Movatterモバイル変換


[0]ホーム

URL:


Skip to main page content
U.S. flag

An official website of the United States government

Dot gov

The .gov means it’s official.
Federal government websites often end in .gov or .mil. Before sharing sensitive information, make sure you’re on a federal government site.

Https

The site is secure.
Thehttps:// ensures that you are connecting to the official website and that any information you provide is encrypted and transmitted securely.

NIH NLM Logo
Log inShow account info
Access keysNCBI HomepageMyNCBI HomepageMain ContentMain Navigation
pubmed logo
Advanced Clipboard
User Guide

Full text links

Free PMC article
Full text links

Actions

Share

.2023;142(1):15.
doi: 10.1186/s13358-023-00277-3. Epub 2023 Aug 16.

Comparative bone histology of two thalattosaurians (Diapsida: Thalattosauria):Askeptosaurus italicus from the Alpine Triassic (Middle Triassic) and a Thalattosauroidea indet. from the Carnian of Oregon (Late Triassic)

Affiliations

Comparative bone histology of two thalattosaurians (Diapsida: Thalattosauria):Askeptosaurus italicus from the Alpine Triassic (Middle Triassic) and a Thalattosauroidea indet. from the Carnian of Oregon (Late Triassic)

N Klein et al. Swiss J Palaeontol.2023.

Abstract

Here, we present the first bone histological and microanatomical study of thalattosaurians, an enigmatic group among Triassic marine reptiles. Two taxa of thalattosaurians, the askeptosauroidAskeptosaurus italicus and one as yet undescribed thalattosauroid, are examined. Both taxa have a rather different microanatomy, tissue type, and growth pattern.Askeptosaurus italicus from the late Anisian middle Besano Formation of the southern Alpine Triassic shows very compact tissue in vertebrae, rib, a gastralium, and femora, and all bones are without medullary cavities. The tissue shows moderate to low vascularization, dominated by highly organized and very coarse parallel-fibred bone, resembling interwoven tissue. Vascularization is dominated by simple longitudinal vascular canals, except for the larger femur ofAskeptosaurus, where simple vascular canals dominate in a radial arrangement. Growth marks stratify the cortex of femora. The vertebrae and humeri from the undescribed thalattosauroid from the late Carnian of Oregon have primary and secondary cancellous bone, resulting in an overall low bone compactness. Two dorsal vertebral centra show dominantly secondary trabeculae, whereas a caudal vertebral centrum shows much primary trabecular bone, globuli ossei, and cartilage, indicating an earlier ontogenetic stage of the specimens or paedomorphosis. The humeri of the thalattosauroid show large, simple vascular canals that are dominantly radially oriented in a scaffold of woven and loosely organized parallel-fibred tissue. Few of the simple vascular canals are thinly but only incompletely lined by parallel-fibered tissue. In the Oregon material, changes in growth rate are only indicated by changes in vascular organization but no distinct growth marks were identified. The compact bone ofAskeptosaurus is best comparable to some pachypleurosaurs, whereas its combination of tissue and vascularity is similar to eosauropterygians in general, except for the coarse nature of its parallel-fibred tissue. The cancellous bone of the Oregon thalattosauroid resembles what is documented in ichthyosaurs and plesiosaurs. However, in contrast to these its tissue does not consist of fibro-lamellar bone type. Tissue types of both thalattosaurian taxa indicate rather different growth rates and growth patterns, associated with different life history strategies. The microanatomy reflects different life styles that fit to the different environments in which they had been found (intraplatform basin vs. open marine). Both thalattosaurian taxa differ from each other but in sum also from all other marine reptile taxa studied so far. Thalattosaurian bone histology documents once more that bone histology provides for certain groups (i.e., Triassic Diapsida) only a poor phylogenetic signal and is more influenced by exogenous factors. Differences in lifestyle, life history traits, and growth rate and pattern enabled all these Triassic marine reptiles to live contemporaneously in the same habitat managing to avoid substantial competition.

Keywords: Coarse parallel-fibred tissue; Globuli ossei; Life style; Microanatomy; Tissue type diversity; Triassic marine reptiles.

© Akademie der Naturwissenschaften Schweiz (SCNAT) 2023.

PubMed Disclaimer

Conflict of interest statement

Competing interestsThere are no competing interests.

Figures

Fig. 1
Fig. 1
Histology of vertebra (AG), rib (H, J) and gastralium (I, K, L) ofAskeptosaurus italicus.A, Transverse section of laterally compressed tail vertebra (PIMUZ T 4839_vert_a) in polarized light.B, Detail of neural spine displaying a medullary region filled by endosteal lamellar bone and surrounded by well and poorly organized coarse parallel-fibered bone of the periosteal region in polarized light.C, Collapsed trabecular structure of the inner centrum (PIMUZ T 4839_vert_a) consisting of endosteal lamellar bone (white/bright areas) and patches of calcified cartilage (some marked by arrows) in polarized light. The dark black spots are diagenetically initiated opaque mineral phases.D, Detail of medullary region and cortex of the tail vertebra (PIMUZ T 4839_vert_a) in polarized light. Dimension/extension of thin periosteal cortex indicated by double headed arrows. Single headed arrows indicate direction of Sharpey’s fibers (in bright grey/whitish and black, the latter are overgrown by opaque mineral phases).E, Detail of periosteal cortex of the tail vertebrae (PIMUZ T 4839_vert_a) in polarized light depicting coarse parallel-fibred tissue showing mainly in the upper left half a honeycomb structure of the thick and coarse scaffold of the parallel-fibred bone.F, Detail of periosteal cortex with primary osteons (arrows) of the tail vertebrae (PIMUZ T 4839_vert_a) in polarized light.G, High magnification of the periosteal cortex of the tail vertebra (PIMUZ T 4839_vert_a) with higher organized and less coarse parallel-fibred tissue in polarized light. The arrow marks Sharpey’s fibers.H, Cross section of the rib of PIMUZ T 4839 in polarized light. Note the dense central medullary region filled by endosteal bone and the nearly avascular, compact periosteal cortex consisting of coarse parallel-fibred bone.I, Cross section of the gastralium of PIMUZ T 4840 in normal light. Note the compact avascular tissue and the accumulations of osteocyte lacunae.J, Detail of rib tissue (endosteal and periosteal) in polarized light as marked with the rectangle in H). Note the coarse parallel-fibred tissue and the simple vascular canals obscured by opaque mineral phases (in black).K, Detail of gastral tissue of PIMUZ T 4840 in polarized light. Note the different degree of organization of the coarse parallel-fibred tissue in polarized light. The arrow marks the direction of Sharpey’s fibers.L, Enlargement of tissue of the gastralium in polarized light. Note the coarse parallel-fibred tissue and Sharpey’s fibers and the dense accumulations of osteocytes. The arrow marks the direction of Sharpey’s fibers. Abbreviations:eb, endosteal lamellar bone;ipo, incompletely lined primary osteons,hclp honeycomb-like pattern,hpfb highly organized coarse parallel-fibred bone,ppfb poorly organized coarse parallel-fibred bone,mr medullary region,Shf Sharpey’s fibers,svc simple vascular canals
Fig. 2
Fig. 2
Histology of femora ofAskeptosaurus italicus.A, Midshaft cross section of the left femur of PIMUZ T 4839 in normal light. Note the overall radial organization of vascular canals and different growth phases as indicated by distinct lines of arrested growth and/or changes in color. Note the shifts of the growth layers indicating compaction (white arrows). Black arrows indicate LAGs.B, Midshaft cross section of the right femur of PIMUZ T 4839 in normal light. Vascularity is less radial and more longitudinally organized. Note the shifts of the growth layers indicating compaction (white arrows). Black arrows indicate LAGs.C, Patches of calcified cartilage embedded in endosteal lamellar bone in the medullary region of the right femur.D, Strong radial organization of simple vascular canals and incompletely lined primary osteons in the outer cortex of the left femur. Note the coarse and loosely organized parallel-fibred tissue alternating with more with more higher organized and more finely organized parallel-fibred tissue.E, Detail of cortex of the right femur depicting alternating coarse and loosely organized parallel-fibred tissue and with more higher organized and more finely organized parallel-fibred tissue.F, Enlargement of outer cortex of the left femur. Note the simple vascular canal (white arrow) that opens into the surface and the coarse nature of the parallel-fibred tissue.G, Region with primary osteons that are completely and incompletely lined by parallel-fibred bone in the left femur.H, Enlargement of coarse parallel-fibred tissue with simple vascular canals.I, Midshaft cross section of the left femur of PIMUZ T 4840 in normal andJ, in polarized light. Note the principally radial orientation of the mainly short radial and longitudinal vascular canals. Vascular density is lower when compared to the femora of PIMUZ T 4839.K, Detail of the cortex from the postaxial bone side in polarized light. Note that the outer cortex shows more vascular canals than the inner cortex. The entire cortex is stratified by growth marks.L, Detail of well vascularized (by simple vascular canals) and poorly organized inner tissue visible in I and J dorsally to the medullary region in polarized light. Note the coarse nature of the loosely organized parallel-fibred tissue.M, Radially organized vascular canal system at the dorsal bone side. Note the funnel-shaped arrangement of tissue along the simple radial vascular canals in polarized light.N, Detail of cortex depicted in K in normal light. Note the accumulation of osteocyte lacunae in the left part of the picture. Abbreviations:cc, calcified cartilage;ipo, incompletely lined primary osteons;mr, medullary region;svc, simple vascular canals
Fig. 3
Fig. 3
Histology of vertebral centra of the thalattosauroid from Oregon.A, Transverse section of a middle dorsal centrum (MNCH F71616) in normal light. Note the overall spongious structure and very thin cortex surrounding the centrum. Rectangles mark the enlarged area depicted inB andC.B, Detail of the thin outer cortex and the spongious inner structure of MNCH F71616 in normal light.C, Enlargement of the thin cortex of MNCH F71616 in normal light.D, Sagittal section of a posterior dorsal centrum (MNCH F70662) in normal light. Rectangles mark the enlarged area depicted in E, F, and G.E, Detail of the anterior/posterior margin of MNCH F70662 depicting collapsed trabeculae and a matrix of cartilage (greyish–blackish) in normal light.F, Primary trabeculae reaching into the outer cortex in MNCH F70662.G, Detail of primary trabeculae in MNCH F70662 in normal light.H, Sagittal section of a middle caudal centrum (MNCH F64330) in normal light. Rectangles mark the enlarged area depicted inIL.I, Anterior or posterior bone side depicting a spongious structure in the inner and a more compact area towards the outer cortex of the middle caudal centrum MNCH F64330 in normal light.J, Boundary between the periosteal tissue to the left and the endochondral, much more finely structured tissue to the right in MNCH F64330 in normal light.K, Detail of parallel-fibred periosteal tissue in the centrum MNCH F64330 in polarized light.L, Detail of the anterior/posterior margin depicting globuli ossei and a cartilage matrix below the articular surface of MNCH F64330 in normal light. Abbreviation:nc neural canal
Fig. 4
Fig. 4
Histology of humeri of the thalattosauroid from Oregon.A, Humerus (MNCH F64270), longitudinal section, core sample. Note that the core was cut somewhat off-center, the neutral area is to the left, distal to the right. Image in normal light.B, Humerus (MNCH F64316), transverse section in normal light.C, Interpretative sketch of the tissue distribution in MNCH F64316.D, Detail of periosteal cortex in MNCH F64316 in normal light. Note the radial trabecular structure of the primary periosteal cortex. The middle layer is seen in the lower left corner, but most of the field of view is covered by the outer layer. The outermost layer is in the upper right corner.E, Detail of primary periosteal cortex in MNCH F64316 in normal andF, polarized light showing the transition zone between the middle (right) and outer layers (left). Note the high amount of plump osteocyte lacunae. Simple vascular and incipient primary osteons canals are mainly oriented longitudinally.G, Enlargement of the transition zone between the middle and outer layers in the periosteal cortex of MNCH F64316 in normal andH, polarized light. Note the low amount of osteocyte lacunae in a relatively high organized parallel-fibred tissue. Vascularity is high, consisting of large longitudinal to radial simple vascular canals with limited osteonal lining.I, Enlargement of parallel-fibred tissue and simple vascular canals in MNCH F64316 in polarized light.J, Detail of the middle layer of the periosteal cortex transitioning to the inner layer (upper right) in MNCH F64316 in normal and K, polarized light. The primary parallel-fibred tissue of the middle layer is here less organized between the vascular canals but partially starts to line vascular canals in higher organization.L, Detail of secondary endosteal trabeculae (top) and primary periosteal ones (bottom) at the transition from the middle to the inner layer of the periosteal cortex in MNCH F64316 in normal andM, polarized light
See this image and copyright information in PMC

Similar articles

See all similar articles

Cited by

References

    1. Anderson KL, Druckenmiller PS, Erickson E, Maxwell EE. Skeletal microstructure of Stenopterygius quadriscissus (reptilia, ichthyosauria) from the posidonienschiefer (posidonia shale, Lower Jurassic) of Germany. Paleontology. 2019;62(3):433–449. doi: 10.1111/pala.12408. - DOI
    1. Bakker RT. Dinosaur heresy-dinosaur renaissance: why we need endothermic archosaurs for a comprehensive theory of bioenergetic evolution. In: Thomas DK, Olson EC, editors. A cold look at warm-blooded dinosaurs. American Association for the Advancement of Science; 1980. pp. 351–362.
    1. Beresford, W. A. 1981. Chondroid bone, secondary cartilage and metaplasia. Munich: Urban and Schwarzemberg.
    1. Buffrénil, V. de, Zylberberg X, Ricqlès, A. de, Padian, K. (Eds.) (2021b). Vertebrate Skeletal Histology and Paleohistology. Boca Raton: CRC Press.
    1. Buffrénil, V. de, & Mazin, J.-M. (1990). Bone histology of the ichthyosaurs: comparative data and functional interpretation. Paleobiology,16, 435–447. 10.1017/S0094837300010174

Related information

LinkOut - more resources

Full text links
Free PMC article
Cite
Send To

NCBI Literature Resources

MeSHPMCBookshelfDisclaimer

The PubMed wordmark and PubMed logo are registered trademarks of the U.S. Department of Health and Human Services (HHS). Unauthorized use of these marks is strictly prohibited.


[8]ページ先頭

©2009-2025 Movatter.jp