taxonID	type	format	identifier	references	title	description	created	creator	contributor	publisher	audience	source	license	rightsHolder	datasetID
03FD87F964540D028B2CF9C5FB473A27.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/13643847/files/figure.png	https://doi.org/10.5281/zenodo.13643847	Fig. 4. Scanning electron micrographs of skeletonized microfossils from the Lower–Middle Cambrian transition of the Esla Nappe, Cantabrian Mountains, Spain. A, B. Chancelloria sp. A; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. A. DGO 21129, longitudinal section. B. DGO 21130, lateral view. C–E. Chancelloria sp. B; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. C. (1+6) sclerite, DGO 21131, lateral views. D. (1+5) sclerite, DGO 21132, upper view. E. Incomplete (1+7) sclerite, DGO 21133, upper view. F. Parazhijnites cf. guizhouensis Qian and Yin, 1984; cambroclavid sclerite; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian; DGO 21134, oblique (F1) and lateral (F2) views. G–J. Torellella sp.; hyolithelminth tubes; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian. G. DGO 21135, lateral view. H. 21136, lateral view. I. DGO 21137, lateral view showing elliptic perforation (I1) and detail of the faint growth lines (squared area on I1; tilt adjust). J. DGO 21138, lateral (J1) and distal (J2) views. K. Phosphatic undefined tube; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian; DGO 21139, lateral view (K1) and detail of broken termination (K2). Scale bars 250 µm, except I2 and K2 for which are 50 µm.	Fig. 4. Scanning electron micrographs of skeletonized microfossils from the Lower–Middle Cambrian transition of the Esla Nappe, Cantabrian Mountains, Spain. A, B. Chancelloria sp. A; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. A. DGO 21129, longitudinal section. B. DGO 21130, lateral view. C–E. Chancelloria sp. B; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. C. (1+6) sclerite, DGO 21131, lateral views. D. (1+5) sclerite, DGO 21132, upper view. E. Incomplete (1+7) sclerite, DGO 21133, upper view. F. Parazhijnites cf. guizhouensis Qian and Yin, 1984; cambroclavid sclerite; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian; DGO 21134, oblique (F1) and lateral (F2) views. G–J. Torellella sp.; hyolithelminth tubes; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian. G. DGO 21135, lateral view. H. 21136, lateral view. I. DGO 21137, lateral view showing elliptic perforation (I1) and detail of the faint growth lines (squared area on I1; tilt adjust). J. DGO 21138, lateral (J1) and distal (J2) views. K. Phosphatic undefined tube; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian; DGO 21139, lateral view (K1) and detail of broken termination (K2). Scale bars 250 µm, except I2 and K2 for which are 50 µm.	2006-12-31	Clausen, Sébastien;Álvaro, J. Javier		Zenodo	biologists	Clausen, Sébastien;Álvaro, J. Javier			
03FD87F964540D028866FBBBFA3438F1.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/13643847/files/figure.png	https://doi.org/10.5281/zenodo.13643847	Fig. 4. Scanning electron micrographs of skeletonized microfossils from the Lower–Middle Cambrian transition of the Esla Nappe, Cantabrian Mountains, Spain. A, B. Chancelloria sp. A; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. A. DGO 21129, longitudinal section. B. DGO 21130, lateral view. C–E. Chancelloria sp. B; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. C. (1+6) sclerite, DGO 21131, lateral views. D. (1+5) sclerite, DGO 21132, upper view. E. Incomplete (1+7) sclerite, DGO 21133, upper view. F. Parazhijnites cf. guizhouensis Qian and Yin, 1984; cambroclavid sclerite; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian; DGO 21134, oblique (F1) and lateral (F2) views. G–J. Torellella sp.; hyolithelminth tubes; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian. G. DGO 21135, lateral view. H. 21136, lateral view. I. DGO 21137, lateral view showing elliptic perforation (I1) and detail of the faint growth lines (squared area on I1; tilt adjust). J. DGO 21138, lateral (J1) and distal (J2) views. K. Phosphatic undefined tube; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian; DGO 21139, lateral view (K1) and detail of broken termination (K2). Scale bars 250 µm, except I2 and K2 for which are 50 µm.	Fig. 4. Scanning electron micrographs of skeletonized microfossils from the Lower–Middle Cambrian transition of the Esla Nappe, Cantabrian Mountains, Spain. A, B. Chancelloria sp. A; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. A. DGO 21129, longitudinal section. B. DGO 21130, lateral view. C–E. Chancelloria sp. B; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. C. (1+6) sclerite, DGO 21131, lateral views. D. (1+5) sclerite, DGO 21132, upper view. E. Incomplete (1+7) sclerite, DGO 21133, upper view. F. Parazhijnites cf. guizhouensis Qian and Yin, 1984; cambroclavid sclerite; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian; DGO 21134, oblique (F1) and lateral (F2) views. G–J. Torellella sp.; hyolithelminth tubes; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian. G. DGO 21135, lateral view. H. 21136, lateral view. I. DGO 21137, lateral view showing elliptic perforation (I1) and detail of the faint growth lines (squared area on I1; tilt adjust). J. DGO 21138, lateral (J1) and distal (J2) views. K. Phosphatic undefined tube; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian; DGO 21139, lateral view (K1) and detail of broken termination (K2). Scale bars 250 µm, except I2 and K2 for which are 50 µm.	2006-12-31	Clausen, Sébastien;Álvaro, J. Javier		Zenodo	biologists	Clausen, Sébastien;Álvaro, J. Javier			
03FD87F964570D008B2CF894FD713D60.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/13643847/files/figure.png	https://doi.org/10.5281/zenodo.13643847	Fig. 4. Scanning electron micrographs of skeletonized microfossils from the Lower–Middle Cambrian transition of the Esla Nappe, Cantabrian Mountains, Spain. A, B. Chancelloria sp. A; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. A. DGO 21129, longitudinal section. B. DGO 21130, lateral view. C–E. Chancelloria sp. B; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. C. (1+6) sclerite, DGO 21131, lateral views. D. (1+5) sclerite, DGO 21132, upper view. E. Incomplete (1+7) sclerite, DGO 21133, upper view. F. Parazhijnites cf. guizhouensis Qian and Yin, 1984; cambroclavid sclerite; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian; DGO 21134, oblique (F1) and lateral (F2) views. G–J. Torellella sp.; hyolithelminth tubes; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian. G. DGO 21135, lateral view. H. 21136, lateral view. I. DGO 21137, lateral view showing elliptic perforation (I1) and detail of the faint growth lines (squared area on I1; tilt adjust). J. DGO 21138, lateral (J1) and distal (J2) views. K. Phosphatic undefined tube; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian; DGO 21139, lateral view (K1) and detail of broken termination (K2). Scale bars 250 µm, except I2 and K2 for which are 50 µm.	Fig. 4. Scanning electron micrographs of skeletonized microfossils from the Lower–Middle Cambrian transition of the Esla Nappe, Cantabrian Mountains, Spain. A, B. Chancelloria sp. A; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. A. DGO 21129, longitudinal section. B. DGO 21130, lateral view. C–E. Chancelloria sp. B; chancelloriid sclerites; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian. C. (1+6) sclerite, DGO 21131, lateral views. D. (1+5) sclerite, DGO 21132, upper view. E. Incomplete (1+7) sclerite, DGO 21133, upper view. F. Parazhijnites cf. guizhouensis Qian and Yin, 1984; cambroclavid sclerite; section Cr4, “Beleño” facies, upper member of the Láncara Formation, early Leonian; DGO 21134, oblique (F1) and lateral (F2) views. G–J. Torellella sp.; hyolithelminth tubes; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian. G. DGO 21135, lateral view. H. 21136, lateral view. I. DGO 21137, lateral view showing elliptic perforation (I1) and detail of the faint growth lines (squared area on I1; tilt adjust). J. DGO 21138, lateral (J1) and distal (J2) views. K. Phosphatic undefined tube; section Cr4, ooid/bioclastic limestone, lower member of the Láncara Formation, latest Early Cambrian; DGO 21139, lateral view (K1) and detail of broken termination (K2). Scale bars 250 µm, except I2 and K2 for which are 50 µm.	2006-12-31	Clausen, Sébastien;Álvaro, J. Javier		Zenodo	biologists	Clausen, Sébastien;Álvaro, J. Javier			
03FD87F9645B0D0A8B2CF913FDF43BFE.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/13643849/files/figure.png	https://doi.org/10.5281/zenodo.13643849	Fig. 7. Thin sections on backscattered SEM of Cantabria labyrinthica gen. et sp. nov. (apatite is white and secondary silica is grey), enigmatic fossil, possible external sclerite of lobopodian affinity from the “Beleño” facies (section Cr4), upper member of the Láncara Formation, early Leonian.A, B, D. Cross−sections with chaotic meshwork microstructure of the sclerites (DGO 21152, DGO 21153, and DGO 21156 respectively) with tubes centripetally increasing in size; note their whole perforated pattern of outer wall. C, E. Transverse sections close to the basal (C, DGO 21154) and the upper side (E, DGO 21155) with subcircular to irregular sections of individual tubes. Overall view (E1) and enlargements (E2, E3) showing the tube walls built of two distinct apatitic layers; see a synapticule−like tube (arrowed) connecting two transverse tubes (E3). Scale bars 250 µm. +	Fig. 7. Thin sections on backscattered SEM of Cantabria labyrinthica gen. et sp. nov. (apatite is white and secondary silica is grey), enigmatic fossil, possible external sclerite of lobopodian affinity from the “Beleño” facies (section Cr4), upper member of the Láncara Formation, early Leonian.A, B, D. Cross−sections with chaotic meshwork microstructure of the sclerites (DGO 21152, DGO 21153, and DGO 21156 respectively) with tubes centripetally increasing in size; note their whole perforated pattern of outer wall. C, E. Transverse sections close to the basal (C, DGO 21154) and the upper side (E, DGO 21155) with subcircular to irregular sections of individual tubes. Overall view (E1) and enlargements (E2, E3) showing the tube walls built of two distinct apatitic layers; see a synapticule−like tube (arrowed) connecting two transverse tubes (E3). Scale bars 250 µm. +	2006-12-31	Clausen, Sébastien;Álvaro, J. Javier		Zenodo	biologists	Clausen, Sébastien;Álvaro, J. Javier			
03FD87F9645B0D0A8B2CF913FDF43BFE.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/13643851/files/figure.png	https://doi.org/10.5281/zenodo.13643851	Fig. 8. Sketch of Cantabria labyrinthica gen. et sp. nov.“ (enigmatic fossil, possible external sclerite of lobopodian affinity) illustrating the cross sections of the previous figure.	Fig. 8. Sketch of Cantabria labyrinthica gen. et sp. nov.“ (enigmatic fossil, possible external sclerite of lobopodian affinity) illustrating the cross sections of the previous figure.	2006-12-31	Clausen, Sébastien;Álvaro, J. Javier		Zenodo	biologists	Clausen, Sébastien;Álvaro, J. Javier			
03FD87F9645B0D0A8B2CF913FDF43BFE.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/13643843/files/figure.png	https://doi.org/10.5281/zenodo.13643843	Fig. 1. A. Pre−Hercynian outcrops of the Iberian Peninsula (stippled) and setting of the Esla Nappe in the Cantabrian Zone (grey area). B. Geologic map of the Esla nappe and stratigraphic sections sampled in this work (Cr1–4 and V1; after Truyols et al. 1990; Aramburu et al. 1992; Álvaro et al. 2000b).	Fig. 1. A. Pre−Hercynian outcrops of the Iberian Peninsula (stippled) and setting of the Esla Nappe in the Cantabrian Zone (grey area). B. Geologic map of the Esla nappe and stratigraphic sections sampled in this work (Cr1–4 and V1; after Truyols et al. 1990; Aramburu et al. 1992; Álvaro et al. 2000b).	2006-12-31	Clausen, Sébastien;Álvaro, J. Javier		Zenodo	biologists	Clausen, Sébastien;Álvaro, J. Javier			
03FD87F9645B0D0A8B2CF913FDF43BFE.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/13643845/files/figure.png	https://doi.org/10.5281/zenodo.13643845	Fig. 2. Stratigraphic units of the Lower–Middle Cambrian boundary interval in the Esla nappe, and setting of the fossils described in the text.	Fig. 2. Stratigraphic units of the Lower–Middle Cambrian boundary interval in the Esla nappe, and setting of the fossils described in the text.	2006-12-31	Clausen, Sébastien;Álvaro, J. Javier		Zenodo	biologists	Clausen, Sébastien;Álvaro, J. Javier			
