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Peer-reviewedCC BY 4.0The Anatomical Record: Advances in Integrative Anatomy and Evolutionary Biology

Osteohistological evidence for terrestrial adaptation and an extended growth period in mekosuchine crocodylians and its potential role in their extinction

Abstract

The Australasian crocodylian fossil record is dominated by the extinct endemic clade Mekosuchinae, with known members spanning the Eocene‐to‐Holocene. This diverse clade exhibited high morphological disparity, from early members superficially similar to Crocodylus , to more terrestrial forms later in the clade's evolutionary history. However, it remains unclear why mekosuchines went extinct whilst Crocodylus continues to thrive in the region, and how the ancestors of this terrestrial clade reached Australasia without long‐distance transoceanic dispersal. One possible explanation is that there was intraclade variation in the growth pattern and life habit of mekosuchine species, and that these, in turn, differ from those of Crocodylus . Here, we present the first osteohistological study of mekosuchines, evaluating the femora of the middle–late Eocene species Kambara taraina and late Oligocene–middle Miocene Baru ( B . wickeni , B . darrowi ). Bone compactness profiles are more characteristic of a terrestrial habit than those of extant crocodylians, with Baru darrowi demonstrating the most terrestrialized profile. Apposition rates are similar in absolute value to those of extant crocodylians, indicating a comparable metabolism; however, high appositional rates throughout mid‐cortical cyclical growth marks suggest that mekosuchines were able (or needed) to maintain a moderate rate of growth for longer than extant crocodylians. Our results indicate that mekosuchines were more terrestrial than Crocodylus and that later‐diverging mekosuchines showed increased terrestrialization; however, they do not indicate that early mekosuchines were well‐adapted to transoceanic dispersal. Heightened terrestrialization and an extended moderate growth period might have made mekosuchines more vulnerable to late Cenozoic aridification in Australia than semi‐aquatic Crocodylus .

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BibTeX
@article{hoffman2026osteohistological,
  title = {{Osteohistological evidence for terrestrial adaptation and an extended growth period in mekosuchine crocodylians and its potential role in their extinction}},
  author = {Devin K Hoffman and Cecily S C Nicholl and Oliver Bradley and Sreya Magar and Marie Sofia Sebaratnam and Alexandra Houssaye and Ryan N Felice and Adam M Yates and Stephen F Poropat and Philip D Mannion},
  journal = {The Anatomical Record: Advances in Integrative Anatomy and Evolutionary Biology},
  year = {2026},
  month = sep,
  doi = {10.1002/ar.70341},
  url = {https://hal.science/hal-05754763v1},
  note = {CC BY 4.0},
}
RIS
TY  - JOUR
TI  - Osteohistological evidence for terrestrial adaptation and an extended growth period in mekosuchine crocodylians and its potential role in their extinction
AU  - Devin K Hoffman
AU  - Cecily S C Nicholl
AU  - Oliver Bradley
AU  - Sreya Magar
AU  - Marie Sofia Sebaratnam
AU  - Alexandra Houssaye
AU  - Ryan N Felice
AU  - Adam M Yates
AU  - Stephen F Poropat
AU  - Philip D Mannion
PY  - 2026
DA  - 2026/09/04
JO  - The Anatomical Record: Advances in Integrative Anatomy and Evolutionary Biology
DO  - 10.1002/ar.70341
UR  - https://hal.science/hal-05754763v1
AB  - The Australasian crocodylian fossil record is dominated by the extinct endemic clade Mekosuchinae, with known members spanning the Eocene‐to‐Holocene. This diverse clade exhibited high morphological disparity, from early members superficially similar to Crocodylus , to more terrestrial forms later in the clade's evolutionary history. However, it remains unclear why mekosuchines went extinct whilst Crocodylus continues to thrive in the region, and how the ancestors of this terrestrial clade reached Australasia without long‐distance transoceanic dispersal. One possible explanation is that there was intraclade variation in the growth pattern and life habit of mekosuchine species, and that these, in turn, differ from those of Crocodylus . Here, we present the first osteohistological study of mekosuchines, evaluating the femora of the middle–late Eocene species Kambara taraina and late Oligocene–middle Miocene Baru ( B . wickeni , B . darrowi ). Bone compactness profiles are more characteristic of a terrestrial habit than those of extant crocodylians, with Baru darrowi demonstrating the most terrestrialized profile. Apposition rates are similar in absolute value to those of extant crocodylians, indicating a comparable metabolism; however, high appositional rates throughout mid‐cortical cyclical growth marks suggest that mekosuchines were able (or needed) to maintain a moderate rate of growth for longer than extant crocodylians. Our results indicate that mekosuchines were more terrestrial than Crocodylus and that later‐diverging mekosuchines showed increased terrestrialization; however, they do not indicate that early mekosuchines were well‐adapted to transoceanic dispersal. Heightened terrestrialization and an extended moderate growth period might have made mekosuchines more vulnerable to late Cenozoic aridification in Australia than semi‐aquatic Crocodylus .
SN  - 1932-8486
SN  - 1932-8494
ER  -