Automated Author ProfileVizcaïno, Daniel
Vizcaïno, Daniel
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 1.0 (sum of 3 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
This dataset contains the digitized treatments in Plazi based on the original journal article Roux, Michel, Martinez, Alain, Vizcaïno, Daniel (2021): A diverse crinoid fauna (Echinodermata, Crinoidea) from the Lower Eocene of the Gulf of Languedoc (Corbières, Aude, southern France). Zootaxa 4963 (2): 201-242, DOI: https://doi.org/10.11646/zootaxa.4963.2.1
Authors
- Roux, Michel ;
- Martinez, Alain ;
- Vizcaïno, Daniel
The distribution of all known Cambrian echinoderm taxa, encompassing both articulated specimens and taxonomically diagnostic isolated ossicles, is documented for the first time. The database described by 2011 comprises 188 species recorded from 65 formations from around the world. Formations that have yielded articulated echinoderms are unequally distributed in space and time. Only Laurentia and West Gondwana provide reasonably complete records at the resolution of Stage. The review of the biogeographical distributions of the eight major echinoderm clades shows that faunas from Laurentia and Northeast Gondwana (China and Korea) are distinct from those of West Gondwana and Southeast Gondwana (Australia); other regions are too poorly sampled to make firm palaeobiogeographical statements. Analysis of alpha diversity (species per formation) shows that diversity rose initially to Cambrian Stage 5, declined into Guzhangian and Paibian before returning to Stage 5 levels by the end of the Cambrian. This pattern is replicated in Laurentia and West Gondwana. We show that taxonomically diagnostic ossicles found in isolation typically occur significantly earlier than the first articulated specimens of the same taxa and provide important information on the first occurrence and palaeobiogeographical distribution of key taxa, and of the phylum as a whole.
Authors
- Zamora, Samuel ;
- Lefebvre, Bertrand ;
- J. Javier Álvaro ;
- Clausen, Sébastien ;
- Elicki, Olaf ;
- Oldrich Fatka ;
- Jell, Peter ;
- Kouchinsky, Artem ;
- Jih-Pai Lin ;
- Nardin, Elise ;
- Parsley, Ronald ;
- Rozhnov, Sergei ;
- Sprinkle, James ;
- Sumrall, Colin D. ;
- Vizcaïno, Daniel ;
- Smith, Andrew B.
The distribution of all known Cambrian echinoderm taxa, encompassing both articulated specimens and taxonomically diagnostic isolated ossicles, is documented for the first time. The database described by 2011 comprises 188 species recorded from 65 formations from around the world. Formations that have yielded articulated echinoderms are unequally distributed in space and time. Only Laurentia and West Gondwana provide reasonably complete records at the resolution of Stage. The review of the biogeographical distributions of the eight major echinoderm clades shows that faunas from Laurentia and Northeast Gondwana (China and Korea) are distinct from those of West Gondwana and Southeast Gondwana (Australia); other regions are too poorly sampled to make firm palaeobiogeographical statements. Analysis of alpha diversity (species per formation) shows that diversity rose initially to Cambrian Stage 5, declined into Guzhangian and Paibian before returning to Stage 5 levels by the end of the Cambrian. This pattern is replicated in Laurentia and West Gondwana. We show that taxonomically diagnostic ossicles found in isolation typically occur significantly earlier than the first articulated specimens of the same taxa and provide important information on the first occurrence and palaeobiogeographical distribution of key taxa, and of the phylum as a whole.
Authors
- Zamora, Samuel ;
- Lefebvre, Bertrand ;
- J. Javier Álvaro ;
- Clausen, Sébastien ;
- Elicki, Olaf ;
- Oldrich Fatka ;
- Jell, Peter ;
- Kouchinsky, Artem ;
- Jih-Pai Lin ;
- Nardin, Elise ;
- Parsley, Ronald ;
- Rozhnov, Sergei ;
- Sprinkle, James ;
- Sumrall, Colin D. ;
- Vizcaïno, Daniel ;
- Smith, Andrew B.