In February this year I started my PhD thesis. As with all PhD’s there are various milestones where you must hand in some sort of report to make sure you aren’t just sitting around all day and drinking beer (tempting though it is). This week I finally completed my 3 month report (only 2 months late) and now I can finally worry about doing some research. This post came about after a brief twitter conversation with fellow PhD student Jon Tennant (aka @Protohedgehog, check out his awesome blog here) from Imperial College London, who suggested doing what he did and blogging his 3 month report so everyone can see what I’m getting up to (for better or for worse). So here you go! It’s a little bit drier than my usual blogging style and has a bit more jargon, but have at it anyway! If there’s anything you want to know more about drop me an email (see about section at top of the blog page for the email address).
Proposed thesis title
Investigations into hearing in toothed mysticetes (Cetacea: Mammalia) via studies of the periotic (petrosal) and mandible.
This thesis will investigate the auditory structures of the inner ear and mandible shape in toothed mysticetes. Whilst at first, these two subjects may at first appear to be disparate fields, consider that in modern cetaceans, auditory cues are the primary method by which they locate their prey, their olfactory abilities being the poorest of any mammal group (Pihlström 2008) and vision being limited due to low light levels in water at depth. Furthermore, in odontocetes (and most archaeocetes except for pakicetids) sound is/was received via the jawbone. Thus, the structure of the jaw must adequately serve the demands of two processes, namely sound reception and prey capture/feeding.
Whilst these aspects have been investigated to varying extent in archaeocetes, odontocetes and extant mysticetes (e.g. Nummela et al. 2004, 2007, Werth 2006, Yamato et al. 2012, Pyenson et al. 2013), there has been insufficient time devoted to them in toothed mysticetes. Toothed mysticetes are however, of particular interest in these aspects for several reasons. The transition from teeth to baleen is one of the key innovations in cetacean evolution, requiring major morphological changes in the skull and perhaps even led to the shift towards enormous body size (Werth 2000, Fitzgerald 2006, Slater et al. 2010). Some species of toothed mysticetes are reported to have possessed “proto-baleen” (Deméré & Berta 2008, Deméré et al. 2008, Berta 2012), but this is based on the inference of homologous structures in the palate and remains to be corroborated by the presence of fossilised baleen in association with one of these toothed mysticete taxa. Yet it is crucial to remember at this point that these toothed mysticetes were not just transitional species, an intermediate point on the path to baleen; rather they were successfully making a living and had carved their own ecological niche. This is the catalyst for this thesis. I plan to investigate how these animals were making a living, what sounds they could hear and how it affected how they fed. Modern mysticetes have low frequency hearing, very different to the high frequency, echolocating odontocetes. What is unknown is what frequencies the toothed mysticetes were capable of hearing. Did they share the low frequency hearing found in modern mysticetes or did the shift to lower frequencies and the attendant morphological changes of the inner ear coincide with the evolution of baleen? The hearing capabilities of the toothed mysticetes will also add further inferential morphological data to their hypothesised feeding ecologies. I plan to test these hypotheses in quantitative manner for the first time (in toothed mysticetes) using morphometric and finite element analyses (FEA). This will be set out in more detail in the research methodology section
Below I briefly review the evolution of early cetaceans and the mysticetes. I then summarise the current knowledge on the evolution of cetacean hearing and mandible shape before outlining my intended research methodology and estimated timeline for the project.
Cetacean Origins: The Archaeocetes
Cetaceans (whales and dolphins) are a poster child of evolution, their origins from land mammals and transition to the ocean giants of today being one of the most extraordinary tales of adaptation. Yet this has not always been the case, their extremely derived morphology causing earlier workers much frustration in their efforts to classify the “most peculiar and aberrant of mammals” (Simpson 1945), with the key revelations of their ancestry not coming to light until the past few decades (Uhen 2010). Now, the numerous fossils documenting almost every stage of this group’s evolution make it one of the most valuable case studies in macroevolution.
Cetaceans are first found in the fossil record in the Early Eocene of Pakistan; these animals were semiaquatic “walking whales” belonging to the Pakicetidae and Ambulocetidae (Gingerich et al. 1983, Thewissen et al. 1996, Madar 2007). They still retained the ability to move around on land although their skeleton was denser than their wholly terrestrial relatives (Madar 2007). By the Middle Eocene, the Remingtonocetidae and Protocetidae had appeared (Kumar & Sahni 1986, Hulbert Jr 1998, Gingerich et al. 2001, 2009, Bajpai et al. 2011) and evolved into nearshore marine (Gingerich et al. 1995, Clementz et al. 2006) animals that possessed a crocodile-like morphology, with long bodies, short limbs and a narrow, elongated rostrum (Thewissen & Bajpai 2009). The protocetids rapidly diversified and spread across the globe, reaching as far as North and South America (Hulbert et al. 1998, Uhen et al. 2011). The transition to an obligately aquatic lifestyle was completed with the appearance of the basilosaurids in the late Middle Eocene. Their remains are known from every continent except for Antarctica (Uhen 2009). Features that indicate a fully marine lifestyle include: acoustic isolation of the auditory structures within the skull via enlarged sinuses; shortened neck; forelimb dorsoventrally flattened to form a flipper; greatly reduced hind limbs that were incapable of supporting the animal’s weight on land and the presence of a tail fluke (Gingerich et al. 1990, Uhen 1998, 2004, 2009). The basilosaurids (and especially the Dorudontinae) are thought to have given rise to Neoceti (the group comprised of Mysticeti and Odontoceti) (Uhen 2004).
Modern mysticetes, also known as the baleen whales due to the keratinous plates attached to the gum of the upper jaw that are used to sieve small marine organisms from seawater, are some of the most awe-inspiring creatures ever to grace this planet. They include the largest animal to have ever evolved, the blue whale (Balaenoptera musculus), which can reach lengths of 30 m and weigh more than 170 tons (Bannister 2009). There are four extant mysticete families: Balaenidae (right, bowhead whales); Balaenopteridae (rorquals); Eschrichtiidae (gray whale) and the enigmatic pygmy right whale (Caperea marginata) which has traditionally been placed in its own family, the Neobalaenidae, but a recent analysis by Fordyce & Marx (2012) found it to belong to the Cetotheriidae, making it the sole living taxon of this family.
Whilst all living mysticetes possess baleen, not all fossil mysticetes share this feature, with early taxa possessing teeth instead. The transition from these toothed mysticetes into the baleen bearing behemoths of today is one area in cetacean evolution that is still subject to vigorous debate and research (Deméré et al. 2008, Esperante et al. 2008, Fitzgerald 2012, Armfield et al. 2013). There are three families of toothed mysticete, the Llanocetidae, Mammalodontidae and the Aetiocetidae, in addition to the still undescribed “archaeomysticete” taxa from the Oligocene of South Carolina (Barnes & Sanders 1996a, b). The Llanocetidae is represented by Llanocetus denticrenatus, from Seymour Island, Antarctica. The holotype consists of a partial mandible and an endocranial cast (Mitchell 1989), although an almost compete skull and partial skeleton, believed to be from the same individual is currently under study by Ewan Fordyce (Berta & Deméré 2009, Fitzgerald 2010). Llanocetus represents the oldest known mysticete and has been interpreted as a filter feeder that is intermediate in form between basilosaurids and crown mysticetes (Fordyce 2003), with the large diastemata between its teeth allowing the teeth to act as a food sieve (Fordyce 2003), or even potentially being filled by baleen (Berta 2012). The mammalodontids consist of the taxa Mammalodon colliveri and Janjucetus hunderi from the Late Oligocene of Australia (Pritchard 1939, Fitzgerald 2006, 2010). These species were small-bodied with short rostra and large orbits. They have been most recently interpreted as a suction-feeder and a macrophagous predator respectively (Fitzgerald 2006, 2010). The aetiocetids were the most numerous toothed mysticete family with a total of five genera. They too were small bodied (estimated length of 2-3 m) but differed from the mammalodontids in that they had a relatively elongate, broad rostrum and mandible that bowed outwards, similar to modern mysticetes (Berta & Deméré 2009). One species of aetiocetid (Aetiocetus weltoni) reportedly possesses palatal foramina and sulci that may homologous with similar structures found in modern mysticetes. These structures house the blood vessels that supply the epithelia from which baleen develops, meaning that it too may have possessed baleen, if even in only an incipient form (Deméré & Berta 2008). The earliest edentulous (toothless) mysticetes are the eomysticetids, known from North America, New Zealand and Mexico (Sanders & Barnes 2002, Berta & Deméré 2009). However the majority of these specimens are yet to be described, therefore the full diversity of this group remains unknown.
The Evolution of Cetacean Hearing
As cetaceans evolved from wholly terrestrial animals into obligately marine mammals during the course of the Eocene, their organ systems underwent major restructuring and modification. Perhaps no other organ system underwent as profound and wholesale a series of changes as that of the ear region which had to evolve the ability to detect sound in a much denser medium.
The ancestors of cetaceans possessed the generalised form of the majority of land mammals. Sound is transmitted via an air-filled external auditory meatus to the tympanic membrane, where the differential pressures cause it to vibrate and pass the sound onto the three middle ear bones, the malleus, incus and stapes. These bones serve to amplify the sound pressure by decreasing the area through which the sound is passed (Nummela et al. 2007). The stapes, in turn, transmits the sound to the fluid-filled cochlea via a piston-like action (Nummela et al. 2004). The vibrations of the cochlear fluid (perilymph) are transmitted to the hair cells of the cochlea and converted into a neural impulse and sent to the brain. This pathway is not effective underwater however as the external auditory meatus becomes filled with water, reducing the pressure differential at the tympanic membrane and therefore greatly diminishing its ability to transmit sounds to the middle ear bones. Furthermore, when underwater, the similar density of animal tissue to water means that sounds will simply travel through the tissues and bones, a phenomenon known as bone conduction (Nummela et al. 2007) and will lessen the animal’s ability to distinguish which direction the sound originally came from.
The earliest whales, the pakicetids, displayed very few adaptations for underwater hearing. They possessed a thickened tympanic bone that lacked a rostromedial connection to the periotic, allowing the tympanic to vibrate independently of the periotic (Nummela et al. 2004). This enhanced their ability to use bone conduction, which would have been the method by which sound was transmitted when underwater, although directional hearing underwater would still have been poor (Nummela et al. 2004, 2007). In the ambulocetids, we see the first use of the mandible and the development of the tympanic plate for use in a sound conduction pathway in cetaceans. These animals possessed a large mandibular foramen, which would have housed a mandibular fat pad. It has been hypothesised that Ambulocetus may have used bone conduction on land, by placing its lower jaw to the ground and hearing the vibrations, in a similar manner to some extant crocodiles (Thewissen et al. 1996). The remingtonocetids and protocetids also possessed large mandibular foramen, but the lateral wall of the mandible is thinner than that seen in ambulocetids, meaning that the sensitivity of their underwater hearing had increased. The land mammal hearing mechanism is still present, indicating that these animals could also still hear in air, albeit poorly. The contact between the tympanic and periotic is also further reduced and the morphology of the middle ear ossicles are beginning to approach that of modern cetaceans (e.g. the malleus now lacks a manubrium for the attachment of the tympanic membrane (Nummela et al. 2007). In protocetids, the periotic has become more detached from the skull via the development of air sinuses, allowing for improved directional underwater hearing (Nummela et al. 2007). In basilosaurids, the ear is functionally the same as modern cetaceans, with the lateral wall of the mandible almost as thin as that in odontocetes, the middle ear bones are similar to those of modern delphinids and the petrotympanic complex is acoustically isolated via air sinuses, implying that underwater hearing was now the primary function of the air. Despite this the basilosaurids still retained an external auditory meatus, although it was most likely hardly ever used (Nummela et al. 2007). This transition from an exclusively terrestrial hearing system to a sensitive underwater hearing system took place in less than 10 million years (Nummela et al. 2004).
The focus of research on the hearing of modern whales has been toothed echolocating whales (odontocetes). The hearing of mysticetes, especially the sound reception pathway, on the other hand, remains virtually unknown. A recent study by Yamato et al. (2012) proposed a potential sound reception pathway via fat body that contacts the petrotympanic complex laterally in the minke whale (Balaenoptera acutorostrata). The sound reception in modern mysticetes is patently different to that in odontocetes as the periotic is attached to the skull via the squamosal and exoccipital bones, whereas it is acoustically isolated in odontocetes. The external auditory meatus is vestigial, and remains debatable whether it is still functional (Yamato et al. 2012).
The Evolution of Cetacean Mandible Shape
The evolution of the cetacean mandible represents the incorporation of this element into the auditory system as the group became progressively more aquatic. The resulting changes in mandibular shape are the product of a trade-off between the animal’s joint need to use the mandible to secure and manipulate prey as well as receiving the sounds of its environment.
The pakicetids, as noted above, did not possess the ability to hear underwater and this is reflected by the fact that they retained the land mammal morphology of the mandible, with a small mandibular foramen (Nummela et al. 2004, 2007). Ambulocetids show the first sign of the development of underwater hearing in cetaceans, possessing a slightly enlarged mandibular foramen, although the lateral wall of the mandible is still relatively thick, meaning that higher frequency sound would be unable to pass through (Nummela et al. 2007). Remingtonocetids and protocetids on the other hand, have evolved a large mandibular foramen, indicating the presence of the mandibular fat pad. The lateral wall of the mandible also became thinner, implying an improved ability to hear underwater. In basilosaurids, both the size of the mandibular foramen and the thickness of the lateral wall approach those seen in odontocetes.
In the toothed mysticetes however, we see further changes to the shape of the mandible. The mandibular symphysis, which in all archaeocetes had been long (Fitzgerald 2012), is shortened. This symphysis also underwent further evolution within the toothed mysticetes. In Janjucetus the symphysis is rigid and sutured, but in the aetiocetids Chonecetus and Aetiocetus the symphysis is elastic and smooth, allowing the mandibles to rotate which is thought to be an adaptation to bulk feeding. The mandibular coronoid process is also relatively larger in the mammalodontids compared to the aetiocetids, although the coronoid process is still relatively larger compared to later diverging mysticetes such as the eomysticetids. The mandibular foramen is large in all toothed mysticetes, suggesting that this method sound reception pathway was still employed by the toothed mysticetes. Aetiocetid mandibles also differ from mammalodontid mandibles in that they are more tubular (Fitzgerald 2010), whereas mammalodontid mandibles more closely approach the shape of archaeocete mandibles.
This thesis aims to investigate the internal structure of the periotic in toothed mysticetes and attempt to discover any intragroup differences by comparing their morphological features. Furthermore, by comparing these structures to that of living taxa whom I plan to use as proxies, I hope to be able to infer what frequency range toothed mysticete hearing fell into. I then plan to study mandible shape in the group in order to determine how the mandibles of the mammalodontids and aetiocetids differ in morphospace relative to other marine tetrapods and also how they cope with applied loads and relate this to any differences in hearing abilities and hypothesised feeding ecologies.
This conceptual framework provides a foundation for the following core questions of the thesis:
- What were the hearing capabilities of the mammalodontids?
- What were the hearing capabilities of the aetiocetids?
- Do toothed mysticete ears scale to body size?
- Did the shift to lower frequency hearing in mysticetes occur before or after the acquisition of a bulk filter feeding lifestyle?
- Where does toothed mysticete mandible shape fall in morphospace relative to other marine tetrapods?
- Do mammalodontids and aetiocetids differ in their ability to cope with applied loads to their mandibles?
- Do the differences in hearing (if any) between mammalodontids and aetiocetids correlate with differences in mandible shape and ability to cope with applied loads?
- Does this relate to hypothesised feeding abilities of the clades?
These core questions will test the following hypotheses:
- That mammalodontids required the ability to hear higher frequencies than that found in extant mysticetes.
- That aetiocetids possessed the ability to hear lower frequencies than the mammalodontids but could still hear higher frequencies than extant mysticetes.
- That the petrotympanic complex in toothed mysticetes will scale isometrically with body size.
- That toothed mysticete mandible shape will fall somewhere in-between that of extant mysticetes and odontocetes in morphospace in a morphometric analysis.
- That the mandibles of mammalodontids (in particular Janjucetus) will be better at coping with shaking and twisting loads than the mandibles of aetiocetids.
These hypotheses will be tested using a variety of methods and technologies. Earlier studies looking at internal structure of the periotic did so using the destructive method of thin sectioning (e.g. Kasuya 1973, Fleischer 1976). This thesis however shall employ the non-destructive method of CT scanning. Extant taxa will be scanned first to establish a proxy for various frequency ranges. Then the fossil taxa will also be scanned and compared to the living taxa to infer hearing capabilities. Whilst I will also research the possibility of defining new characteristics to use, the following list of morphological characters of the petrotympanic complex, both qualitative and quantitative, will be used to help determine hearing capacities in the fossil taxa:
- Mass of the tympanic, periotic, malleus, incus and stapes (where available).
- Volume of the tympanic.
- Area of the tympanic plate and oval window.
- Thickness of tympanic plate.
- Density of malleus, incus and stapes (where available).
- Radii ratio.
– This is the ratio of the radius of the cochlea at its base to the radius of the cochlea at its apex. This ratio is strongly correlated with low frequency hearing limits (Manoussaki et al. 2008).
- Position of areas of high cochlear foramina density.
– The cochlear foramina housed the cochlear nerve fibres that transmitted the converted sound waves to the brain. Areas of high foramina density therefore represent areas of high nerve density. The position of these high density areas will therefore indicate what frequencies the animal was sensitive to as lower frequency sounds tend to travel further along the cochlear canal due to their longer wavelengths, whereas high frequency sounds will attenuate rapidly and be detected near the base of the cochlear canal (Geisler & Luo 1996).
- Diameter of spiral ganglionic canal.
– This feature is related to the previous one as Geisler & Luo (1996) found that the highest diameter of the spiral ganglionic canal coincided with the position of the area of high foramina density in the fossil mysticete Herpetocetus.
- Width of the laminar gap.
– The width of the gap between the two spiral lamina of the cochlea roughly approximates the width of the basilar membrane. A wider laminar gap at the same point in two different cochleae can indicate better sensitivity to lower frequencies. Ketten (2000) however cautions against using the laminar gap as synonymous with basilar membrane width, noting that membrane width can be overestimated by up to 110% in modern mysticetes. However, as a comparison between two cochleae the width of the gap of one relative to the other may indicate sensitivity to higher or lower frequencies.
- Extent of inner and outer lamina.
– The length of the outer bony lamina of the cochlea can be used a generic indicator of high or low frequency hearing. In odontocetes the outer lamina is present for a greater length of the cochlea, whereas in mysticetes it is reduced or absent (Ketten 2000). This is believed to affect the stiffness of the basilar membrane, the stiff, rigid membrane of odontocetes being better at detecting high frequencies than the more flexible membrane in modern mysticetes.
- Basal ratio.
– This is the axial height of the cochlea divided by the basal diameter of the cochlea. This is found to be generally negatively proportional to frequency (Ketten & Wartzok 1990). Geisler & Luo (1996) note that values for the basal ratio may vary across different studies, depending on how the diameter is measured.
- Axial pitch.
– This is the axial height of the cochlea divided by the number of turns of the cochlea. This is found to be generally negatively proportional to frequency.
- Ratio of scala tympani to scala vestibuli.
– The cochlea is divided into three chambers by membranes. These are the scala tympani, scala vestibule and scala media. This ratio was proposed by Fleischer (1976) as method for estimating frequency ranges where a large scala tympani relative to a small scala vestibuli implies high frequency hearing. Geisler & Luo (1996) found however that this condition occurs in mysticetes also and stated that it remains to be seen how effective this ratio is in distinguishing between low and high frequency hearing. This feature may or may not yet be used in this thesis.
The morphometric analysis section of this thesis will take a landmark based approach. This will involve obtaining scan data on both extant and fossil specimens. These will be gathered by myself from Museum Victoria specimens, specimens from other museum collections (via travelling to them or engaging the services of researches at those institutions) and scans already collected by colleagues. The specimens will include as wide an array of marine tetrapods (e.g. mysticetes, odontocetes, and pinnipeds) as possible to frame the following FEA study in a broader context. Using this dataset, landmarks on each specimen will be selected using an appropriate software package (e.g. Landmark (O’Higgins & Jones 2006)). Exact landmarks used in the morphometric analysis will be determined at a later point as homology of locations and functional significance must be ensured; however, the following list gives an example of some that will likely be employed:
- Anterior of jaw (origin) – midline.
- Posterior apex of mandible – left and right.
- Posterior apex of symphysis – midline.
- Dorsal apex of coronoid process – left and right.
- Dorsal apex of symphysis at widest point – midline.
- Ventral apex of symphysis at widest point – midline.
Once landmarks have been selected the data will be analyses using morphometric analysis software (e.g. Morphologika). Statistical techniques will be employed to eliminate as many confounding factors (e.g. size) as possible, before a multivariate (principle component analysis will be run.
The morphometric analysis component serves to frame the FEA in a broad phylogenetic context. In order to execute the FEA, scan data of toothed mysticete mandibles will used to create meshes for each taxon. Pending any new data on the effectiveness of low versus high order elements to construct meshes, low order elements will be used for the FEA. In order to ensure that results of the FEA are as consistent as possible with reality, boundary conditions will be set to constrain the model in space (i.e. simulations of muscle attachments, force vectors, etc.). FEA will be undertaken using specific software such as Strand7. Mandible models will be subjected to loading in various directions to compare effects of different hypothesised feeding styles on strain patterns. Statistical analysis of strain values will be undertaken using R.
Thesis Structure & Estimated Timeline
The following sections will form chapter/papers in my thesis. This is a preliminary structure only as these sections may yet be separated or combined into papers as my research progresses:
- Review of petrotympanic morphology of toothed mysticetes.
– This review paper will complement other works such as Ekdale et al. (2011) and Luo & Gingerich (1999) that have detailed the morphology of the petrotympanic complex in modern mysticetes and archaeocetes respectively.
- Study of mammalodontid hearing.
- Study of aetiocetid hearing.
- Comparison of toothed mysticete hearing, both intragroup and against extant cetaceans.
- Toothed mysticete scaling study.
– This study may yet be removed from the thesis as I have concerns over the availability of middle ear ossicle data from fossil taxa, preventing all of the necessary data from being compiled. This will be decided upon at a future date and other ideas may be pursued instead.
- Morphometric analysis of marine tetrapod mandible shape.
- FEA of toothed mysticete mandibles.
Armfield, B.A., Zheng, Z., Bajpai, S., Vinyard, C.J. & Thewissen, J.G.M., 2013. Development and evolution of the unique cetacean dentition. PeerJ 1:e24 http://dx.doi.org/10.7717/peerj.24.
Barnes, L.G. & Sanders, A.E., 1996a. The transition from archaeocetes to mysticetes: Late Oligocene toothed mysticetes from near Charleston, South Carolina. Paleontological Society Special Publication 8, 24.
Barnes, L.G. & Sanders, A.E., 1996b. The transition from Archaeoceti to Mysticeti: Late Oligocene toothed mysticetes from South Carolina, U.S.A. Journal of Vertebrate Paleontology 16, 21A.
Berta, A., 2012. Return to the Sea. The life and evolutionary times of marine mammals. University of California Press, Berkeley, 205 pp.
Berta, A. & Deméré, T.A., 2009. Mysticetes, Evolution. In Perrin, W.F., Würsig, B. & Thewissen, J.G.M., eds, Encyclopedia of Marine Mammals 2nd edition. Academic Press, Sydney, 749–753.
Bannister, J.L., 2009. Baleen Whales (Mysticetes). In Perrin, W.F., Würsig, B. & Thewissen, J.G.M., eds, Encyclopedia of Marine Mammals 2nd edition. Academic Press, Sydney, 80–89.
Clementz, M.T., Goswami, A., Gingerich, P.D. & Koch P.L., 2006. Isotopic records from early whales and sea cows: contrasting patterns of ecological transition. Journal of Vertebrate Paleontology 26, 355–70.
Deméré, T.A., Berta, A., 2008. Skull anatomy of the Oligocene toothed mysticete Aetiocetus weltoni (Mammalia; Cetacea): implications for mysticete evolution and functional anatomy. Zoological Journal of the Linnean Society of London 154, 302–352.
Deméré, T.A., McGowen, M.R., Berta, A., Gatesy, J., 2008. Morphological and molecular evidence for a stepwise evolutionary transition from teeth to baleen in mysticete whales. Systematic Biology 57, 15–37.
Ekdale, E.G., Berta, A. & Deméré, T.A., 2011. The Comparative Osteology of the Petrotympanic Complex (Ear Region) of Extant Baleen Whales (Cetacea: Mysticeti). PLoS ONE 6(6): e21311. doi:10.1371/journal.pone.0021311 http://www.plosone.org/article/info%3Adoi%2F10.1371%2Fjournal.pone.0021311.
Esperante, R., Brand, L.R., Nick, K.E., Poma, O. & Urbina M., 2008. Exceptional occurrence of fossil baleen in shallow marine sediments of the Neogene Pisco Formation, Southern Peru. Palaeogeography, Palaeoclimatology, Palaeoecology 257, 344–60.
Fitzgerald, E.M.G., 2006. A bizarre new toothed mysticete (Cetacea) from Australia and the early evolution of baleen whales. Proceedings of the Royal Society B: Biological Sciences 273, 2955–2963.
Fitzgerald, E.M.G., 2010. The morphology and systematics of Mammalodon colliveri (Cetacea: Mysticeti), a toothed mysticete from the Oligocene of Australia. Zoological Journal of the Linnean Society of London 158, 367–476.
Fitzgerald, E.M.G., 2012. Archaeocete-like jaws in a baleen whale. Biology Letters 8, 94–96.
Fleischer, G., 1976. Hearing in extinct cetaceans as determined by cochlear structure. Journal of Paleontology 50, 133–152.
Fordyce, R.E., 2003. Early crown-group Cetacea in the southern ocean: the toothed archaic mysticete Llanocetus. Journal of Vertebrate Paleontology 23, 50A.
Fordyce, R.E. & Marx, F.G., 2012. The pygmy right whale Caperea marginata: the last of the cetotheres. Proceedings of the Royal Society B: Biological Sciences 280, 20122645. http://dx.doi.org/10.1098/rspb.2012.2645.
Geisler, J.H. & Luo, Z.X., 1996. The petrosal and inner ear of Herpetocetus sp. (Mammalia: Cetacea) and their implications for the phylogeny of hearing of archaic mysticetes. Journal of Paleontology 70, 1045–1066.
Gingerich, P.D., Wells, N., Russell, D. & Shah, S.M., 1983. Origin of whales in epicontinental remnant seas: new evidence from the early Eocene of Pakistan. Science 220, 403–406.
Gingerich, P.D., ul-Haq, M., von Koenigswald, W., Sanders, W.J., Smith, B.H. & Zalmout, E.S., 1990. Hindlimbs of Eocene Basilosaurus: evidence of feet in whales. Science 249, 154–157.
Gingerich, P.D., Arif, M. & Clyde, W.C., 1995. New archaeocetes (Mammalia, Cetacea) from the middle Eocene Domanda Formation of the Sulaiman Range, Punjab (Pakistan). Contributions of the Museum Paleontology of the University of Michigan 29, 291–330.
Gingerich, P.D., Haq, M.U., Zalmout, I.S., Khan, I.H., Malakani, M.S., 2001. Origin of whales from early artiodactyls: hands and feet of Eocene Protocetidae from Pakistan. Science 293, 2239–2242.
Gingerich, P.D., ul-Haq, M., von Koenigswald, W., Sanders, W.J., Smith, B.H., Zalmout, E.S., 2009. New protocetid whale from the middle Eocene of Pakistan: birth on land, precocial development, and sexual dimorphism. PLoS One 4, e4366. http://dx.doi.org/10.1371/journal.pone.0004366.
Hulbert Jr., R.C., 1998. Postcranial osteology of the North American middle Eocene protocetid Georgiacetus. In Thewissen, J.G.M., ed, The Emergence of Whales, Evolutionary Patterns in the Origin of Cetacea. Plenum Press, New York, 235–267.
Hulbert, R.C. Jr, Petkewich, R.M., Bishop, G.A., Bukry, D & Aleshire D.P., 1998. A new middle Eocene protocetid whale (Mammalia: Cetacea: Archaeoceti) and associated biota from Georgia. Journal of Paleontology 72, 907–27.
Kasuya, T., 1973. Systematic consideration of recent toothed whales based on morphology of tympano-periotic bone. The Scientific Reports of the Whale Research Institute (Tokyo) 25, 1–103.
Ketten, D.R., 2000. Cetacean ears. In Au, W.W.L., Popper, A.N., Fay, R.R., eds, Hearing by whales and dolphins. Springer-Verlag, New York, 43–108.
Kumar, K., Sahni, A., 1986. Remingtonocetus harudiensis, new combination, a middle Eocene archaeocete (Mammalia, Cetacea) from western Kutch, India. Journal of Vertebrate Paleontology 6, 326–349.
Luo, Z.X. & Gingerich, P.D., 1999. Terrestrial Mesonychia to aquatic Cetacea: transformation of the basicranium and evolution of hearing in whales. University of Michigan Papers on Paleontology 31, 1–98.
Madar, S.I., 2007. The postcranial skeleton of early Eocene pakicetid cetaceans. Journal of Paleontology 81, 176–200.
Manoussaki, D., Chadwick, R.S., Ketten, D.R., Arruda, J., Dimitriadis, E.K. & O’Malley, J.T., 2008. The influence of cochlear shape on low-frequency hearing. Proceedings of the National Academy of Sciences 105, 6162–6166.
Mitchell, E.D., 1989. A new cetacean from the late Eocene La Meseta Formation, Seymour Island, Antarctic Peninsula. Canadian Journal of Fisheries and Aquatic Sciences 46, 2219–2235.
Nummela, S., Thewissen, J.G.M., Bajpai, S., Hussain, S.T. & Kumar, K., 2004. Eocene evolution of whale hearing. Nature 430, 776–778.
Nummela, S., Thewissen, J.G.M., Bajpai, S., Hussain, T., Kumar, K., 2007. Sound transmission in archaic and modern whales: anatomical adaptations for underwater hearing. Anatomical Record 290, 716–733.
O’Higgins, P. & Jones, N., 2006. Tools for statistical shape analysis. Hull York Medical School, http://sites.google.com/site/hymsfme/resources.
Pihlström, H., 2008. Comparative anatomy and physiology of chemical senses in aquatic mammals. In, Thewissen, J.G.M. & Nummela, S., eds, Sensory Evolution on the Threshold: Adaptations in secondarily aquatic vertebrates. University of California Press, Berkeley, 95–109.
Pritchard, G.B., 1939. On the discovery of a fossil whale in the older tertiaries of Torquay, Victoria. Victorian Naturalist 55, 151–59.
Pyenson, N.D., Goldbogen, J.A. & Shadwick, R.E., 2013. Mandible allometry in extant and fossil Balaenopteridae (Cetacea: Mammalia): the largest vertebrate skeletal element and its role in rorqual lunge feeding. Biological Journal of the Linnean Society 108, 586–599.
Sanders, A. E. & Barnes, L.G., (2002). Paleontology of the Late Oligocene Ashley and Chandler Bridge Formations of South Carolina, 3: Eomysticetidae, a new family of primitive mysticetes (Mammalia: Cetacea). Smithsonian Contributions to Paleobiology 93, 313–356.
Simpson, G.G., 1945. The principles of classification and a classification of mammals. Bulletin of the American Museum of Natural History 85, 1–350.
Slater, G.J., Price, S.A., Santini, F. & Alfaro, M.E., 2010. Diversity versus disparity and the radiation of modern cetaceans. Proceedings of the Royal Society B: Biological Sciences 277, 3097–3104.
Thewissen, J.G.M. & Bajpai, S., 2009. New skeletal material of Andrewsiphius and Kutchicetus, two Eocene cetaceans from India. Journal of Paleontology 83, 635–63.
Thewissen, J.G.M., Madar, S.I. & Hussain, S.T., 1996. Ambulocetus natans, an Eocene cetacean (Mammalia) from Pakistan. Courier Forschungsinstitut Senckenberg 191, 1–86.
Uhen, M.D., 2004. Form, function, and anatomy of Dorudon atrox (Mammalia, Cetacea): an archaeocete from the middle to late Eocene of Egypt. University of Michigan Papers in Paleontology 34, 1–222.
Uhen, M.D., 2009. Basilosaurids. In Perrin, W.F., Würsig, B. & Thewissen, J.G.M., eds, Encyclopedia of Marine Mammals 2nd edition. Academic Press, Sydney, 91–94.
Uhen, M.D., 2010. The origin(s) of whales. Annual Review of Earth and Planetary Sciences 38, 189–219.
Uhen, M.D., Pyenson, N.D., Devries, T.J., Urbina, M. & Renne, P.R., 2011. New Middle Eocene Whales From The Pisco Basin Of Peru. Journal of Paleontology, 85, 955–969.
Werth, A.J., 2000. Marine mammals. In, Schwenk, K., ed, Feeding: Form, Function and Evolution in Tetrapod Vertebrates. Academic Press, New York, 475–514.
Werth, A.J., 2006. Mandibular and dental variation and the evolution of suction feeding in Odontoceti. Journal of Mammalogy 87, 579–588.
Yamato, M., Ketten, D.R., Arruda, J., Cramer, S., Moore, K., 2012. The auditory anatomy of the minke whale (Balaenoptera acutorostrata): a potential fatty sound reception pathway in a baleen whale. Anatomical Record 295, 991–998.
Another post, another field trip! I’ve been quite fortunate so far this year, this trip was my third already and it’s only March (I think my fiancé has forgotten who I am)! In my defence though, this trip was only a short two night stay, with a day and a half worth of field work.
But enough already, where did I go? The locality we were digging at is known as Eric the Red West and it is situated on the southern coast of Victoria’s Otways ranges, around four hours west of Melbourne. The name of the site comes from a famous ship known as Eric the Red that wrecked there in 1880, whose anchor lies just east of our dig site, hence the Eric the Red West! The rocks at this locality are similar to those found at the site of my last field trip at Flat Rocks, Inverloch, which is on the other side of Melbourne. However the rocks in the Otways, although also Early Cretaceous, are around 10 million years younger than those found at Inverloch. They would have once been part of the same single unit but geological events in the Miocene have split them into two separate groups. The fossils found from the Otways are from the Eumarella Formation, Otways Group and the Flat Rocks fossils are from the Wonthaggi Formation, Strzelecki Group (Benson et al., 2012). This temporal difference between the two areas gives us a unique opportunity to study the evolution of life here in Victoria during the early Cretaceous as we can compare the two sites and look for differences in the flora and fauna.
Another bonus of a field trip to the Otways is the camp we get to stay in. Called Bimbi Park, it is situated right in the middle of the Otways Ranges National Park (so no Internet, hence the lateness of this blog post) where you are surrounded by trees full of Koalas, although at night when you’re trying to sleep and the males won’t stop bellowing they can lose their appeal momentarily! It really is a beautiful picturesque spot for getting away from it all and I’d definitely recommend it should you ever find yourself in that neck of the woods.
Tourism plugs aside, there have been several notable finds at the Eric the Red West site since it was first prospected in 2005 (Kool, 2010). There tends to be fewer finds at the Otways site, but the material is often of better quality than Flat Rocks. One of the best came on that very first day of prospecting when an articulated tail and complete right foot of a small ornithopod dinosaur was discovered. In 2006 Inverloch and Otways dig stalwart Mary Walters found a mammal jaw (not her first one either) and more recently, dig regular Alanna Maguire has found the first upper mammal jaw from the Cretaceous of Australia (something that is still being researched at present).
This field season is proving to be a very profitable one with the record for number of bones found in one day at the site being broken on the Monday I was there, and just prior to writing this post I read (via the Dinosaur Dreaming blog) that they had found two ornithopod jaws! There are some very exciting fossil layers being chased into the rock at present and hopefully they keep finding more cool stuff!
Now, where should I go for my next field trip…?
Benson, RBJ, Rich, TH, Vickers-Rich, P, Hall, M (2012) Theropod Fauna from Southern Australia Indicates High Polar Diversity and Climate-Driven Dinosaur Provinciality. PLOS One 7(5): e37122. doi:10.1371/journal.pone.0037122.
Australia has been separated from the rest of the world for the majority of the last 65 million years, with complete separation occurring around 30 million years ago. This has given the various forms of life on the continent plenty of time to evolve into their own unique groups. One particularly fascinating and enigmatic group is the family of extinct, giant flightless birds known as the dromornithids.
Australia today is famous for a group of flightless birds known as the emus; and for a long time the dromornithids were believed to be members of the same group of birds (the ratites). However, in 1998 a study by Murray and Megirian demonstrated that dromornithids are in fact neognathous birds in the Anseriformes. Nonetheless, it remains debatable as to which anseriform group is sister to the dromornithids (Murray & Vickers-Rich 2004, Olson 2005, Agnolin 2007). With a fossil record spanning around 25 million years, dromornithids are known from the late Oligocene through to the late Pleistocene (Field & Boles 1998, Nguyen et al. 2010). An ancient origin for the group is implied by a possible dromornithid foot impression from the early Eocene (approx. 50 million years ago) of Queensland (Vickers-Rich and Molnar 1996). Following an overdue taxonomic revision of the Dromornithidae (Nguyen et al. 2010), the family includes seven accepted species in four genera, with a geographic distribution including every state in Australia. The largest species, Dromornis stirtoni, is estimated to have stood at 3 m tall and weighed up to 500 kg, potentially even larger than the famous elephant bird of Madagascar.
There has been some debate as to whether the dromornithids were herbivorous or carnivorous, with features of the skull hinting at the potential for either way of life. Skull material is not known from every species however, and all members of the group may not have shared the same feeding ecology. Gizzard stones have been found in association with dromornithid remains, suggesting they needed the stones to help process plant material, although carnivores such as crocodiles are also known to possess them.
The dromornithids went extinct in the late Pleistocene and it is still unclear what combination of human hunting, landscape changing or climate change was the ultimate cause of their demise.
I have also had a personal interest in the dromornithids as myself and Dr. Erich Fitzgerald published a short paper on the Dromornithids last year (Park and Fitzgerald, 2012). In it we detailed the oldest known occurrence of the dromornithids in Victoria, a poorly preserved partial tarsometatarsus (one of the bones in the legs of birds). This bone appeared to represent a new species as it could not be referred to any of the known taxa elsewhere in Australia. Previously, the earliest known dromornithids in Victoria were from the late Pleistocene ( approx. 30,000 years ago) Lancefield Swamp locality, so this find pushes their presence in Victoria back in time considerably. It also cautions against deriving evolutionary patterns solely on the basis of fossils from northern Australia.
The dromornithids as a group still retain a lot of mystery and unanswered questions, and are long overdue for a thorough reanalysis. In fact, one of my colleagues plans to do exactly that over the next few years and I for one look forward to seeing what new details he can reveal about these ‘magnificent Mihirungs’.
AGNOLIN, F.L., 2007. Brontornis burmeisteri Moreno & Mercerat, un Anseriformes (Aves) gigante del Mioceno medio de
Patagonia, Argentina. Revista del Museo Argentino de Ciencias Naturales 9, 15–25.
FIELD, J.H. & BOLES, W.E., 1998. Genyornis newtoni and Dromaius novaehollandiae at 30,000 b.p. in central northern New South Wales. Alcheringa 22, 177–188.
MURRAY, P.F. & MEGIRIAN, D., 1998. The skull of dromornithid birds: anatomical evidence for their relationship to Anseriformes. Records of the South Australian Museum 31, 51–97.
MURRAY, P.F. & VICKERS-RICH, P., 2004. Magnificent Mihirungs: the Colossal Flightless Birds of the Australian Dreamtime. Indiana University Press, Bloomington, 410 pp.
NGUYEN, J.M.T., BOLES, W.E. & HAND, S.J., 2010. New material of Barawertornis tedfordi, a dromornithid bird from the Oligo- Miocene of Australia, and its phylogenetic implications. Records of the Australian Museum 62, 45–60.
OLSON, S.L., 2005. Review of Magnificent Mihirungs: the Colossal Flightless Birds of the Australian Dreamtime. The Auk 122, 367–371.
Travis Park & Erich M. G. Fitzgerald (2012): A late Miocene–early Pliocene Mihirung bird (Aves: Dromornithidae) from Victoria, southeast Australia, Alcheringa: An Australasian Journal of Palaeontology, 36:3, 419-422.
VICKERS-RICH, P. & MOLNAR, R.E., 1996. The foot of a bird from the Eocene Redbank Plains Formation of Queensland, Australia. Alcheringa 20, 21–29.
After an exciting end to my time in Christchurch I thought Dunedin might be the destination for a more relaxing few days. However the excitement began on the drive down to Dunedin! I was given a lift by Dr. Alan Tennyson, Curator of Vertebrates at Te Papa Museum in Wellington. On the way south from Christchurch we decided to take slight detour and head to Haugh’s quarry in the Hakataramea Valley to have a brief look around to see if we could spot any fossils. We spent about 90 minutes looking around and were about to get back in the truck to continue on to Dunedin when Alan said “let’s have a quick look around the top of the quarry”. We searched around there for a few minutes until Alan found a bit of bone exposed. We brushed a bit of sediment away, the bone kept going. We brushed more sediment away, the bone still kept going! After a few minutes more it became apparent that this was a seriously large animal, we had bone spread out along at least a two metre long strip and there was no sign of the end of it! It was a fossil whale of some description, though what exactly remains to be seen. We realised that we were not going to be able to excavate this fossil ourselves and we were already going to be late for the beginning of the conference, so we decided to take some photos of what we had uncovered and head on to Dunedin.
The next day we showed the images to Professor Ewan Fordyce, head of the Geology department at University of Otago and world-renowned authority on fossil whales. He was intrigued enough to want to go and excavate the fossil on Wednesday but then he received a phone call that two whales (Arnoux’s beaked whale or Berardius arnuxii) had stranded near Bluff, at the southern end of the island. He then invited me to come along on Wednesday and help dissect one of them! So I spent Wednesday covered in blood, guts and (when I helped to move the head) brains! Great fun!
When I wasn’t helping discover fossil whales or dissect dead extant ones, I also attended a few of the talks at the conference. Unfortunately there wasn’t as many palaeontology related talks as I had hoped, but it was more than made up for by the amount of research and field trips I got to go on. I managed to get lots of photos of the collections at University of Otago and Otago Museum. I also met a lot of new colleagues and (I hope) friends, one of whom, Bobby Boessenecker, has one of the best palaeontology blogs going.
Dunedin is a beautiful little city and is definitely worth a visit if the opportunity presents itself.
A big thank you goes to Ewan Fordyce for allowing access to his collections, taking time out of his busy schedule to talk with me and of course for letting me join in on the whale dissection.
Another big thank you goes to Alan Tennyson for driving me around everywhere as well as several interesting discussions.
And a massive thank you goes to Felix and Ikerne for letting me stay with them for the week, I look forward to returning the favour one day in Melbourne!
A great trip and I look froward to returning to New Zealand as soon as possible.
One of the best things about being a palaeontologist (even a student one) is getting to travel around the world to visit other museums, fossil sites and to attend conferences. At the moment I’m attending the 7th Southern Connections Congress 2013 in Dunedin on the South Island of New Zealand (planning to post about this at the end of the week). But since I was coming to New Zealand I thought I would include a trip to the Canterbury Museum in Christchurch to visit their collections and have a look around.
I’ve already mentioned in a previous post that the fossil record of penguins in Australia is somewhat fragmentary. There’s very few complete elements, let alone complete skeletons. New Zealand does not suffer this affliction too however, with some absolutely amazing specimens that I would kill for to have in Australia!
So when I spent two days last week in the collections of the Canterbury Museum, I was like the proverbial kid in the candy shop. There were some amazing penguin specimens and some very interesting cetacean specimens too. I took as many photographs as possible in the short time I had to build up my reference collection. It’s a lovely museum with beautiful botanical gardens and park right beside it, well worth a visit if you’re ever in that part of the world.
I couldn’t write something about Christchurch without mentioning the earthquake that struck on the 23rd February 2011, killing almost 200 people and destroying most of the CBD. When you see things like that on the news it’s almost impossible to comprehend the extent of the devastation of an event of that magnitude. But it was certainly brought home to me during my few days in Christchurch, even nearly two years after the earthquake. The CBD is still fenced off and out-of-bounds to the public and the city itself is effectively one big construction site, I’ve never experienced anything quite like it.
I was even given a brief reminder that the tectonic activity underneath Christchurch continues unabated. I was sitting in my room at the hostel I was staying in on Saturday night (I’m a party animal, I know) when the whole building began to shake! Fortunately it was a relatively weak quake and only lasted for around 10 seconds, but for those 10 seconds my heart rate increased rather rapidly!
But the city is rebuilding, and the feeling I got from the people I spoke to in Christchurch is that it will be stronger than ever when it is rebuilt. It is certainly worth visiting.
A big thanks goes to Dr. Paul Scofield for granting me access to the collections in Canterbury Museum and for the lunchtime beers!
Everybody loves penguins. From Happy Feet to the plethora of nature documentaries on the breeding cycle of the Emperor penguin, who can resist that awkward shuffle on land and the effortless grace in water? One facet of the penguin story that most people won’t be as familiar with is penguin palaeontology. This field has seen a renaissance since the early 1990’s with New Zealand and South America and Antarctica leading the way and South Africa also having their fair share of attention. One region that has been left out of this flurry of penguin research is Australia.
The published fossil record of penguins in Australia, although limited compared to that of Antarctica, New Zealand and South America, spans some 40 million years from the late Eocene to Recent (Ksepka and Ando, 2011). The majority of previous work has been produced by one author, none other than George Gaylord Simpson (Simpson, 1957, 1959, 1965, 1970), with the first publication released in 1938 (Finlayson, 1938) and the last primary research conducted by Van Tets and O’Connor (1983) a 30 year lull! A total of ten different localities are known from South Australia and Victoria (Park and Fitzgerald, 2012). In addition to numerous unidentifiable fragments, a total of five species have been named from the Australian material: Pachydyptes simpsoni (Eocene); Anthropodyptes gilli (Miocene); Pseudaptenodytes macraei (Miocene); Pseudaptenodytes minor (Miocene) and Tasidyptes hunteri (Holocene). Only two of these (A. gilli and P. macraei) are at present considered taxonomically distinct and only one species (P. simpsoni) is known from associated remains. All other species are based on individual and/or partial specimens, with the majority of specimens being too fragmentary for identification below the family level.
A new paper co-authored by myself and Dr. Erich Fitzgerald (senior curator of vertebrate palaeontology at Museum Victoria) reviews the fossil record of penguins in Australia. Whilst the record is undoubtedly fragmentary, material is known from every epoch since the Eocene and virtually every find up until now has been by chance. So the potential is there for new discoveries to be made, should actually someone go and specifically look for fossil penguins. Furthermore, material has continued to accumulate in museum collections over the past 30 years despite the lack of research, some of it worthy of further study (keep your eyes peeled later in the year for that). So consider this an unfinished story, the fossil penguins of Australia have a few more tales to tell.
Link to the paper: http://museumvictoria.com.au/pages/41623/momv-2012-vol-69-pp309-325.pdf
Finlayson, H. H. 1938. On the occurrence of a fossil penguin in Miocene beds in South Australia. Transactions of the Royal Society of South Australia 62:14–17.
Ksepka, D. T., and T. Ando. 2011. Penguins Past, Present, and Future: Trends in the Evolution of the Sphenisciformes; pp. 155–186 in G. Dyke, and G. Kaiser (eds.), Living Dinosaurs. The Evolutionary History of Modern Birds. Wiley-Blackwell, West Sussex.
Park, T., and E. M. G. Fitzgerald. 2012. A review of Australian fossil penguins (Aves: Sphenisciformes). Memoirs of Museum Victoria 69: 309–325
Simpson, G. G. 1957. Australian fossil penguins, with remarks on penguin evolution and distribution. Records of the South Australian Museum 13:51–70.
Simpson, G. G. 1959. A new fossil penguin from Australia. Proceedings of the Royal Society of Victoria 71:113–119.
Simpson, G. G. 1965. New record of a fossil penguin in Australia. Proceedings of the Royal Society of Victoria 79:91–93.
Simpson, G. G. 1970. Miocene penguins from Victoria, Australia, Chubut, Argentina. Memoirs of the National Museum, Victoria 31:17–24.
Van Tets, G. F., and S. O’Connor. 1983. The Hunter Island penguin, an extinct new genus and species from a Tasmanian midden. Records of the Queen Victoria Museum 81:1–13.