Fig. 24 in The paleoecology and taphonomy of a Santonian-Campanian (Upper Cretaceous) dinosaur-bearing vertebrate locality from Bulgaria: a window into an underexplored part of the Late Cretaceous European

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Main Authors: Nikolov, Vladimir, Pavlishina, Polina, Dochev, Docho, Brusatte, Stephen L.
Format: Recurso digital
Published: Zenodo 2025
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author Nikolov, Vladimir
Pavlishina, Polina
Dochev, Docho
Brusatte, Stephen L.
author_facet Nikolov, Vladimir
Pavlishina, Polina
Dochev, Docho
Brusatte, Stephen L.
contents Fig. 24 Osteohistology of titanosaur bones in cross-polarized light. a Secondary osteons and Wedl tunnels in the outermost cortex of NMNHS FR17. The dotted line traces the bone surfaces. b Partially recrystallized bone tissue in perimedullary developed bone trabeculae in NMNHS FR17 (λ-filter is used). c, d Numerous secondary osteons (c) and Haversian bone (d) in the outermost cortex of NMNHS FR24. Note the presence of Wedl tunnels along the bone surface and how the latter cuts deeply into the peripherally positioned secondary osteons. e, f Extreme cortical bone remodelling and local formation of Wedl tunnels in NMNHS FR55. rc recrystallization, rm rock matrix, so secondary osteons, wt Wedl tunnels. Scale bar: a–d, f—100 μm; e—250 μm
format Recurso digital
id zenodo_https___doi_org_10_5281_zenodo_16972676
institution Zenodo
language
publishDate 2025
publisher Zenodo
record_format zenodo
spellingShingle Fig. 24 in The paleoecology and taphonomy of a Santonian-Campanian (Upper Cretaceous) dinosaur-bearing vertebrate locality from Bulgaria: a window into an underexplored part of the Late Cretaceous European
Nikolov, Vladimir
Pavlishina, Polina
Dochev, Docho
Brusatte, Stephen L.
Biodiversity
Taxonomy
Fig. 24 Osteohistology of titanosaur bones in cross-polarized light. a Secondary osteons and Wedl tunnels in the outermost cortex of NMNHS FR17. The dotted line traces the bone surfaces. b Partially recrystallized bone tissue in perimedullary developed bone trabeculae in NMNHS FR17 (λ-filter is used). c, d Numerous secondary osteons (c) and Haversian bone (d) in the outermost cortex of NMNHS FR24. Note the presence of Wedl tunnels along the bone surface and how the latter cuts deeply into the peripherally positioned secondary osteons. e, f Extreme cortical bone remodelling and local formation of Wedl tunnels in NMNHS FR55. rc recrystallization, rm rock matrix, so secondary osteons, wt Wedl tunnels. Scale bar: a–d, f—100 μm; e—250 μm
title Fig. 24 in The paleoecology and taphonomy of a Santonian-Campanian (Upper Cretaceous) dinosaur-bearing vertebrate locality from Bulgaria: a window into an underexplored part of the Late Cretaceous European
topic Biodiversity
Taxonomy
url https://doi.org/10.5281/zenodo.16972676