantarum</i> (PV937062, PV937063, PV937065), <i>Lactobacillus paracasei</i> (PV937064), and <i>Lactobacillus acidophilus</i> (PV937061). The agar well diffusion method was used to optimize the effects of culture age, pH, temperature, organic solvents, ultraviolet radiation, protease treatment, and storage conditions on the bacteriocin activity. This study demonstrated that optimized bacteriocins by LAB from Nigerian fermented food has the potential to be an effective food preservative by extending the shelf life of fruit juices as a safe and environmentally friendly alternative to synthetic preservatives to enhance food safety and quality.
DOI: 10.13130/rd_unimi/epaoaq/85htdo
title: Giugno_1881_Pagina_048.jpg

description: Bulletin of 1881/06/12
DOI: 10.6084/m9.figshare.30847388.v1
title: Data set on stability studies on antibacterial activity of cell free supernatant and crude bacteriocin of lactic acid bacteria isolates from Nigerian fermented foods

description: Antibacterial activity of cell free supernatants and crude bacteriocin from lactic acid bacteria
DOI: 10.6084/m9.figshare.30847388.v2
title: Data set on stability studies on antibacterial activity of cell free supernatant and crude bacteriocin of lactic acid bacteria isolates from Nigerian fermented foods

description: The increasing need for natural and safe food preservatives has triggered interest in bacteriocins (antimicrobial peptides) produced by lactic acid bacteria (LAB) as viable alternatives to chemical preservatives. This study aimed to optimize bacteriocin production from LAB isolated from Nigerian fermented foods and to evaluate its effectiveness in extending the shelf life of selected fruit juices. A total of 33 LAB strains were isolated from Nigerian local fermented foods (iru, fufu, and ogi) using MRS agar, screened for antibacterial activity against selected foodborne pathogens, and characterized using 16S rRNA sequencing. Five LAB strains were identified: <i>Lactobacillus plantarum</i> (PV937062, PV937063, PV937065), <i>Lactobacillus paracasei</i> (PV937064), and <i>Lactobacillus acidophilus</i> (PV937061). The agar well diffusion method was used to optimize the effects of culture age, pH, temperature, organic solvents, ultraviolet radiation, protease treatment, and storage conditions on the bacteriocin activity. This study demonstrated that optimized bacteriocins by LAB from Nigerian fermented food has the potential to be an effective food preservative by extending the shelf life of fruit juices as a safe and environmentally friendly alternative to synthetic preservatives to enhance food safety and quality.
DOI: 10.13130/rd_unimi/epaoaq/v4v5au
title: Giugno_1881_Pagina_049.jpg

description: Bulletin of 1881/06/13
DOI: 10.13130/rd_unimi/epaoaq/ecz8ut
title: Giugno_1881_Pagina_050.jpg

description: Bulletin of 1881/06/13
DOI: 10.13130/rd_unimi/epaoaq/gqmayg
title: Giugno_1881_Pagina_051.jpg

description: Bulletin of 1881/06/13
DOI: 10.13130/rd_unimi/epaoaq/vcbeok
title: Giugno_1881_Pagina_052.jpg

description: Bulletin of 1881/06/13
DOI: 10.13130/rd_unimi/epaoaq/lhx5sl
title: Giugno_1881_Pagina_053.jpg

description: Bulletin of 1881/06/14
DOI: 10.13130/rd_unimi/epaoaq/c00otn
title: Giugno_1881_Pagina_054.jpg

description: Bulletin of 1881/06/14
DOI: 10.13130/rd_unimi/epaoaq/gyicvd
title: Giugno_1881_Pagina_055.jpg

description: Bulletin of 1881/06/14
DOI: 10.13130/rd_unimi/epaoaq/iwgztq
title: Giugno_1881_Pagina_056.jpg

description: Bulletin of 1881/06/14
DOI: 10.13130/rd_unimi/epaoaq/850fay
title: Giugno_1881_Pagina_057.jpg

description: Bulletin of 1881/06/15
DOI: 10.13130/rd_unimi/epaoaq/mn1kv8
title: Giugno_1881_Pagina_058.jpg

description: Bulletin of 1881/06/15
DOI: 10.13130/rd_unimi/epaoaq/jta7bq
title: Giugno_1881_Pagina_059.jpg

description: Bulletin of 1881/06/15
DOI: 10.13130/rd_unimi/epaoaq/0u3enw
title: Giugno_1881_Pagina_060.jpg

description: Bulletin of 1881/06/15
DOI: 10.13130/rd_unimi/epaoaq/fvfazm
title: Giugno_1881_Pagina_061.jpg

description: Bulletin of 1881/06/16
DOI: 10.13130/rd_unimi/epaoaq/ydp8xm
title: Giugno_1881_Pagina_062.jpg

description: Bulletin of 1881/06/16
DOI: 10.13130/rd_unimi/epaoaq/ommivy
title: Giugno_1881_Pagina_063.jpg

description: Bulletin of 1881/06/16
DOI: 10.13130/rd_unimi/epaoaq/ppl0qe
title: Giugno_1881_Pagina_064.jpg

description: Bulletin of 1881/06/16
DOI: 10.13130/rd_unimi/epaoaq/gtzm0m
title: Giugno_1881_Pagina_065.jpg

description: Bulletin of 1881/06/17
DOI: 10.13130/rd_unimi/epaoaq/a56mpl
title: Giugno_1881_Pagina_066.jpg

description: Bulletin of 1881/06/17
DOI: 10.13130/rd_unimi/epaoaq/0oymgk
title: Giugno_1881_Pagina_067.jpg

description: Bulletin of 1881/06/17
DOI: 10.13130/rd_unimi/epaoaq/lywpr7
title: Giugno_1881_Pagina_068.jpg

description: Bulletin of 1881/06/17
DOI: 10.13130/rd_unimi/epaoaq/0un2y6
title: Giugno_1881_Pagina_069.jpg

description: Bulletin of 1881/06/18
DOI: 10.13130/rd_unimi/epaoaq/bj3rgr
title: Giugno_1881_Pagina_070.jpg

description: Bulletin of 1881/06/18
DOI: 10.6084/m9.figshare.30362786
title: The ~1.9 Ga syn-collisional granitic magmatism in the Sushui Complex: new evidence for the late Paleoproterozoic tectonic evolution of the southern North China Craton

description: The late Paleoproterozoic tectonic evolution of the southern North China Craton (NCC) remains controversial, largely due to its complex structural position and ambiguous magmatic-metamorphic records. This study presents an integrated petrology, whole-rock geochemistry, and in-situ zircon U-Pb-Hf isotopic investigation of newly identified monzogranites from the Sushui Complex. LA-ICP-MS zircon U-Pb dating yields emplacement ages of 1904 ± 37 Ma and 1895 ± 37 Ma. Geochemically, these rocks are high-K calc-alkaline I-type granites characterized by elevated SiO<sub>2</sub> and K<sub>2</sub>O/Na<sub>2</sub>O ratios, low A/CNK and Fe<sub>2</sub>O<sub>3</sub><sup>T</sup>/MgO values, and zircon saturation temperatures ranging from 635°C to 842°C. They exhibit a moderately fractionated REE patterns ((La/Yb)<sub>N</sub> = 1.76–35.92) with significant negative Eu anomalies (δEu = 0.42–0.71). Zircons exhibit uniformly negative ε<sub>Hf</sub>(<i>t</i>) values (−6.8 to −4.7) and Neo- to Mesoarchean two-stage Hf model ages (T<sub>DM2</sub> = 2.82–2.96 Ga). These geochemical and isotopic features, combined with regional correlations, indicate that the monzogranite rocks were likely originated from partial melting of pre-existing Neoarchean TTGs, and formed in a syn-collisional setting. Combined with regional magmatic, metamorphic, and sedimentary evidence, we propose that the southern NCC underwent a tectonic transition from compressional collision to extension between 2.1 and 1.8 Ga. We further interpret the ca. 1.94–1.90 Ga tectono-magmatic events as recording the assembly of the Columbia supercontinent, and the ca. 1.80–1.70 Ga extensional activities as corresponding to its subsequent break-up.
DOI: 10.6084/m9.figshare.30362786.v1
title: The ~1.9 Ga syn-collisional granitic magmatism in the Sushui Complex: new evidence for the late Paleoproterozoic tectonic evolution of the southern North China Craton

description: The late Paleoproterozoic tectonic evolution of the southern North China Craton (NCC) remains controversial, largely due to its complex structural position and ambiguous magmatic-metamorphic records. This study presents an integrated petrology, whole-rock geochemistry, and in-situ zircon U-Pb-Hf isotopic investigation of newly identified monzogranites from the Sushui Complex. LA-ICP-MS zircon U-Pb dating yields emplacement ages of 1904 ± 37 Ma and 1895 ± 37 Ma. Geochemically, these rocks are high-K calc-alkaline I-type granites characterized by elevated SiO<sub>2</sub> and K<sub>2</sub>O/Na<sub>2</sub>O ratios, low A/CNK and Fe<sub>2</sub>O<sub>3</sub><sup>T</sup>/MgO values, and zircon saturation temperatures ranging from 635°C to 842°C. They exhibit a moderately fractionated REE patterns ((La/Yb)<sub>N</sub> = 1.76–35.92) with significant negative Eu anomalies (δEu = 0.42–0.71). Zircons exhibit uniformly negative ε<sub>Hf</sub>(<i>t</i>) values (−6.8 to −4.7) and Neo- to Mesoarchean two-stage Hf model ages (T<sub>DM2</sub> = 2.82–2.96 Ga). These geochemical and isotopic features, combined with regional correlations, indicate that the monzogranite rocks were likely originated from partial melting of pre-existing Neoarchean TTGs, and formed in a syn-collisional setting. Combined with regional magmatic, metamorphic, and sedimentary evidence, we propose that the southern NCC underwent a tectonic transition from compressional collision to extension between 2.1 and 1.8 Ga. We further interpret the ca. 1.94–1.90 Ga tectono-magmatic events as recording the assembly of the Columbia supercontinent, and the ca. 1.80–1.70 Ga extensional activities as corresponding to its subsequent break-up.
DOI: 10.13130/rd_unimi/epaoaq/1m5su7
title: Giugno_1881_Pagina_071.jpg

description: Bulletin of 1881/06/18
DOI: 10.6084/m9.figshare.30231303
title: Ophiolitic metamafic remnants of Palaeoproterozoic oceanic crust from the Cláudio shear zone, Southern São Francisco Craton (Brazil)

description: Early evidence of plate tectonics as a global phenomenon can be provided by Palaeoproterozoic ophiolites. Metamafic rocks preserved within the Southern São Francisco Craton (Brazil) along the Cláudio shear zone (suture zone) are regarded as part of the dismembered Cláudio meta-ophiolite. Here, we investigate the petrology and tectono-magmatic setting of these metamafites using petrography, whole-rock geochemistry, and mineral chemistry. Geochronological data and geodynamic implications were explored using Sm-Nd and U-Pb methods. We found that their protoliths (gabbro and basalt) are tholeiitic and sub-alkaline with an E-MORB signature, suggesting that they were remnants of oceanic crust. Metagabbro preserves igneous relics and prograde assemblages from very low- to medium-grade metamorphism. Metabasalts showed an assemblage of amphibolite facies. The 2276 Ma whole-rock Sm-Nd T<sub>DM</sub> model age and the 2050 Ma U-Pb age of metamorphic zircons indicate a Palaeoproterozoic evolution of the palaeo-oceanic basin. It was closed owing to NW-dipping subduction, followed by continental collision involving the Divinópolis and Campo Belo/Bonfim metamorphic complexes. Our results support previous studies that suggest a possible connection between São Francisco-Congo and North China/Yangtze cratons during the formation of the Columbia (Nuna) supercontinent. Furthermore, this study provides additional evidence supporting that modern-style plate tectonics operated during the Palaeoproterozoic.
DOI: 10.6084/m9.figshare.30231303.v1
title: Ophiolitic metamafic remnants of Palaeoproterozoic oceanic crust from the Cláudio shear zone, Southern São Francisco Craton (Brazil)

description: Early evidence of plate tectonics as a global phenomenon can be provided by Palaeoproterozoic ophiolites. Metamafic rocks preserved within the Southern São Francisco Craton (Brazil) along the Cláudio shear zone (suture zone) are regarded as part of the dismembered Cláudio meta-ophiolite. Here, we investigate the petrology and tectono-magmatic setting of these metamafites using petrography, whole-rock geochemistry, and mineral chemistry. Geochronological data and geodynamic implications were explored using Sm-Nd and U-Pb methods. We found that their protoliths (gabbro and basalt) are tholeiitic and sub-alkaline with an E-MORB signature, suggesting that they were remnants of oceanic crust. Metagabbro preserves igneous relics and prograde assemblages from very low- to medium-grade metamorphism. Metabasalts showed an assemblage of amphibolite facies. The 2276 Ma whole-rock Sm-Nd T<sub>DM</sub> model age and the 2050 Ma U-Pb age of metamorphic zircons indicate a Palaeoproterozoic evolution of the palaeo-oceanic basin. It was closed owing to NW-dipping subduction, followed by continental collision involving the Divinópolis and Campo Belo/Bonfim metamorphic complexes. Our results support previous studies that suggest a possible connection between São Francisco-Congo and North China/Yangtze cratons during the formation of the Columbia (Nuna) supercontinent. Furthermore, this study provides additional evidence supporting that modern-style plate tectonics operated during the Palaeoproterozoic.
DOI: 10.13130/rd_unimi/epaoaq/995hpt
title: Giugno_1881_Pagina_072.jpg

description: Bulletin of 1881/06/18
DOI: 10.6084/m9.figshare.30102833
title: Late Carboniferous to Early Permian granitoids from central Inner Mongolia, north China: petrogenesis and tectonic implications

description: Traditional models suggest that the final closure of the Paleo-Asian Ocean (PAO) occurred during the Late Permian to Triassic. However, the timing of the closure remains a topic of considerable debate. The widespread distribution of A-type granites dating from the Carboniferous to Permian periods indicates that closure may have occurred earlier, potentially as far back as the Late Carboniferous to Early Permian or even the Late Devonian. The granitoids with ages from the Late Carboniferous to Early Permian in northeastern Erenhot, within the Xing’an-Mongolian Orogenic Belt (XMOB), offer insightful perspectives on the complicated tectonic history related to the eventual closure of the PAO. By studying zircon U-Pb ages, Hf isotopic composition, and whole-rock geochemical composition of granitoids from the Zhunsujihua Granitic Belt (ZGB) and Baolage Granitic Belt (BGB) in northeastern Erenhot, we aim to gain a better understanding of their petrogenesis and tectonic settings while also constraining the closure time of the PAO. Zircon U-Pb ages of the ZGB and BGB granitoids span from 288 to 317 Ma and from 275 to 295 Ma, respectively. These granitoids have compositional ranges of 70.16–78.04 wt% SiO<sub>2</sub>, 3.73–5.02 wt% K<sub>2</sub>O, and 10.48–15.65 wt% Al<sub>2</sub>O<sub>3</sub>, and show light rare earth element (LREE) enrichment and negative Eu anomalies. The ZGB alkali-feldspar granite exhibits adakitic characteristics, whereas other ZGB granitoids show I-type features. The BGB granitoids display A-type signatures. Zircon ε<sub>Hf</sub>(t) values vary from + 10.05 to + 15.48, with young two-stage Hf model ages (T<sub>DM2</sub>) spanning from 332 to 656 Ma, suggesting that both the ZGB and BGB granitoids have originated from partial melting of juvenile crustal materials. These findings suggest that the granitoids formed during the transition from subduction to post-collisional extension, which implies that the PAO in the northeastern region of Erenhot had closed at the latest by the Early Permian.
DOI: 10.6084/m9.figshare.30102833.v2
title: Late Carboniferous to Early Permian granitoids from central Inner Mongolia, north China: petrogenesis and tectonic implications

description: Traditional models suggest that the final closure of the Paleo-Asian Ocean (PAO) occurred during the Late Permian to Triassic. However, the timing of the closure remains a topic of considerable debate. The widespread distribution of A-type granites dating from the Carboniferous to Permian periods indicates that closure may have occurred earlier, potentially as far back as the Late Carboniferous to Early Permian or even the Late Devonian. The granitoids with ages from the Late Carboniferous to Early Permian in northeastern Erenhot, within the Xing’an-Mongolian Orogenic Belt (XMOB), offer insightful perspectives on the complicated tectonic history related to the eventual closure of the PAO. By studying zircon U-Pb ages, Hf isotopic composition, and whole-rock geochemical composition of granitoids from the Zhunsujihua Granitic Belt (ZGB) and Baolage Granitic Belt (BGB) in northeastern Erenhot, we aim to gain a better understanding of their petrogenesis and tectonic settings while also constraining the closure time of the PAO. Zircon U-Pb ages of the ZGB and BGB granitoids span from 288 to 317 Ma and from 275 to 295 Ma, respectively. These granitoids have compositional ranges of 70.16–78.04 wt% SiO<sub>2</sub>, 3.73–5.02 wt% K<sub>2</sub>O, and 10.48–15.65 wt% Al<sub>2</sub>O<sub>3</sub>, and show light rare earth element (LREE) enrichment and negative Eu anomalies. The ZGB alkali-feldspar granite exhibits adakitic characteristics, whereas other ZGB granitoids show I-type features. The BGB granitoids display A-type signatures. Zircon ε<sub>Hf</sub>(t) values vary from + 10.05 to + 15.48, with young two-stage Hf model ages (T<sub>DM2</sub>) spanning from 332 to 656 Ma, suggesting that both the ZGB and BGB granitoids have originated from partial melting of juvenile crustal materials. These findings suggest that the granitoids formed during the transition from subduction to post-collisional extension, which implies that the PAO in the northeastern region of Erenhot had closed at the latest by the Early Permian.
DOI: 10.13130/rd_unimi/epaoaq/ditjf7
title: Giugno_1881_Pagina_073.jpg

description: Bulletin of 1881/06/19
DOI: 10.6084/m9.figshare.30102833.v1
title: Late carboniferous to early Permian granitoids from central Inner Mongolia, north China: petrogenesis and tectonic implications

description: Traditional models suggest that the final closure of the Paleo-Asian Ocean (PAO) occurred during the Late Permian to Triassic. However, the timing of the closure remains a topic of considerable debate. The widespread distribution of A-type granites dating from the Carboniferous to Permian periods indicates that closure may have occurred earlier, potentially as far back as the Late Carboniferous to Early Permian or even the Late Devonian. The granitoids with ages from the Late Carboniferous to Early Permian in northeastern Erenhot, within the Xing’an-Mongolian Orogenic Belt (XMOB), offer insightful perspectives on the complicated tectonic history related to the eventual closure of the PAO. By studying zircon U-Pb ages, Hf isotopic composition, and whole-rock geochemical composition of granitoids from the Zhunsujihua Granitic Belt (ZGB) and Baolage Granitic Belt (BGB) in northeastern Erenhot, we aim to gain a better understanding of their petrogenesis and tectonic settings while also constraining the closure time of the PAO. Zircon U-Pb ages of the ZGB and BGB granitoids span from 288 to 317 Ma and from 275 to 295 Ma, respectively. These granitoids have compositional ranges of 70.16–78.04 wt% SiO<sub>2</sub>, 3.73–5.02 wt% K<sub>2</sub>O, and 10.48–15.65 wt% Al<sub>2</sub>O<sub>3</sub>, and show light rare earth element (LREE) enrichment and negative Eu anomalies. The ZGB alkali-feldspar granite exhibits adakitic characteristics, whereas other ZGB granitoids show I-type features. The BGB granitoids display A-type signatures. Zircon ε<sub>Hf</sub>(t) values vary from + 10.05 to + 15.48, with young two-stage Hf model ages (T<sub>DM2</sub>) spanning from 332 to 656 Ma, suggesting that both the ZGB and BGB granitoids have originated from partial melting of juvenile crustal materials. These findings suggest that the granitoids formed during the transition from subduction to post-collisional extension, which implies that the PAO in the northeastern region of Erenhot had closed at the latest by the Early Permian.
DOI: 10.13130/rd_unimi/epaoaq/d1m81l
title: Giugno_1881_Pagina_074.jpg

description: Bulletin of 1881/06/19
DOI: 10.15468/dl.mfcbdt
title: Occurrence Download

description: A dataset containing 696 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Melursus ursinus",
 "HasCoordinate is TRUE"
 ]
}

 The dataset includes 696 records from 22 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0044331-251120083545085/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.