Abstract
Activity pattern, or the time of day when an animal is awake and active, is highly associated with that animal's ecology. There are two principal activity patterns: diurnal, or awake during the day in a photopic, or high light level, environment; and nocturnal, awake at night in scotopic, or low light level, conditions. Nocturnal and diurnal birds exhibit characteristic eye shapes associated with their activity pattern, with nocturnal bird eyes optimized for visual sensitivity with large corneal diameters relative to their eye axial lengths, and diurnal birds optimized for visual acuity, with larger axial lengths of the eye relative to their corneal diameters. The current study had three aims: (1) to quantify the nature of the relationship between the avian eye and its associated bony anatomy, the orbit and the sclerotic ring; (2) to investigate how activity pattern is reflected in that bony anatomy; and (3) to identify how much bony anatomy is required to interpret activity pattern reliably for a bird that does not have the soft tissue available for study, specifically, for a fossil. Knowledge of extinct avian activity patterns would be useful in making palaeoecological interpretations. Here eye, orbit and sclerotic ring morphologies of 140 nocturnal and diurnal bird species are analysed in a phylogenetic context. Although there is a close relationship between the avian eye and orbit, activity pattern can only be reliably interpreted for bony-only specimens, such as a fossil, that include both measurements of the sclerotic ring and orbit depth. Any missing data render the fossil analysis inaccurate, including fossil specimens that are flat and therefore do not have an orbit depth available. For example, activity pattern cannot be determined with confidence for Archaeopteryx lithographica, which has a complete sclerotic ring but no orbit depth measurement. Many of the bird fossils currently available that retain a good sclerotic ring tend to be flat specimens, while three-dimensionally preserved bird fossils tend not to have a well-preserved sclerotic ring or a well-defined optic foramen, necessary for delimiting the orbit depth.
Keywords: avian, diurnal, eye, fossil, nocturnal, orbit, sclerotic ring, vision
Introduction
Many aspects of an animal's life history are associated with activity pattern, the time of day when that animal is awake and active. There are two major activity patterns: diurnal, active during the day in a light-rich, or photopic, environment, and nocturnal, active after sunset in a light-limited, or scotopic, environment. ‘Scotopic’ and ‘nocturnal’ are interchangeable terms for the purposes of this study, as are ‘photopic’ and ‘diurnal’. Animals may also be crepuscular, active only during dawn and dusk, or cathemeral, equally likely to be active at any time of day. Previous studies on the eye suggest a common organizational principle of how activity pattern is reflected in eye shape: nocturnal birds have a larger corneal diameter relative to the axial length of the eye, probably as an adaptation for increased visual sensitivity to light, while diurnal birds exhibit a larger axial length of the eye relative to the corneal diameter (Hall, 2005; Hall & Ross, 2007; Ross et al. 2007), a shape correlated with increased visual acuity (Martin, 1982, 1990; Ross, 2000; Land & Nilsson, 2002).
Many bony structures are dependent on adjacent soft tissue to achieve their adult shapes, including muscular and other soft tissues. It is reasonable to expect eye size and shape to be correlated with the associated bony anatomy. The sense organs, including the eye, exert a mechanical influence on normal skull morphogenesis (Hanken, 1983; Thorgood, 1988; Hanken & Thorgood, 1993). When eye formation is disrupted in embryonic chicks (Columbre & Crelin, 1957; Tonneyckmuller, 1974; Vanlimborgh & Tonneyckmuller, 1976) and infant humans (Taylor, 1939; Moss & Young, 1960), orbit development is also disrupted. For example, when microphthalmia (a pathologically small optic globe) occurs naturally or is artificially induced, the orbital structure conforms to the reduced size of the eye, and general facial structure is malformed (Columbre & Crelin, 1957; Tonneyckmuller, 1974; Vanlimborgh & Tonneyckmuller, 1976).
Thus far, primates are the only group for which the relationship between the eye and orbit has been investigated. It has been shown that in small primates the eyeball fills a greater proportion of the orbit than in larger primates (Schultz, 1940). The relationships between activity pattern and bony anatomy have also been investigated in primates, and this information has been utilized for the interpretation of activity pattern for fossil primates. Kay & Cartmill (1977), in the context of an extant comparative base of similarly sized mammals, found that orbital aperture width relative to skull length separates nocturnal and diurnal primates with skull lengths of less than 70 mm. Kay & Kirk (2000) also demonstrated that at small body sizes nocturnal primates exhibit larger orbit diameters than diurnal primates. Heesy & Ross (2001) later showed that, for individuals with skull lengths less than or equal to 65 mm, orbital aperture size can be estimated accurately enough to reconstruct activity pattern in fossil primates from only 10 mm of the orbital rim and an upper molar.
For primates, as mammals, the only bony correlate of eye size and shape is the morphology of the orbit itself. In the absence of the eye, it is only possible to infer the size and shape of that portion of the eye that is directly contained within the orbit, and there is no apparent way to estimate how much of the eyeball protrudes from the bone. Additionally, because with increasing body size primate orbit volumes increase at a greater rate than eye volumes, at larger body sizes dimensions of the orbit do not accurately predict the size or shape of the eye (Schultz, 1940; Kay & Cartmill, 1977; Kay & Kirk, 2000; Heesy & Ross, 2001). Birds, however, like the great majority of diapsids, have an additional bony structure, the sclerotic ring, which houses that portion of the eye that is not contained within the orbit (see Fig. 1; Lemmrich, 1931; Proctor & Lynch, 1993). The sclerotic ring is a series of ossicles in the shape of a ring that is contained within the sclera of the eye, the inner diameter of which surrounds the corneal diameter (see Fig. 1). The exact structure of the sclerotic ring varies across birds in terms of length, degree of curvature, number of ossicles and thickness. It has been hypothesized that information about the soft tissue of the eye can be inferred from the dimensions of the sclerotic ring in ichthyosaurs (Motani et al. 1999; Humphries & Ruxton, 2002; Fernandez et al. 2005), in lizards (Rinehart et al. 2004; Hall, 2005) and in birds (Rowe, 2000; Rinehart et al. 2004). However, to date, the nature of the relationship between hard and soft tissue of the avian eye and orbit has not yet been quantified.
Unlike many mammals, the avian orbit does not contain a fat pad. The only muscles that are present within the orbit proper are the extraocular muscles (Proctor & Lynch, 1993; my personal observation). Although there are several jaw adductor muscles that attach to the ventral-most area of the orbit, these muscles are small and do not protrude significantly into the orbit (Proctor & Lynch, 1993; my personal observation). Therefore, the dimensions of both the orbit and the sclerotic ring may allow for interpretation of the size and shape of the eye when the soft tissue is unavailable for study, as is the case for fossil birds. As the size and shape of the avian eyeball is well correlated with activity pattern (Martin, 1990, 1999; Garamszegi et al. 2002; Hall, 2005; Hall & Ross, 2007; Ross et al. 2007), I hypothesize that the size and shape of the orbit and the sclerotic ring might also be correlated with activity pattern in birds, as has been previously shown to be the case for the eye and orbit in small-bodied primates.
There are three aims to the current study: (1) to quantify the nature of the relationship between the soft-tissue eye and the hard-tissue orbit and sclerotic ring in birds, (2) to investigate how activity pattern is reflected in the bony anatomy associated with the eye, and (3) to identify how much of the bony anatomy is required to interpret activity pattern reliably for a bird that does not have the soft tissue available for study, specifically, for a fossil. For example, Archaeopteryx lithographica is an early stem bird species and as such is of interest to many palaeontologists as part of the investigation into the ecological context of avian evolution. A. lithographica is not a crown taxon, and is therefore not suitable for Witmer's ‘first-order’ fossil interpretation, whereby a fossil structure can be most robustly interpreted when the fossil taxon is ‘bracketed’ by two extant species that exhibit the same bony structure and that has the same function in both bracketing species (Witmer, 1995). However, the Berlin specimen of A. lithographica retains a very well-preserved sclerotic ring, and there has been some discussion about whether palaeoecological and visual information can be interpreted on this basis (e.g. Rinehart et al. 2004). Most fossils, regardless of taxon, and regardless of age, have some missing data; A. lithographica exhibits all of the variables required by this study except one, orbit depth, and is here analysed in the context of the extant comparative database, to determine if there is a possibility for an activity pattern interpretation for a fossil with some missing data.
Materials and methods
Study animals
Data were collected on the eyeballs, orbits and sclerotic rings for 75 specimens of 60 non-passerine bird species (see Table 1). These data were supplemented by hard-tissue-only measurements of 131 specimens of 80 non-passerine bird species (see Table 1). Study groups included Strigiformes (barn owls and true owls), Psittaciformes (parrots), Columbiformes (pigeons), Apodiformes (swifts), Falconiformes (falcons), Accipitridrae (hawks), Caprimulgidae (nightjars), Aegothelidae (owlet-nightjars), Nyctibidae (potoos), Podargidae (frogmouths), Charadriiformes [shorebirds (hard tissue measurements only)], and three groups of ratites [ostriches, cassowaries (hard-tissue measurements only) and tinamous (hard-tissue measurements only)]. One fossil bird was included in this study, the Berlin specimen of A. lithographica, which has a complete sclerotic ring but no orbit depth. Specimens were obtained from the Departments of Ornithology of the American Museum of Natural History (New York), the Field Museum of Natural History (Chicago) and the British National Museum of Natural History (Tring, UK). A. lithographica was measured from a plaster cast at the National Museum of Natural History (Washington, DC). One frozen ostrich specimen was obtained from the Witmer Lab at Ohio University (Athens, OH). All of the other wet specimens were preserved in ethanol, and individuals exhibiting any pathology or unusual preservational deformation were excluded from this study.
Table 1.
Taxon | Activity pattern | n wet | n dry | Orbit depth | Orbit diameter | Sclerotic ring inner diameter | Sclerotic ring max. length | Axial sclerotic ring length | Corneal diameter | Axial length | Head length |
---|---|---|---|---|---|---|---|---|---|---|---|
Strigiformes | |||||||||||
Athene noctua* | photopic | 2 | 1 | 10.28 | 18.92 | 12.46 | 7.95 | 7.01 | 11.52 | 18.27 | 52.90 |
Athene brama* | photopic | 2 | 7.30 | 18.90 | 10.99 | 7.23 | 5.71 | 10.92 | 17.11 | 46.75 | |
Glaucidium brasilianum* | photopic | 1 | 1 | 8.57 | 19.73 | 11.95 | 8.26 | 7.54 | 11.44 | 18.05 | 47.73 |
Glaucidium perlatum | photopic | 1 | 7.89 | 16.99 | 10.97 | 7.63 | 6.82 | 10.97 | 16.80 | 31.38 | |
Glaucidium jardinii | photopic | 1 | 6.38 | 14.55 | 7.91 | 6.73 | 5.90 | 7.91 | 11.92 | 27.74 | |
Glaucidium tephronatum | photopic | 1 | 8.69 | 15.54 | 8.99 | 5.24 | 30.04 | ||||
Bubo africanus | scotopic | 2 | 15.64 | 29.28 | 20.19 | 14.19 | 14.11 | 17.58 | 23.03 | 43.86 | |
Bubo bubo* | scotopic | 1 | 21.86 | 35.58 | 23.23 | 19.14 | 17.80 | 20.15 | 33.95 | 61.23 | |
Bubo virginianus* | scotopic | 4 | 18.39 | 38.61 | 23.49 | 18.62 | 17.93 | 57.08 | |||
Strix aluco | scotopic | 2 | 3 | 16.17 | 25.25 | 17.80 | 12.94 | 12.16 | 15.35 | 24.96 | 67.01 |
Strix varia* | scotopic | 4 | 13.49 | 29.40 | 17.24 | 11.49 | 9.90 | 47.56 | |||
Strix occidentalis | scotopic | 1 | 14.28 | 29.65 | 18.52 | 11.58 | 10.09 | 48.66 | |||
Nyctea scandiaca* | photopic | 1 | 19.91 | 32.29 | 21.33 | 19.87 | 18.58 | 56.02 | |||
Otus scops* | scotopic | 2 | 8.00 | 16.76 | 10.94 | 6.48 | 5.75 | 9.86 | 13.78 | 41.42 | |
Otus asio* | scotopic | 1 | 1 | 9.59 | 22.75 | 14.42 | 10.83 | 9.85 | 13.76 | 20.04 | 46.01 |
Otus rutilis | scotopic | 1 | 8.77 | 19.22 | 12.72 | 8.50 | 7.61 | 12.72 | 17.24 | 32.39 | |
Otus longicornis | scotopic | 1 | 8.00 | 19.59 | 11.78 | 8.33 | 7.58 | 11.78 | 17.89 | 29.21 | |
Tyto alba* | scotopic | 5 | 4 | 10.62 | 18.67 | 12.01 | 7.21 | 7.13 | 11.24 | 17.80 | 63.90 |
Asio flammeus | scotopic | 3 | 9.39 | 19.70 | 12.41 | 6.97 | 60.30 | ||||
Asio otus | scotopic | 3 | 10.01 | 19.61 | 13.18 | 5.86 | 5.33 | 60.42 | |||
Ketupa ketupa | scotopic | 1 | 15.59 | 29.65 | 16.62 | 11.48 | 9.64 | 47.47 | |||
Ketupa zeylonensis | scotopic | 1 | 16.26 | 32.95 | 20.07 | 11.55 | 9.39 | 50.19 | |||
Scotopelia peli | scotopic | 1 | 21.27 | 34.41 | 22.68 | 12.72 | 6.76 | 102.62 | |||
Surnia ulula* | scotopic | 1 | 14.24 | 21.95 | 12.13 | 8.59 | 40.03 | ||||
Podargidae | |||||||||||
Podargus strigoides* | scotopic | 1 | 1 | 18.43 | 25.40 | 15.06 | 9.73 | 6.40 | 14.11 | 20.23 | 71.34 |
Aegothelidae | |||||||||||
Aegotheles insignis* | scotopic | 1 | 3.37 | 13.66 | 8.06 | 4.93 | 8.09 | 9.27 | 21.87 | ||
Nyctibidae | |||||||||||
Nyctibius griseus* | scotopic | 1 | 11.26 | 24.21 | 17.48 | 5.93 | 5.28 | 17.48 | 19.24 | 34.35 | |
Caprimulgidae | |||||||||||
Caprimulgus europaeus* | scotopic | 1 | 1 | 7.04 | 13.85 | 10.71 | 3.38 | 2.96 | 9.77 | 12.06 | 38.86 |
Caprimulgus macrurus* | scotopic | 1 | 1 | 5.88 | 15.50 | 10.61 | 2.97 | 2.20 | 10.61 | 12.95 | 34.06 |
Caprimulgus madagascariensis | scotopic | 1 | 7.90 | 14.11 | 9.02 | 3.36 | 2.54 | 9.02 | 11.42 | 23.55 | |
Caprimulgus pectoralis | scotopic | 1 | 6.16 | 14.36 | 8.26 | 2.91 | 1.60 | 39.84 | |||
Macrodiperyx vexillaria | scotopic | 1 | 8.39 | 16.25 | 10.41 | 2.27 | 1.81 | 39.67 | |||
Panyptila sanctiheironymi | scotopic | 1 | 5.41 | 13.05 | 6.13 | 2.02 | 1.45 | 34.18 | |||
Uropsalis segmentata | scotopic | 1 | 4.71 | 13.96 | 10.75 | 3.28 | 3.05 | 10.75 | 11.85 | 22.16 | |
Eurostopodus macrotis | scotopic | 1 | 11.98 | 20.42 | 13.99 | 5.58 | 4.42 | 13.99 | 18.41 | 27.71 | |
Hydropsalis climacocerca | scotopic | 1 | 5.72 | 11.91 | 7.77 | 2.97 | 2.35 | 7.77 | 9.58 | 20.02 | |
Nyctidromus albicollis* | scotopic | 1 | 5.56 | 14.96 | 10.68 | 3.71 | 3.14 | 10.68 | 12.25 | 25.86 | |
Scotornis climacurus | scotopic | 1 | 6.45 | 12.80 | . | 2.94 | 0.00 | 12.36 | 20.09 | ||
Podager nacunda* | scotopic | 1 | 9.35 | 18.84 | 12.20 | 4.99 | 3.73 | 12.20 | 14.64 | 27.63 | |
Nyctiphyrnus ocellatus | scotopic | 1 | 6.23 | 14.80 | 8.54 | 3.64 | 2.93 | 8.54 | 10.33 | 23.17 | |
Falconiformes | |||||||||||
Falco sparverius* | photopic | 1 | 3 | 9.11 | 15.42 | 8.20 | 5.18 | 1.68 | 8.20 | 11.98 | 35.85 |
Ictina plumbea | photopic | 1 | 13.84 | 18.87 | 9.08 | 6.64 | 4.79 | 9.08 | 16.81 | 37.14 | |
Polyborus plancus | photopic | 3 | 18.28 | 26.90 | 10.00 | 4.34 | 1.30 | 37.14 | |||
Falco columbarius | photopic | 3 | 16.62 | 16.28 | 9.78 | 2.46 | 44.74 | ||||
Falco mexicanus | photopic | 1 | 21.69 | 25.20 | 13.84 | 5.29 | 3.54 | 70.45 | |||
Falco ruficolus | photopic | 2 | 22.39 | 27.01 | 22.59 | 6.19 | 82.31 | ||||
Micrastur glivicollis* | photopic | 1 | 18.16 | 20.12 | 11.26 | 4.75 | 3.26 | 54.75 | |||
Micrastur semitorquatus | photopic | 1 | 22.25 | 27.66 | 13.52 | 5.40 | 3.18 | 70.56 | |||
Microheriax caerulescens* | photopic | 2 | 9.34 | 11.77 | 5.84 | 2.14 | 1.23 | 29.94 | |||
Sagittarius serpentarius* | photopic | 1 | 27.46 | 35.52 | 12.60 | 5.84 | 66.36 | ||||
Accipidrae | |||||||||||
Accipiter francesi | photopic | 1 | 11.26 | 17.75 | 9.76 | 7.93 | 6.94 | 9.76 | 15.08 | 32.58 | |
Buteo buteo* | photopic | 2 | 17.77 | 23.24 | 14.71 | 7.63 | 50.55 | ||||
Buteo jamaicensis* | photopic | 2 | 19.83 | 29.71 | 16.11 | 9.60 | 55.87 | ||||
Aquila chrysaetos* | photopic | 1 | 24.89 | 38.01 | 19.77 | 9.67 | 68.18 | ||||
Accipiter cooperi* | photopic | 2 | 11.76 | 21.80 | 10.99 | 4.73 | 40.61 | ||||
Apodiformes | |||||||||||
Collocalia fuciphaga | photopic | 2 | 4.14 | 10.11 | 6.05 | 4.71 | 4.38 | 4.69 | 8.68 | 24.06 | |
Collocalia esculenta* | photopic | 3 | 4.09 | 7.14 | 4.37 | 2.73 | 2.24 | 3.91 | 5.92 | 20.43 | |
Collocalia brevirostris | photopic | 1 | 4.38 | 9.55 | 4.55 | 2.68 | 4.55 | 7.17 | 14.88 | ||
Apus apus* | photopic | 2 | 6.45 | 11.93 | 6.54 | 3.64 | 2.49 | 5.05 | 9.96 | 30.48 | |
Apus barbatus* | photopic | 1 | 5.98 | 11.99 | 6.40 | 4.35 | 3.39 | 6.40 | 10.00 | 21.33 | |
Cypsiurius parvus* | photopic | 3 | 4.29 | 9.12 | 5.25 | 4.89 | 2.66 | 4.64 | 7.59 | 21.16 | |
Cypseloides rutilus | photopic | 1 | 5.53 | 10.84 | 5.08 | 3.97 | 2.95 | 5.08 | 8.34 | 16.15 | |
Cypseloides phelpsi | photopic | 1 | 1 | 5.84 | 11.40 | 5.18 | 4.48 | 3.69 | 5.18 | 8.26 | 19.25 |
Thalurania glaucopis | photopic | 1 | 3.70 | 5.68 | 2.65 | 1.41 | 0.69 | 2.65 | 3.37 | 11.34 | |
Chaetura brachyura* | photopic | 1 | 5.62 | 10.21 | 4.78 | 4.29 | 3.03 | 4.78 | 7.02 | 17.69 | |
Chaetura cinereiventris | photopic | 1 | 2.34 | 6.19 | 4.01 | 1.75 | 1.50 | 21.51 | |||
Chaetura pelagica | photopic | 1 | 7.01 | 10.84 | 4.43 | 2.25 | 1.61 | 26.79 | |||
Campylopterus duidae | photopic | 1 | 4.36 | 6.37 | 1.92 | 1.92 | 1.29 | 2.82 | 4.56 | 13.27 | |
Heledoya branickii | photopic | 1 | 3.07 | 6.13 | 3.08 | 1.12 | 0.00 | 3.08 | 4.45 | 11.48 | |
Telacanthura ussheri | photopic | 1 | 5.44 | 10.11 | 5.79 | 3.35 | 2.52 | 5.79 | 8.44 | 20.83 | |
Psittaciformes | |||||||||||
Pionus menstruus* | photopic | 1 | 1 | 11.79 | 15.98 | 7.57 | 4.40 | 1.10 | 7.52 | 10.57 | 46.12 |
Deroptyus accipitrinus* | photopic | 1 | 13.84 | 17.10 | 7.22 | 5.15 | 2.59 | 7.22 | 13.34 | 47.51 | |
Poicephalus senagalus* | photopic | 1 | 8.85 | 13.96 | 6.65 | 3.91 | 2.71 | 6.65 | 10.90 | 38.02 | |
Pyrrhyra rhodogaster | photopic | 1 | 7.05 | 12.09 | 5.55 | 2.64 | 0.60 | 5.55 | 7.98 | 33.84 | |
Polytelis alexandriae* | photopic | 1 | 7.09 | 12.64 | 5.44 | 3.02 | 1.41 | 5.44 | 7.74 | 31.78 | |
Rychpsutta pachyryncha | photopic | 1 | 10.50 | 14.28 | 7.68 | 3.72 | 2.45 | 7.68 | 9.57 | 51.09 | |
Aratinga weddellii | photopic | 1 | 6.74 | 12.92 | 6.08 | 3.54 | 2.17 | 6.08 | 8.59 | 33.36 | |
Chalcopsitta atra | photopic | 1 | 7.32 | 13.70 | 6.23 | 3.79 | 2.27 | 6.23 | 10.26 | 41.87 | |
Loriculus galgulus | photopic | 1 | 6.13 | 9.31 | 4.40 | 0.78 | 0.00 | 29.49 | |||
Psittacus erithacus timni | photopic | 1 | 11.11 | 16.72 | 7.88 | 0.95 | 0.00 | 57.94 | |||
Poicephalus senegalus* | photopic | 1 | 9.67 | 14.47 | 6.17 | 1.53 | 0.00 | 46.00 | |||
Psittacuse erithacus | photopic | 1 | 12.43 | 18.34 | 7.48 | 1.72 | 0.00 | 65.66 | |||
Poicephalus cryptoxanthus | photopic | 1 | 6.64 | 14.74 | 6.19 | 1.49 | 0.00 | 43.57 | |||
Agapornis canus* | photopic | 1 | 4.70 | 8.31 | 3.32 | 0.77 | 0.00 | 29.00 | |||
Loriculus philippensis | photopic | 1 | 6.11 | 9.54 | 4.86 | 0.58 | 0.00 | 32.48 | |||
Psittacula alexandri fasciata | photopic | 1 | 9.03 | 13.13 | 6.15 | 1.47 | 0.00 | 47.40 | |||
Agapornis nigrensis | photopic | 1 | 5.60 | 8.13 | 3.64 | 0.67 | 0.00 | 30.98 | |||
Agapornis personata | photopic | 1 | 5.12 | 10.65 | 4.65 | 1.06 | 0.00 | 33.45 | |||
Agapornis roseicollis | photopic | 1 | 5.74 | 9.94 | 4.80 | 0.68 | 0.00 | 33.53 | |||
Psittacula krameri* | photopic | 1 | 8.18 | 13.76 | 5.95 | 0.74 | 0.00 | 40.84 | |||
Psittacula roseata | photopic | 1 | 7.67 | 9.91 | 5.26 | 0.59 | 0.00 | 36.12 | |||
Agapornis taranta | photopic | 1 | 6.30 | 10.54 | 4.27 | 1.08 | 0.00 | 34.74 | |||
Anodorynchus glaucus | photopic | 1 | 16.08 | 23.20 | 9.17 | 1.78 | 0.00 | 85.56 | |||
Graydidascalus brachyurus | photopic | 1 | 11.34 | 13.34 | 7.20 | 1.35 | 0.00 | 99.12 | |||
Pionus sordidus | photopic | 1 | 12.53 | 14.89 | 6.65 | 1.71 | 0.00 | 50.12 | |||
Pionites leucogaster | photopic | 1 | 12.38 | 14.07 | 7.19 | 1.72 | 0.00 | 50.38 | |||
Aratinga erythrogenys | photopic | 1 | 13.05 | 14.76 | 7.00 | 0.88 | 0.00 | 48.43 | |||
Nondayus nenday | photopic | 1 | 9.16 | 12.56 | 6.14 | 0.96 | 0.00 | 46.70 | |||
Bolborynchus aurifrons | photopic | 1 | 5.54 | 8.76 | 4.32 | 0.69 | 0.00 | 29.79 | |||
Aratinga leucopthalmus* | photopic | 1 | 11.38 | 14.44 | 6.45 | 1.19 | 0.00 | 51.39 | |||
Myopsitta monachus | photopic | 1 | 7.91 | 10.96 | 4.94 | 1.14 | 0.00 | 38.09 | |||
Pezoporus wallicus* | scotopic | 1 | 7.94 | 13.33 | 6.85 | 2.47 | 2.05 | 26.89 | |||
Columbiformes | |||||||||||
Turtur afer* | photopic | 1 | 6.47 | 12.84 | 5.01 | 3.47 | 2.06 | 5.01 | 8.28 | 23.46 | |
Gallicolumba luzonica* | photopic | 1 | 7.54 | 14.32 | 6.22 | 3.20 | 0.00 | 6.22 | 7.30 | 28.75 | |
Lepitola verreauxi* | photopic | 1 | 9.82 | 14.62 | 5.98 | 4.61 | 2.92 | 5.98 | 9.84 | 32.01 | |
Geotrygon montana* | photopic | 1 | 6.41 | 12.65 | 5.69 | 3.25 | 5.69 | 8.87 | 26.01 | ||
Treron vernans | photopic | 1 | 8.14 | 13.73 | 5.76 | 3.59 | 2.43 | 5.76 | 8.33 | 28.98 | |
Chalcops indica | photopic | 1 | 2 | 7.99 | 13.53 | 6.23 | 3.29 | 1.18 | 6.23 | 8.87 | 25.66 |
Streptopelia chinensis | photopic | 1 | 6.77 | 13.74 | 5.35 | 3.65 | 1.96 | 5.35 | 8.83 | 24.82 | |
Pterocles cornata | photopic | 1 | 6.28 | 13.85 | 6.73 | 4.03 | 2.67 | 6.73 | 10.46 | 29.61 | |
Columba plumbea* | photopic | 1 | 7.09 | 13.44 | 6.24 | 3.94 | 2.28 | 6.24 | 9.39 | 30.72 | |
Streptopelia vinacea* | photopic | 1 | 6.43 | 12.84 | 6.07 | 2.01 | 0.92 | 26.48 | |||
Leucosarcia melanoleuca | photopic | 1 | 10.73 | 16.26 | 7.95 | 2.71 | 1.68 | 32.04 | |||
Zenaiela asiatica | photopic | 1 | 6.79 | 13.64 | 6.97 | 2.39 | 1.35 | 29.70 | |||
Ptilinopus aurantiif | photopic | 1 | 8.51 | 13.66 | 6.90 | 1.93 | 0.55 | 30.24 | |||
Zenaida macroura | photopic | 1 | 5.40 | 13.30 | 6.55 | 2.03 | 1.28 | 26.91 | |||
Petrophassa plumifer | photopic | 1 | 5.92 | 12.43 | 5.16 | 2.12 | 1.28 | 23.98 | |||
Ocyphaps lophotes | photopic | 1 | 8.11 | 14.39 | 6.44 | 2.08 | 1.32 | 28.71 | |||
Goura victoria | photopic | 1 | 13.19 | 23.76 | 10.68 | 4.62 | 3.24 | 47.55 | |||
Struthioniformes | |||||||||||
Struthio camellus | photopic | 1 | 2 | 39.30 | 47.19 | 26.41 | 8.15 | 6.17 | 11.53 | 38.00 | 94.40 |
Casuariiformes | |||||||||||
Casuariius sp.* | photopic | 1 | 31.60 | 19.61 | 7.28 | 120.12 | |||||
Tinamiformes | |||||||||||
Eudromia elegans | photopic | 1 | 6.24 | 16.77 | 8.25 | 3.75 | 2.60 | 33.25 | |||
Nothoprocta ornata* | photopic | 1 | 7.68 | 14.35 | 7.25 | 3.13 | 1.78 | 29.93 | |||
Crypturellus tataupa | photopic | 1 | 7.10 | 12.19 | 5.27 | 2.59 | 0.81 | 24.90 | |||
Crypturellus noctivagus | photopic | 1 | 9.94 | 17.57 | 9.25 | 3.89 | 3.09 | 34.70 | |||
Charadriiformes | |||||||||||
Scolopax minor | photopic | 2 | 7.95 | 14.20 | 9.03 | 2.36 | 1.41 | 27.09 | |||
Scolopax rusticola | scotopic | 2 | 10.27 | 16.39 | 9.80 | 2.38 | 1.38 | 29.43 | |||
Gallinago gallinago | scotopic | 2 | 4.89 | 10.84 | 5.99 | 1.52 | 1.26 | 22.71 | |||
Vanellus tricolor* | photopic | 2 | 8.75 | 16.88 | 7.95 | 3.22 | 2.30 | 29.15 | |||
Pluvalis dominica | photopic | 3 | 5.73 | 16.41 | 8.49 | 2.51 | 2.55 | 28.07 | |||
Numenius phaeopus hudsonicus | photopic | 2 | 6.71 | 16.79 | 7.45 | 3.40 | 1.95 | 34.94 | |||
Charadrius melodus | photopic | 1 | 5.28 | 12.30 | 6.66 | 2.31 | 1.84 | 21.66 | |||
Charadrius vociferus* | photopic | 3 | 6.54 | 14.36 | 7.47 | 2.27 | 1.80 | 25.15 | |||
Burhinus oedicnemus | scotopic | 1 | 8.91 | 22.38 | 12.81 | 4.96 | 3.80 | 38.38 | |||
Burhinus bistratus* | scotopic | 1 | 19.26 | 27.15 | 15.95 | 5.35 | 4.50 | 45.94 | |||
Burhinus capensis | scotopic | 1 | 16.43 | 25.67 | 15.28 | 4.65 | 3.67 | 41.19 | |||
Burhinus magnirostris | scotopic | 2 | 17.08 | 26.46 | 16.27 | 4.56 | 4.88 | 46.39 | |||
Haematops palliatus* | photopic | 1 | 8.99 | 19.02 | 9.81 | 3.52 | 3.02 | 33.55 |
Included in the phylogeny for phylogenetic independent contrasts.
Raw data for eye dimensions and related hard-tissue variables. All birds were coded for activity pattern from the literature as follows: (1) König et al. (1999) and del Hoyo et al. (2000); (2) Cleere & Nurney (1998); (3) Ferguson-Lees & Christie (2001); (4) Chantler & Driessens (1995); (5) Juniper & Parr (1998); (6) del Hoyo et al. (1997); (7) del Hoyo et al. (1992); (8) del Hoyo et al. (1996). For axial sclerotic ring length measurements, if the cell is blank, the measurement is not present; if ‘0’ is indicated, the sclerotic ring is flat and therefore no length can be calculated.
Measurements
Soft tissue
Measurements follow Ritland (1982) and Hall & Ross (2007) as follows. For alcohol-preserved specimens, in order to gain access to the eyeball, the eyelid was reflected or removed and the eye was removed from the orbit via blunt dissection using closed, curved scissors and forceps to preserve the eye from accidental puncture. After removal from the orbit, the eyeball was cleaned of all extraocular muscles and remaining fascia, and was inflated using a small amount of preservative injected by a syringe inserted on an angle into the sclera just inferior to the outer edge of the sclerotic ring. Preservative was injected until the eye was fully inflated and would not accept any additional liquid. At that point, maximum corneal diameters and maximum axial lengths of the eye were measured with digital calipers to 0.01 mm. For many of the larger specimens, this required several injections, in which case care was taken to utilize the same puncture hole each time. Any eye that could not be fully inflated was not measured.
Hard tissue
In wet specimens, the orbit was cleaned of fascia and extraocular muscles to allow for clear identification of all bony landmarks. Otherwise, measurements of hard tissue were identical in wet specimens and in dry skulls.
The sclerotic ring cannot be separated from the eye in wet specimens, but in prepared skulls the sclerotic ring is a separate structure from the rest of the skull and is therefore measured independently. All measurements were taken with digital calipers to the nearest 0.01 mm (see Fig. 1). Maximum supero-inferior orbital diameter was measured from the dorsal frontal bone to the quadratojugal. Orbit depth was measured using the depth gauge of the digital calipers from the position of the maximum orbital diameter to the optic foramen (see Fig. 2). If the specimen was too large for the distal end of the calipers to span the orbital diameter, a ruler was placed in the position of the maximum orbital diameter, and the orbit depth was measured from the midpoint of the ruler to the optic foramen. The thickness of the ruler was subtracted from the depth measurement. Head length was measured from the centrepoint of the junction of the beak and skull to inion (posteriormost point on the skull). On the sclerotic ring, maximum inner diameter, maximum outer diameter and maximum length were measured. In most birds the maximum length of the sclerotic ring is obliquely orientated to the visual axis of the eye and therefore may not accurately measure that portion of the axial length of the eye that is housed by the sclerotic ring. Therefore, an additional measurement of sclerotic ring length that is orientated along the axial length of the eye was calculated by treating the maximum length of the sclerotic ring as the hypoteneuse of a right-angled triangle, and half the difference between the outer and inner diameters of the sclerotic ring as the base of this triange. Pythagoras’ theorem was then utilized to solve for the other side of the triangle, and the result was termed the ‘axial sclerotic ring length’ because it is the measurement of the sclerotic ring length that is along the axial length of the eye (Fig. 1).
The Berlin specimen of A. lithographica is contained within a flat slab and is two-dimensional. Therefore, orbit depth was not available, but all other hard-tissue measurements were recorded.
Data analysis
Standard statistical analysis
In order to quantify the relationship between hard and soft tissue in the avian eye and orbit, regressions were calculated to determine the strength of the relationship between the (1) corneal diameter and two bony correlates: (a) the inner diameter of the sclerotic ring and (b) the orbit diameter; and (2) the axial length of the eye with five bony correlates: (a) orbit depth, (b) maximum length of the sclerotic ring, (c) axial sclerotic ring length, (d) the orbit depth added to the maximum length of the sclerotic ring, and (e) the orbit depth added to the axial sclerotic ring length.
In order to quantify the relationship between hard tissue and activity pattern, initially each bird species included in this study was categorized by activity pattern from the literature (del Hoyo et al. 1992, 1996, 1997, 2000; Chantler & Driessens, 1995; Cleere & Nurney, 1998; Juniper & Parr, 1998; König et al. 1999; Ferguson-Lees & Christie, 2001). All animals were classified as either nocturnal or diurnal; there are no cathemeral or crepuscular animals included in this study. The inner diameter of the sclerotic ring, the bony correlate of corneal diameter, was then regressed against each of the five bony correlates for the axial length of the eye (orbit depth, maximum sclerotic ring length, axial sclerotic ring length, the orbit depth added to the maximum length of the sclerotic ring, and the orbit depth added to the axial sclerotic ring length) to investigate the nature of the relationship between the variables. Because the nature of the relationship between orbit diameter and head length has been shown to be useful for interpreting activity pattern in primates (Kay & Cartmill, 1977; Heesy & Ross, 2001), this relationship was also quantified in avians. Inner diameter of the sclerotic ring was then also regressed against head length; for mammals, orbit diameter is the only bony correlate of corneal diameter, but in avians, the inner diameter of the sclerotic ring is a significantly closer bony correlate of corneal diameter, and this measurement may be more useful than orbit diameter in interpreting avian activity pattern.
Because measurement error and natural variation affect both dependent and independent variables, reduced major axis (RMA) was the Model II line-fitting technique utilized in the present study; this method does not assume that variance in either variable is more significant, or that one is influencing the other (Ricker, 1984; Rayner, 1985; Plotnick, 1989; Sokal & Rohlf, 1995). Initially, a single RMA line was calculated for each regression, residuals were calculated from that line for all birds plotted, and a one-way anova was calculated comparing nocturnal and diurnal birds. Then, for each pair of variables, two RMA lines were calculated, one for diurnal birds and one for nocturnal birds. The regression lines were then tested for homogeneity, and then analysis of covariance (ancova) was used to interpret differences in elevation for the activity patterns (Sokal & Rohlf, 1995). The two techniques were utilized for two reasons: first, to confirm the ancova results for differences between groups and, second, to compare differences between nocturnal and diurnal animals in situations where the individual nocturnal and diurnal RMA slopes were not homogeneous and therefore not appropriate for ancova analysis to interpret elevational differences between nocturnal and diurnal birds.
Eight one-way anovas were calculated to determine if there was a significant difference between the activity patterns for the single hard-tissue variables, including (1) log10 inner diameter of the sclerotic ring, (2) log10sclerotic ring maximum length, (3) log10axial sclerotic ring length, (4) log10 orbit depth, (5) log10 orbit diameter, (6) log10 (orbit depth + maximum sclerotic ring length), (7) log10 (orbit depth + axial sclerotic ring length), and (8) log10 shape ratio of the inner diameter of the sclerotic ring (the bony correlate of corneal diameter) versus orbit depth + sclerotic ring length (a bony correlate of the axial length of the eye). This ratio allows for an examination of the shape of the orbit and sclerotic ring without the influence of size. In order to ensure that the ratio has no remaining relationship with size, the ratio was regressed against head length, the body size variable that was available for all the animals in this study.
Interquartile boxplots were generated for each variable to display the differences between the means and ranges of each activity pattern. Residuals were calculated in Excel, scatter plots, boxplots and anovas were calculated in SPSS 8.0 (Chicago, IL, USA), and regressions and ancovas were calculated in SMATR (Falster et al. 2003).
After all analyses were completed, the measurement values for A. lithographica were plotted on all scatter graphs and boxplots that did not involve orbit depth, the one measurement that was not available for the fossil. This was done to compare the fossil with extant animals of known activity pattern to determine if its activity pattern can be interpreted.
Phylogenetic comparative methods
Standard statistical methods assume independent data observations (Sokal & Rohlf, 1995). However, a common character observed in closely related animals may not be independent. Therefore, in order to take phylogeny into account, this study utilizes independent contrast analysis (Felsenstein, 1985; Harvey & Pagel, 1991), performed in the PDAP module of Mesquite (Maddison & Maddison, 2003; Midford et al. 2005). Currently, avian phylogenetic relationships are highly debated and there is no single commonly accepted phylogeny that includes all the animals in this study. Therefore, individual lower taxonomic-level trees were compiled from individual group phylogenies in Iwaniuk (2003), updated by several more recent lower taxonomic-level molecular phylogenies (Dumbacher et al. 2003; Garcia-Moreno et al. 2003; Paton et al. 2003; Thimassen et al. 2003; Poe & Chubb, 2004; Thomas et al. 2004). Of the 140 species included in the present study, it was possible to find group phylogenies that included 45. Whenever more than one possible cladogram was presented in a systematic analysis, the more resolved tree was always chosen. These individual composite lower-level group phylogenies were then assembled into three different large-scale composite phylogenies using Mesquite (Maddison & Maddison, 2003), including one each that reflects the inter-ordinal relationships from Cracraft et al. (2004), Ericson et al. (2006) and Livezey & Zusi (2007). However, even utilizing the best-resolved trees available, some polytomies in the final trees were unavoidable (see supplementary Fig. S1). There is at present contradictory evidence for branch lengths from the fossil record, molecular clock studies and from biogeography (reviewed in Cracraft, 2000; see also Graur & Martin, 2004). However, branch lengths can affect computations of node values in independent contrast analyses and therefore cannot be ignored. Therefore, in this analysis, branch lengths were both set to 1, and also were recalculated in Mesquite following Grafen (1989) and Pagel (1992), as per Blomberg et al. (2003). Contrasts calculated with these different branch lengths was evaluated for the appropriate fit to the tip data following Díaz-Uriarte & Garland (1998).
Results
The vertebrate eye generally scales with negative allometry to body size (Ritland, 1982; Kiltie, 2000; Hall, 2005, 2008; Ross et al. 2007; Hall & Ross, 2007). However, in the present study, the bony correlates of axial length of the eye (orbit depth, sclerotic ring length and the two variables summed together) scaled nearly isometrically with head length (see Table 2). Orbit diameter and head length scaled with negative allometry, but the inner diameter of the sclerotic ring and head length scaled with positive allometry (see Table 2).
Table 2.
Activity pattern | Y-variable | X-variable | RMA slope | CI | r2 | Significant ancova? |
---|---|---|---|---|---|---|
scotopic | inner diameter sclerotic ring | orbit depth + sclerotic ring length | 0.717 | 0.634–0.811 | 0.858 | yes |
photopic | inner diameter sclerotic ring | orbit depth + sclerotic ring length | 0.975 | 0.852–1.114 | 0.551 | yes |
scotopic | inner diameter sclerotic ring | orbit depth + axial sclerotic ring length | 0.451 | 0.356–0.571 | 0.474 | slopes not homogeneous |
photopic | inner diameter sclerotic ring | orbit depth + axial sclerotic ring length | 0.724 | 0.603–0.87 | 0.243 | slopes not homogeneous |
scotopic | inner diameter sclerotic ring | sclerotic ring length | 0.548 | 0.466–0.646 | 0.75 | slopes not homogeneous |
photopic | inner diameter sclerotic ring | sclerotic ring length | 0.651 | 0.552–0.766 | 0.329 | slopes not homogeneous |
scotopic | inner diameter sclerotic ring | axial sclerotic ring length | 0.443 | 0.371–0.528 | 0.709 | slopes not homogeneous |
photopic | inner diameter sclerotic ring | axial sclerotic ring length | 0.606 | 0.794–1.069 | 0.284 | slopes not homogeneous |
scotopic | inner diameter sclerotic ring | orbit depth | 0.753 | 0.638–0.890 | 0.741 | slopes not homogeneous |
photopic | inner diameter sclerotic ring | orbit depth | 0.751 | 0.794–1.069 | 0.448 | slopes not homogeneous |
scotopic | orbit diameter | orbit depth | 0.71 | 0.619–0.815 | 0.824 | yes |
photopic | orbit diameter | orbit depth | 0.77 | 0.707–0.844 | 0.812 | yes |
scotopic | orbit diameter | head length | 0.874 | 0.784–1.023 | 0.533 | yes |
photopic | orbit diameter | head length | 0.895 | 0.7–1.092 | 0.575 | yes |
both | orbit diameter | head length | 0.793 | 0.626–0.916 | 0.704 | |
scotopic | inner diameter sclerotic ring | head length | 0.928 | 0.737–1.168 | 0.499 | yes |
photopic | inner diameter sclerotic ring | head length | 1.068 | 0.911–1.251 | 0.378 | yes |
both | inner diameter sclerotic ring | head length | 1.24 | 1.03–1.49 | 0.524 | |
both | orbit depth + sclerotic ring length | head length | 1.03 | 0.902–1.18 | 0.747 | |
both | orbit depth | head length | 1.03 | 0.902–1.18 | 0.747 | |
both | sclerotic ring length | head length | 1.24 | 1.05–1.46 | 0.623 |
Comparisons between soft and hard tissue
All relationships between soft-tissue variables and their hard-tissue correlates were highly significant (P < 0.001) (see Table 3). The corneal diameter and the inner diameter of the sclerotic ring scaled with slight negative allometry, and the axial length of the eye scaled nearly isometrically with both the orbit depth and the orbit depth summed with the sclerotic ring length (see Table 3). However, the axial length of the eye and the sclerotic ring length considered alone scaled with slight negative allometry (see Table 3).
Table 3.
Soft-tissue variable | Hard-tissue variable | P-value | r2 | RMA slope | CI | Phylogenetic independent contrast RMA slope |
---|---|---|---|---|---|---|
corneal diameter | inner diameter sclerotic ring | < 0.001 | 0.936 | 0.9 | 0.842–0.963 | 0.99 |
corneal diameter | orbit diameter | < 0.001 | 0.686 | 1.48 | 1.28–1.72 | |
axial length of the eye | orbit depth + sclerotic ring max length | < 0.001 | 0.836 | 1.01 | 0.91–1.13 | 0.977 |
axial length of the eye | sclerotic ring max length | < 0.001 | 0.793 | 0.889 | 0.785–0.999 | 1.008 |
axial length of the eye | orbit depth + axial sclerotic ring length | < 0.001 | 0.526 | 0.633 | 0.527–0.76 | |
axial length of the eye | axial sclerotic ring length | < 0.001 | 0.678 | 0.609 | 0.524–0.709 | |
axial length of the eye | orbit depth | < 0.001 | 0.694 | 0.994 | 0.855–1.156 | 0.777 |
Summary results for comparisons between soft-tissue variables and their hard-tissue correlates.
Activity pattern analysis utilizing hard-tissue-only measurements
One-way anovaresults for the residuals calculated from a single RMA line calculated for both nocturnal and diurnal birds considered together showed significant differences between nocturnal and diurnal birds for all pairs of hard-tissue variables except for the inner diameter of the sclerotic ring (y-variable) and the sclerotic ring maximum length or the axial sclerotic ring length (x-variable) (see Table 4).
Table 4.
Y-variable | X-variable | RMA Regression Equation | anovaP-value | anovaF-value |
---|---|---|---|---|
sclerotic ring inner diameter | orbit depth + sclerotic ring length | y = (1.2)(x) − 0.49 | < 0.001 | 11.658 |
sclerotic ring inner diameter | orbit depth + axial sclerotic ring length | y = (0.644)(x) + 0.307 | < 0.001 | 25.571 |
sclerotic ring inner diameter | sclerotic ring maximum length | y = (0.997)(x) + 0.231 | 0.216 | 1.546 |
sclerotic ring inner diameter | axial sclerotic ring length | y = (0.7)(x) + 0.66 | 0.227 | 1.47 |
sclerotic ring inner diameter | orbit depth | y = (1.38)(x) − 0.34 | < 0.001 | 18.861 |
sclerotic ring inner diameter | head length | y = (1.24)(x) − 0.946 | < 0.001 | 33.168 |
orbit diameter | orbit depth | y = (0.888)(x) − 0.946 | < 0.001 | 13.902 |
orbit diameter | head length | y = (0.973)(x) − 0.016 | 0.002 | 9.883 |
Summary results for the anova analyses of residuals calculated from a single RMA line. A significant anova P-value indicates a significant difference between nocturnal and diurnal activity patterns. All variables produced a significant anova except for when measurements of the sclerotic ring are considered alone, indicating that activity pattern can not be interpreted from an isolated sclerotic ring with no other information.
When RMA lines were calculated individually for each activity pattern for each pair of hard-tissue variables, ancova analyses confirmed anova results. There were significant elevational differences between the regression lines for nocturnal and diurnal birds, for those slopes that passed the tests for homogeneity (see Table 2 and Figs 3 and 4).
All one-way anovas performed on single hard-tissue variables showed significant differences between activity patterns, except for log10 sclerotic ring maximum length and log10 axial sclerotic ring length (see Table 5 and Fig. 5). anovas were calculated in SPSS 8.0 (see Table 5).
Table 5.
Variable | n | Mean | SD | df | F-variable | P-value |
---|---|---|---|---|---|---|
inner diameter sclerotic ring* | 137 | 0.9212 | 0.2163 | 136 | 51.738 | < 0.001 |
orbit depth + axial sclerotic ring length | 138 | 1.0529 | 0.2302 | 137 | 11.428 | 0.001 |
sclerotic ring max length | 138 | 0.5388 | 0.3361 | 137 | 27.101 | < 0.001 |
axial sclerotic ring length | 98 | 0.4764 | 0.3308 | 97 | 23.362 | < 0.001 |
orbit depth | 138 | 0.9503 | 0.2185 | 137 | 2.382 | 0.125 |
orbit diameter | 137 | 1.1972 | 0.1739 | 136 | 22.301 | < 0.001 |
orbit depth + sclerotic ring length | 138 | 1.1108 | 0.2199 | 137 | 10.197 | 0.002 |
shape ratio** | 137 | −0.1908 | 0.1041 | 136 | 47.438 | < 0.001 |
Results for anova analyses. These anovas compare means of nocturnal and diurnal animals to determine if univariate variables can differentiate between the activity patterns.
This is the only variable with significant results for the phylogenetic independent contrast analysis.
The shape ratio = log10(inner diameter sclerotic ring – [orbit depth + sclerotic ring length]).
There was a non-significant correlation between the shape ratio [inner diameter of sclerotic ring/(orbit depth + sclerotic ring length)] and head length, suggesting that this ratio can be utilized to examine shape differences between the activity patterns with no significant remaining relationship with size (P = 0.017, r2 = 0.041).
Phylogenetic correction
Branch length diagnostics generated in PDAP from the all = 1, Grafen (1989) and Pagel (1992) algorithms demonstrated that each of these had the requisite lack of fit between tree topology, branch lengths and tip data (Díaz-Uriarte & Garland, 1998). Visual examination of the effects of each of these branch length transformations on the contrast data suggested that the Pagel (1992) algorithm best suited the analysis (see Midford et al. 2005). Phylogenetically corrected analyses of the morphological variables described above for the Cracraft et al. (2004) and Livezey & Zusi (2007) phylogenies revealed non-significant differences between the two activity patterns except for the inner diameter of the sclerotic ring (Cracraft et al. 2004: Spearman's rho = 0.598, P = 0.005, 20 contrasts reflecting change between activity patterns; Livezey & Zusi, 2007: Spearman's rho = 0.588, P = 0.02, 17 contrasts reflecting change between activity patterns). Similar analyses for the Ericson et al. (2006) phylogeny were all non-significant.
Activity pattern interpretation for A. lithographica
As seen in Figs 4 and 5, measurements from the Berlin specimen of A. lithographica plot within the ranges of both nocturnal and diurnal birds. Therefore, no activity pattern determination can be made based on the available information for Archaeopteryx.
Discussion
Comparisons between soft and hard tissue
There is a strong relationship between the avian eye, orbit and sclerotic ring, which underlines the importance of the visual system to the evolution of the avian skull. Many of the RMA slopes between a soft-tissue variable and its bony correlate indicate relationships that either include or are near isometry. The corneal diameter is virtually identical to the inner diameter of the sclerotic ring (see Fig. 1); the relationship is highly significant (P < 0.001) and nearly all of the variance is explained with an r2 of 0.936. Therefore, the inner diameter of the sclerotic ring is a useful correlate of the corneal diameter for birds in which the soft tissue is unavailable for study, i.e. specifically for fossil birds.
The axial length of the eye, highly associated with an animal's visual acuity (Hughes, 1977; Land, 1980; Green et al. 1980; Martin, 1982, 1990, 1999), has a significant relationship with both orbit depth (r2 = 0.694), maximum length of the sclerotic ring (r2 = 0.793) and axial sclerotic ring length (r2 = 0.547). However, the relationship between soft and hard tissue is the strongest if the sum of orbit depth and the maximum sclerotic ring length is compared with the axial length of the eye (r2 = 0.836), with an RMA regression slope that indicates isometry. This is logical, as the soft tissue of the eye is only partially housed by either the orbit or the sclerotic ring individually, but when both are considered together, the only portion of the eye without a close bony correlate is that portion of the cornea that protrudes from the inner diameter of the sclerotic ring (see Fig. 1). Interestingly, when the axial sclerotic ring length is considered together with the orbit depth, relatively little of the variance is explained (r2 = 0.362). This may be because as this measurement is calculated from two measurements, both of which have measurement error, rather than collected directly from bony specimens, measurement error is exacerbated. Additionally, as it was not possible to calculate the axial sclerotic ring length for specimens with flat sclerotic rings, the orbit depth alone was used to calculate statistics for many diurnal birds, including most Columbiformes (see Table 1). It may be that there was a reduction in variance explained given that for those animals there was a portion of the axial length of the eye that did not have a bony correlate that was partially compensated for by the use of the maximum sclerotic ring length.
Activity pattern analysis utilizing hard-tissue-only measurements and interpretation of A. lithographica
Soft-tissue-only analysis has shown that the size and shape of a bird's eyeball reflect its activity pattern: nocturnal birds have a larger corneal diameter relative to the axial length of the eye, and diurnal birds have a larger axial length of the eye relative to the corneal diameter (Ritland, 1982; Martin, 1999; Hall, 2005; Hall & Ross, 2007; Ross et al. 2007). This study shows that when all the hard-tissue variables are available for analysis, it is possible to infer the size and shape of the eyeball, and that these hard-tissue variables are well associated with the bird's activity pattern.
Analysis of phylogenetically independent contrasts did not show significant differences between nocturnal and diurnal birds for any of the variables except the inner diameter of the sclerotic ring. PIC analysis of the relevant soft-tissue variables, i.e. corneal diameter and axial length of the eye, also did not find these size variables to be statisistically different between activity patterns (Hall, 2005; Hall & Ross, 2007). However, the log10 shape ratio of corneal diameter versus axial length of the eye was found previously to be highly significantly different for birds with different activity patterns (Hall, 2005; Hall & Ross, 2007). Here the equivalent bony shape ratio, the log10 ratio of the inner diameter of the sclerotic ring/(sclerotic ring length + orbit depth), was not found to be significant in a phylogenetic context. However, this may be because the hard-tissue sample size in the present study (45 species) is significantly smaller than the soft-tissue sample size (202 species: Hall, 2005; Hall & Ross, 2007). Therefore, a PIC analysis of the shape ratio may be significant for an increased hard-tissue sample size.
In standard statistical analysis, anova analyses of residuals show a significant difference between the means of nocturnal and diurnal birds, indicating that all hard-tissue variables are statistically capable of differentiating between the activity patterns except measurements of the sclerotic ring alone. These results are confirmed by the ancova analyses of elevational differences between RMA regression lines for nocturnal and diurnal birds. Also, all anova analyses of these individual hard-tissue variables show statistically significant differences between the means of nocturnal and diurnal animals. However, not all the hard-tissue variables are equally capable of separating nocturnal and diurnal birds. One aim of the present study was to see how much bony anatomy is required to interpret activity pattern reasonably, especially to do so for fossils that are usually incomplete specimens. Just dimensions of the sclerotic ring alone do not separate nocturnal and diurnal birds well (Fig. 4). Also, a scatter plot of just orbital dimensions, orbit diameter on the y- and orbit depth on the x-axis, reveals considerable overlap between nocturnal and diurnal birds (Fig. 4). The best separation between nocturnal and diurnal birds in scatter plots is when dimensions of both orbit depth and sclerotic ring are available (Fig. 3). Therefore, although the Berlin specimen of A. lithographica preserves many of the variables included here, including the inner diameter of the sclerotic ring, maximum sclerotic ring length, orbit diameter and head length, orbit depth and axial sclerotic ring length are unavailable. Inner diameter of the sclerotic ring and the maximum length of the sclerotic ring are insufficient to interpret activity pattern: the fossil plotted within the ranges of both nocturnal and diurnal birds for all available variables, and thus activity pattern cannot be reliably interpreted (Figs 4 and 5).
The measurements that have been useful for primate activity pattern studies, orbit diameter and skull length (Kay & Cartmill, 1977; Heesy & Ross, 2001), are not useful for birds. Although there is a significant ancova between nocturnal and diurnal birds, the scatter plot shows extensive overlap between the two activity patterns (see Fig. 4c). The inner diameter of the sclerotic ring on the y-axis and head length on the x-axis shows better separation between nocturnal and diurnal birds (see Fig. 4b). This is logical because there is a much closer relationship between corneal diameter and inner diameter of the sclerotic ring than there is with orbit diameter. However, there is still significant overlap between nocturnal and diurnal birds, and head length is not as useful as direct measurements of orbit depth and sclerotic ring for interpreting activity pattern in birds.
Although all anova analyses of these hard-tissue variables show statistically significant differences between the means of nocturnal and diurnal animals, the boxplots in Fig. 5 all show single variables with considerable overlap in range between the activity patterns, and fossil interpretation would only be possible for a bird that plotted in the extremes. The single variable with the best separation between nocturnal and diurnal animals is the inner diameter of the sclerotic ring, the bony correlate of the corneal diameter, which in turn is highly associated with visual sensitivity (Fig. 5). This is also the only hard-tissue variable that phylogenetically independent contrast analysis found to be significantly different between nocturnal and diurnal birds in two of the three tree topologies analysed. However, the inner diameter of the sclerotic ring still shows considerable overlap between the activity patterns, and, as discussed above, Archaeopteryx plots within the ranges of both activity patterns. For the great majority of the birds in this sample, an isolated sclerotic ring is not sufficient to interpret activity pattern reliably, nor are dimensions of just the sclerotic ring and the orbit diameter, and studies that attempt to do so (e.g. Rinehart et al. 2004) are not robust. Except for those birds that plot in the extremes of the nocturnal and diurnal ranges, dimensions of both the sclerotic ring and orbit depth are necessary to make a reliable activity pattern interpretation.
It would be a great advance in understanding the evolution and palaeoecologies of birds if activity pattern could be interpreted from bony variables alone. However, most bird fossils found thus far are incomplete in some way, due at least in part to the fragile nature of bird osteology. Therefore, this important limitation must be considered by bird and non-avian dinosaur palaeontologists because, for the majority of bird fossils currently available, it is not possible to interpret avian palaeo-activity patterns directly from a fossil. However, the present study quantifies scaling relationships between the avian eye, orbit and sclerotic ring, and underlines the importance of the visual system in influencing the evolution of avian skull morphology.
Concluding remarks
This study quantifies the scaling relationships between the hard and soft tissue of the avian eye and orbit, showing that there is a close relationship between the soft tissue (corneal diameter and axial length of the eye) and hard tissue (the orbit and sclerotic ring). Activity pattern significantly influences the morphology of the orbit and sclerotic ring, just as it influences the soft tissue of the avian eye. Although it is theoretically possible to interpret activity pattern from hard-tissue characteristics alone, not all hard-tissue variables are equally capable of differentiating between nocturnal and diurnal birds. The clearest separation between activity patterns is possible when dimensions of both the sclerotic ring and the orbit depth are considered together. It is not currently possible to interpret the activity pattern of A. lithographica reliably, for which orbit depth is not available.
Acknowledgments
For access to specimens, I thank the American Museum of Natural History (New York), the Field Museum of Natural History (Chicago), the National Museum of Natural History, Smithsonian Institution (Washington, DC), the British National Museum of Natural History (Tring, UK), and the Witmer Lab (Athens, OH). I thank my funding sources, including the Society of Integrative and Comparative Biology Grant-in-Aid-of-Research, the Frank M. Chapman Memorial Fund, the Field Museum of Natural History Visiting Scholarship, and the Jurassic Foundation. This work was part of a PhD thesis, and here I thank my advisory committee, including Drs Callum Ross, Matthew Carrano, Susan Evans, Catherine Forster, William Jungers and Nathan Kley. In addition, for helpful comments I thank Drs Joel Cracraft, Andrzej Elzanowski, Christopher Heesy, Keith Metzger, Patrick O'Connor, Maureen O'Leary, F. James Rohlf, Karen Samonds and Lawrence Witmer. For great assistance in figure composition, I thank Dr Beth Townsend. For invaluable assistance in the phylogenetic analysis, I thank Drs Christopher Heesy, Andrew Iwaniuk and Jason Kamilar. Lastly, I thank Dr Julia Clarke and two anonymous reviewers for helpful comments on submitted drafts of the manuscript.
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