Showing posts with label Placoderm. Show all posts
Showing posts with label Placoderm. Show all posts

Thursday, May 21, 2020

[PaleoIchthyology • 2020] Was the Devonian Placoderm Titanichthys A Suspension Feeder?


Titanichthys sp.

in Coatham, Vinther, Rayfield & Klug, 2020.
Illustration: Mark Witton 

Abstract
Large nektonic suspension feeders have evolved multiple times. The apparent trend among apex predators for some evolving into feeding on small zooplankton is of interest for understanding the associated shifts in anatomy and behaviour, while the spatial and temporal distribution gives clues to an inherent relationship with ocean primary productivity and how past and future perturbations to these may impact on the different tiers of the food web. The evolution of large nektonic suspension feeders—‘gentle giants’—occurred four times among chondrichthyan fishes (e.g. whale sharks, basking sharks and manta rays), as well as in baleen whales (mysticetes), the Mesozoic pachycormid fishes and at least twice in radiodontan stem group arthropods (Anomalocaridids) during the Cambrian explosion. The Late Devonian placoderm Titanichthys has tentatively been considered to have been a megaplanktivore, primarily due to its gigantic size and narrow, edentulous jaws while no suspension-feeding apparatus have ever been reported. Here, the potential for microphagy and other feeding behaviours in Titanichthys is assessed via a comparative study of jaw mechanics in Titanichthys and other placoderms with presumably differing feeding habits (macrophagy and durophagy). Finite-element models of the lower jaws of Titanichthys termieri in comparison to Dunkleosteus terrelli and Tafilalichthys lavocati reveal considerably less resistance to von Mises stress in this taxon. Comparisons with a selection of large-bodied extant taxa of similar ecological diversity reveal similar disparities in jaw stress resistance. Our results, therefore, conform to the hypothesis that Titanichthys was a suspension feeder with jaws ill-suited for biting and crushing but well suited for gaping ram feeding.

Keywords: suspension feeding, Devonian, Arthrodira, Titanichthys, comparative biomechanics



Figure 1. Left inferognathal of Titanichthys termieri (PIMUZ A/I 4716), from the Southern Maïder basin, Morocco. The specimen is nearly complete, excluding the anteriormost tip. The inferognathal lacks both dentition and shearing surfaces. It has been glued together where fractures occurred. Photographed at the University of Zurich. Total length = 96 cm.


 Conclusion: 
FEA of the lower jaw of Titanichthys revealed that it was significantly less resistant to von Mises stress than those of related arthrodires that used macrophagous feeding strategies. This suggests that these strategies would not have been viable for Titanichthys, as its jaw would have been insufficiently mechanically robust. Consequently, it is highly likely that Titanichthys was a suspension feeder—a feeding method that is likely to exert considerably less stress on the jaw than macrophagous feeding modes. The validity of assigning suspension feeding based on jaw mechanical resilience is supported by the roughly equivalent patterns known from lineages containing extant suspension feeders.

Common morphological trends in the convergent evolution of megaplanktivores can not only be observed but quantified mechanically using FEA. A variety of methods were used to compare between the jaw models, due to imperfections with solely comparing visually or using average stress. The intervals method grouped feeding strategies to an extent, providing an additional perspective.

Tafilalichthys, probably a member of the Mylostomatidae and, therefore, one of Titanichthys' closest relatives, appears to have been durophagous. Durophagy is the likely feeding mode of all crown-group mylostomatids except Titanichthys, suggesting that it evolved from a durophagous ancestor. This durophage-to-planktivore transition is surprisingly common among convergently evolved giant suspension feeders: it is also seen in multiple, independently evolved planktivorous elasmobranch lineages.

The presence of a megaplanktivore in the Famennian supports the theory that productivity was high in the Late Devonian, which was probably a result of increased eutrophication caused by the diversification of terrestrial tracheophytes and the advent of arborescence. It reflects the link between the increasing complexity of Devonian marine ecosystems and the functional diversity of Arthrodira, which occupied a wide range of ecological niches. Most significantly, it reveals that vertebrate megaplanktivores probably existed over 150 Ma prior to the Mesozoic pachycormids, previously considered the earliest definitive giant suspension feeders.


Samuel J. Coatham, Jakob Vinther, Emily J. Rayfield and Christian Klug. 2020. Was the Devonian Placoderm Titanichthys A Suspension Feeder? Royal Society Open Science. DOI: 10.1098/rsos.200272  

Ancient giant armored fish fed in a similar way to basking sharks

Wednesday, October 26, 2016

[PaleoIchthyology • 2016] Bothriolepis rex • A New Large-bodied Species of Bothriolepis (Antiarchi) from the Upper Devonian of Ellesmere Island, Nunavut, Canada


Bothriolepis rex 
 Downs, Daeschler, Garcia & Shubin, 2016 


ABSTRACT
New material from the Upper Devonian (Frasnian) Nordstrand Point Formation of Ellesmere Island, Nunavut, Canada, represents the largest known species of antiarch and the first described from the Nordstrand Point Formation. Bothriolepis rex, sp. nov., is additionally remarkable for the thickness and compactness of its dermal skeletal plates. The new species is diagnosed by a preorbital recess with a horizontal rostral margin; the presence of a wide unornamented border surrounding the infraorbital sensory line; central sensory lines that meet the margin of the nuchal close to the lateral corners; a supraotic thickening that does not extend caudal to a transverse crista of the nuchal; and a tall lateral lamina of the anterior dorsolateral. The thick and compact armor of Bothriolepis rex, sp. nov., recalls that of the co-occurring Perscheia pulla and gives occasion to a physical and ecological review of dermal skeletal mass and density in large-bodied, bottom-dwelling organisms in nonmarine ecosystems during the Late Devonian.


Fossil bones from the skull of Bothriolepis rex and a line drawing of the head viewed from above. The large, thick bones create an armor with a single opening for the eyes. The mouth is on the lower surface of the skull, indicating a bottom-feeding lifestyle.
Photo by Valentina Garcia, drawing by Jason Downs. 


SYSTEMATIC PALEONTOLOGY

ANTIARCHI Cope, 1885
BOTHRIOLEPIDIDAE Cope, 1886

BOTHRIOLEPIS Eichwald, 1840

 BOTHRIOLEPIS REX, sp. nov.
Bothriolepis sp. Elliott et al., 2004.

Holotype— NUFV 1192, nuchal plate (Fig. 3).

Etymology— From the Latin ‘rex,’ king, in reference to the large body size.

Type Locality and Horizon— NV2K11 site (N77 06.1630 W87 09.0640), Nordstrand Point Formation near Okse Bay on southern Ellesmere Island, Nunavut, Canada. Palynological data indicate a middle Frasnian age (Maclarenii zone of Embry and Klovan, 1976).

A rendition of what the Bothriolepis rex would have looked like in its natural habitat along with a comparison of its size to that of a T. rex and an average human being.
Art by Jason Poole/Academy of Natural Sciences. 


Jason P. Downs, Edward B. Daeschler, Valentina E. Garcia and Neil H. Shubin. 2016. A New Large-bodied Species of Bothriolepis (Antiarchi) from the Upper Devonian of Ellesmere Island, Nunavut, Canada.  Journal of Vertebrate Paleontology.  DOI: 10.1080/02724634.2016.1221833

A New ‘King’ — New, Gigantic, Ancient Armored Fish Discovered   https://shar.es/1E5ANd 

   

Saturday, September 3, 2016

[PaleoIchthyology • 2016] Placoderm Assemblage from the Tetrapod-Bearing Locality of Strud (Belgium, Upper Famennian) Provides Evidence for a Fish Nursery


Fig 2. Reconstruction of the immature placoderms and diagrammatic model of the Strud nursery.
Immature placoderms (from top to bottom) Turrisaspis strudensis (left lateral view), Grossilepis rikiki (dorsal view), Phyllolepis undulata (dorsal view). Diagrammatic model of the Strud nursery displaying the habitat partitioning: on the left, shallow waters of the nursery with immature placoderms inside and Rhacophyton plant on the bank; on the right, deeper area with the placoderm adults. Scale bars equal 2 cm. Animal and environmental reconstructions by J. Jacquot Haméon (MNHN, Paris). 

Abstract

The placoderm fauna of the upper Famennian tetrapod-bearing locality of Strud, Belgium, includes the antiarch Grossilepis rikiki, the arthrodire groenlandaspidid Turrisaspis strudensis and the phyllolepidid Phyllolepis undulata. Based on morphological and morphometric evidence, the placoderm specimens from Strud are predominantly recognised as immature specimens and this locality as representing a placoderm nursery. The Strud depositional environment corresponds to a channel in an alluvial plain, and the presence of a nursery in such environment could have provided nutrients and protection to the placoderm offspring. This represents one of the earliest pieces of evidence for this sort of habitat partitioning in vertebrate history, with adults living more distantly from the nursery and using the nursery only to spawn or give live birth.

Fig 2. Reconstruction of the immature placoderms and diagrammatic model of the Strud nursery.
 Immature placoderms (from top to bottom) Turrisaspis strudensis (left lateral view), Grossilepis rikiki (dorsal view), Phyllolepis undulata (dorsal view). Diagrammatic model of the Strud nursery displaying the habitat partitioning: on the left, shallow waters of the nursery with immature placoderms inside and Rhacophyton plant on the bank; on the right, deeper area with the placoderm adults. Scale bars equal 2 cm. Animal and environmental reconstructions by J. Jacquot Haméon (MNHN, Paris).


Sébastien Olive, Gaël Clément, Edward B. Daeschler and Vincent Dupret. 2016. Placoderm Assemblage from the Tetrapod-Bearing Locality of Strud (Belgium, Upper Famennian) Provides Evidence for a Fish Nursery. PLoS ONE. 11(8): e0161540.


Thursday, August 18, 2016

[PaleoIchthyology • 2008] Materpiscis attenboroughi • Live Birth in the Devonian Period: Placoderm Fish from the Gogo Area of north-west Western Australia


Materpiscis attenboroughi  Long, Trinajstic, Young & Senden, 2008 

Artist’s reconstruction of Materpiscis gen. nov. giving birth.
by B. Choo. DOI:  10.1038/nature06966 

Materpiscis attenboroughi  
Long, Trinajstic, Young & Senden, 2008

   a, Diagram showing position of embryo and yolk sac within the mother. b, Artist’s reconstruction of Materpiscis gen. nov. giving birth (by B. Choo).

The extinct placoderm fishes were the dominant group of vertebrates throughout the Middle Palaeozoic era, yet controversy about their relationships within the gnathostomes (jawed vertebrates) is partly due to different interpretations of their reproductive biology. Here we document the oldest record of a live-bearing vertebrate in a new ptyctodontid placoderm, Materpiscis attenboroughi gen. et sp. nov., from the Late Devonian Gogo Formation of Australia (approximately 380 million years ago). The new specimen, remarkably preserved in three dimensions, contains a single, intra-uterine embryo connected by a permineralized umbilical cord. An amorphous crystalline mass near the umbilical cord possibly represents the recrystallized yolk sac. Another ptyctodont from the Gogo Formation, Austroptyctodus gardineri, also shows three small embryos inside it in the same position. Ptyctodontids have already provided the oldest definite evidence for vertebrate copulation8, and the new specimens confirm that some placoderms had a remarkably advanced reproductive biology, comparable to that of some modern sharks and rays. The new discovery points to internal fertilization and viviparity in vertebrates as originating earliest within placoderms.


Placodermi McCoy, 1848
Ptyctodontida Gross, 1932

Materpiscis attenboroughi gen. et sp. nov.

Etymology. Generic name from the Latin meaning ‘mother fish’; species name in honour of Sir David Attenborough, who first drew attention to the Gogo fish sites in his 1979 series Life on Earth.

Holotype. WAM 07.12.1 (Western Australian Museum, Perth).

Age and locality. From the Stromatoporoid camp locality, Gogo Station, near Fitzroy Crossing, Western Australia (Late Devonian, early Frasnian).

Diagnosis. A small aspinothoracid ptyctodontid fish having an anteriorly pointed nuchal plate that participates in the posterior margin of the skull roof, broad roughly triangular-shaped preorbitals that meet mesially; the marginal plate has a large postorbital region with parallel rows of tubercles adorning it; the submarginal is strap-like and strongly curved mesially; robust triturating tooth plates that meet only at anterior tips, superognathals with moderately high anterior dorsal process. The body is scaleless.


Dr John Long of Museum Victoria in Melbourne holds a model of a placoderm fish fossil that was was found in the Gogo area of north-west Western Australia and was named Materpiscis attenboroughi.
 Photograph: William West/AFP/Getty Images 



John A. Long, Kate Trinajstic, Gavin C. Young and Tim Senden. 2008. Live Birth in the Devonian Period. Nature. 453; 650-652. DOI:  10.1038/nature06966 

Oldest Live-Birth Fossil Found; Fish Had Umbilical Cord