Palaeognathae

Ratites and Tinamous

47 AVIAN ORDERS

Palaeognathae

Galloanserae

Mirandornithes

Columbaves

Otidimorphae

Columbimorphae

Elementaves

GRUAE

Opisthocomimorphae

Gruimorphae

Ardeae

Eurypygimorphae

Aequornithes

Strisores

Telluraves

Afroaves

Australaves

PALAEOGNATHAE Pycraft, 1900

The oldest major division among living birds is between the Palaeognathae and Neognathae. It was first recognized by Pycraft (1900). Kuhl et al. (2021) estimate that the split occurred around 94±4 mya. Stiller et al.'s (2024) figure ED-2 reads out at about 92.5±7.5 mya.

Although the ratites had long been considered related, the tinamous were thought to be distinct. Pycraft completed the group by adding the tinamous to the ratites, creating the Palaeognathae. This consists of the volant tinamous, the non-volant ratites (ostriches, rheas, emus, cassowaries, kiwis), and their extinct relatives, which include moas, elephant birds, and the Lithornithiformes (sometimes called false tinamous).

Traditionally, the Palaeognathae were divided into the flightless ratites and the volant tinamous. Some of the earlier generic evidence seemed to support this division (e.g., Haddrath and Baker, 2001).

This simple picture is now known to be wrong. An avalanche of more recent studies, including Chojnowski et al. (2008), Hackett et al. (2008), Harshman et al. (2008), Phillips et al. (2010), Faircloth et al. (2012), Haddrath and Baker (2012), J.V. Smith et al. (2013), Grealy et al. (2017), Yonezawa et al. (2017), Cloutier et al. (2019), Sackton et al. (2019), Urantówka et al. (2020), Simmons et al. (2022), and Takezaki (2023), have come to a very different conclusion. The ratites are not a natural grouping! The ratites are not monophyletic. This result is also supported by large-scale bird phylogenies such as Hackett et al. (2008), Prum et al. (2015), Kuhl et al. (2021), and Stiller et al. (2024).

Moas, Elephant Birds, and Lithornithiformes

The problem is that some of the ratites are more closely related to the volant tinamous than they are to other ratites. In particular, the ostriches are no more closely related to most of the other ratites than they are to the tinamous.

Palaeognathae tree

The diagram to the right shows the current situation. It includes not only living birds, but some extinct taxa. By using ancient DNA, we have been able to properly place the extinct Elephant Birds and Moas on the tree.

Unfortunately, ancient DNA only works if the fossils are not too ancient, so the extinct Lithornithiformes are a problem. Comparison of bones suggests that the most likely possibilities are that they are sister to the tinamous (Johnston, 2011; Nesbitt and Clarke, 2016), or are sister to all of the surviving paleognaths (Worthy et al., 2017; Yonezawa et al., 2017). I suspect the latter is correct. That is reflected in the accompanying diagram.

In fact, the situation with the Lithornithiformes may not be this simple. They may not even be a monophyletic group. See Nesbitt and Clarke (2016) and Widrig and Field (2022) for more on the Lithornithiformes.

What about the Rheas?

It's clear enough that the ostriches are the basal among the extant Palaeognathae. Once we get beyond the ostriches, things are not as clear-cut.

The remaining Palaeognathae comprise three groups: (1) rheas, (2) tinamous (and the recently extinct moas), and (3) cassowaries, emus, kiwis and the recently extinct elephant birds. These groups all separated over a short period of time, near the beginning of the Paleogene. E.g., Yonezawa et al. (2017) estimate the three groups separated from one another over a period of 4 million years.

So which group separated first? Even though it has been extensively studied, the short time period makes it hard to answer this question. Many analyses (e.g., Harshman et al., 2008; Phillips et al., 2010; J.V. Smith et al., 2013) favor putting the rheas first.

However, when Haddrath and Baker (2012) considered retroposons, the balance temporarily shifted to the tinamaou/moa clade, and that is the topology we formerly followed here. It is also the topology found by Cloutier et al. (2019), who used both coalescent and concatenated methods to address the question. The coalescent methods found that group (2), the tinamous and moas separated first. In contrast, concatenation favored group (1), the rheas.

Cloutier et al. attributed this discrepancy to incomplete lineage sorting. This is not surprising as the lineages all arose over a period of about 4 million years. Because coalescent methods are generally more accurate, I assumed the moas and tinamous separated first. TiF has followed this starting in December 2009 (version 2.52 of this file).

Somewhat more recent analyses such as Urantówka et al. (2020), Simmons et al. (2022), and Takezaki (2023) favor putting the rheas first. Simmons et al. (2022) considered three possibilities, which they color-coded:

Figure 1 in Sackton et al. (2019) looks suspiciously like a hard polytomy. Mirarab et al. (2024) discovered that an apparent hard polyomy in Neoaves in the same time frame was due to a frozen segment of DNA. Stiller et al. (2024) developed a phylogeny that corrected for that. Lo and behold, it also resolves the Palaeognathae. The main tree in Stiller et al. supports the blue topology, where the Rheas are closer to the tinamous and moas. That is the topology now used by TiF. Questions still remain as the high guanine-cytosine content in the loci of the blue clades may have biased the result. In particular, the red topology cannot be completely ruled out.

Armed with a correct phylogeny (hopefully!), we can properly calibrate the divisions in the Palaeognathae. Stiller et al. (2024) did this, and found that all 5 Palaeognath orders dated to just before the end of the Cretaceous. I expect this really means just after, but it makes that point that all of the Palaeognath bird orders are truly ancient.

Flightlessness Common in Ratites

This topology suggests that flightlessness has evolved at least 6 times (!) in the Palaeognathae: in ostriches, rheas, moas, elephant birds, emus/cassowaries, and kiwis. The fact that the tinamous can fly implies flightlessness evolved at least four times. The distribution of the emus/cassowaries, elephant birds, kiwis suggests they each had volant ancestors, accounting for the other two times.

Paleognath Geography

There is further relevant DNA evidence indicating that the extinct elephant birds of Madagascar are the closest relatives of the kiwis (Mitchell et al., 2014b), with a common ancestor perhaps 50 mya. This is a problem for vicariance theories driven by continental drift because Madagascar likely separated from Gondwana considerably earlier, perhaps 120 mya. In that case, the ancestor of the elephant birds would have had to fly, and we can infer that flight was indpendently lost in the rheas, emu/cassorwary, elephant bird, and kiwi lineages, a total of 6 losses of flight. This is not an unreasonable number. One only has to consider all of the flightless rails to see that.

Paleognath Orders

The Palaeognathae are divided into several orders in recognition of the great antiquity of the various branches. Stiller et al. (2024) have all of the Palaeognath orders splitting shortly before the end of the Cretaceous period, although uncertainly does not rule out all splitting after the K/T (or K/Pg) boundary. Other sources come to different conclusions. Phillips et al. (2010) estimated the ostriches diverged from the rest of the Palaeognathae about 60-95 mya, while Chojnowski et al. (2008) dated this divergence around 64±22 mya, soon after the end of the Cretaceous. Haddrath and Baker (2012) put it at 73-119 mya. Mapping Jarvis et al. (2014) onto the phylogeny used here suggests that the split was about 84 mya (interval 58-96 mya).

The Cassowaries and Emus are much more closely related than the other paleognath groups, and are placed in a single family: Casuariidae. Although the Moas and Elephant Birds are not part of the main TiF list, a genus-level phylogeny of both is given in the tree diagram. The Moa tree is based on Bunce et al. (2009).

Based on calibrated trees, I suspect that only the ostriches and possibly false tinamous survived the Chicxulub meteorite that ended both the Cretaceous period and all of the non-avian dinosaurs.

STRUTHIONIFORMES Latham, 1790

Struthionidae: Ostriches Vigors, 1825

The authors for family-group names are mostly based on Bock (1994), while the authors for order-group names are primarily based on the series by Brodkorb (1963–1978). In both cases, additional sources have been consulted (e.g., Livezey and Zusi (2007)). In a number of cases, I have managed to examine the original (thank you Google Books!). The ICZN does not regulate order-group names. However, for parvorders (-ida), infraorders (-ides), suborders (-i), orders (-iformes), and superorders (-imorphae), I am attempting to follow similar rules. In particular, they are based on priority and the orginal use must been at an ordinal level and must be based on an included genus name (type genus) actually used by that author. The endings have been adjusted to modern usage.

1 genus, 2 species HBW-1

CASUARIIFORMES P.L. Sclater 1880

The Dromaiidae (Emus) have been merged into the Casuariidae (cassowaries) because the split between them seems fairly recent. The molecular dates in Phillips et al. (2010) and in Haddrath and Baker (2012) already suggested they were so closely related that they could be treated as a single family. More precise dating by Prum et al. (2015) placed the split at about 10 million years ago, too close to even rank them as subfamilies.

Casuariidae: Emus and Cassowaries Kaup, 1847

2 genera, 4 species HBW-1

Heupink et al. (2011) argue that the extinct King Island Emu, Dromaius ater, was quite closely related to the extinct Tasmanian subspecies of the Emu, and is best considered a dwarf subspecies of Dromaius novaehollandiae. The Kangaroo Island Emu, D. baudinianus, seems likely to have been no more different from the Emu than the King Island Emu was, so I am also considering it a subspecies of the Emu, D. novaehollandiae.

APTERYGIFORMES Haeckel 1866

Apterygidae tree

The order of the Kiwis reflects the phylogeny in Burbidge et al. (2003) and Shepherd et al. (2012). Burbidge et al. also provide evidence for recognizing 3 extant species of brown kiwi, as is done here. Shepherd et al. found evidence of an extinct northern clade of Little Spotted Kiwi that may deserve recognition as a separate species. The DNA samples of this potential species are from bones of unknown age.

Apterygidae: Kiwis G.R. Gray, 1840

1 genus, 5 species HBW-1

RHEIFORMES Forbes, 1884

Rheidae: Rheas Bonaparte, 1849

1 genus, 2 species HBW-1

TINAMIFORMES Huxley, 1872

Tinamidae tree
Click for Tinamou species tree

The Tinamiformes (and their extinct Moa cousins) form the remaining branch of the Palaeognathae. The taxonomy of the Tinamous is now based on Musher et al. (2024) and SACC.

The age of the Tinamidae crown group is rather uncertain. Almeida et al. (Figure 3) give an age of 40 million years based on the complete data (black lines in their Fig. 3), but only about 30 million years based on the RAG2 gene (gray lines). To add to the confusion, Prum et al. (2015) puts it near 26 million years ago. Generally speaking, I prefer to go with Prum's number. As a result, the age estimates for genera must even younger than shown by the gray lines. In particular, Prum et al. place the basal split in Eudromiinae at about 21 mya and the split between Cryptura and Tinamus at about 17 mya. This compares with about 25 and 21 mya according to the gray lines.

The Tinamidae naturally divide into two subfamilies: Eudromiinae (Steppe Tinamous) and Tinaminae (Forest Tinamous) and 8 genera.

The current arrangement of the Tinamidae follows Figure 2 of Musher et al. (2024). The current species tree marks the species with new DNA data using bright red asterisks. Only one species was not sampled, the Slaty-breasted Tinamou, Tinamus boucardi. Its placement reflects hybridization in Honduras with the Thicket Tinamou, Tinamus cinnamomeus (Monroe, 1968).

Besides reordering the tinamous, the Musher et al. tree suggests that the Andean Tinamou, Nothoprocta pentlandii, represents two non-sister species. In Birds of the High Andes, Fjeldså and Krabbe (1990) noted that the Andean Tinamou consists of a brownish group of subspecies and a grayish group. Accordingly, I've split the Andean Tinamou, Nothoprocta pentlandii, into two species:

The New Tinamus, plus Cryptura and Crypturus

You may be puzzled by the way I use Tinamus. Wasn't Tinamus major the type? How can it be booted out of Tinamus? What happened?

Well, although people have treated Tinamus major as the type, it isn't! I don't know the complete story, but the genus Tinamus had been attributed to Latham (1790) until Hermann's 1783 Tabula affinitatum animalium was eventually noticed. This clearly has priority over Latham.

The problem is that the type must be among the species named in the original description. Hermann only mentioned soui. He also referred to a description of tinamous in Buffon, who included major and a few others, but did not explicitly refer to the species included in Buffon. Names included only by reference cannot be among the originally included nominal species. The ICZN rules are quite clear on this (Art. 67.2.3). They are also clear that the type must be an originally included nominal species. That means that Tinamus soui is the only possible type species for Tinamus.

This problem was pointed out in BirdForum by Laurent Raty. Some of the details are also mentioned on the Richmond cards for Tinamus here and here, where the reference to Buffon is accepted. And yes, Buffon is the same Buffon as in Buffon's needle problem. Using the (now incorrect) inclusion of Buffon's species, Apstein fixed the type as major in 1915. I'm not sure when the code explicitly barred inclusion by reference.

No one seems willing to follow the Code here, so I thought I would stir the pot by doing so. One problem with the Code is that it can cause (scientific) naming chaos. Ideally, the ICZN would decide in favor of stability here and elsewhere (e.g., Sulidae) and preserve traditional usage.

As major is also the type of Cryptura, I've put what had been the Tinamus species in Cryptura. What had been called Crypturellus is now mostly called Tinamus, with the others (cinereus and berlepschi) in Crypturus. Yes, it's confusing, but it's long past time to correct this.

Type Species

The table below lists the type species for each of the genera used by the current TiF list. Type species are noted on the species tree by leading black 5-pointed stars.

Genus Type Species Author Year

Tinamotis pentlandii Vigors 1837
Eudromia elegans I. Geoffroy Saint-Hilaire 1832
Nothura boraquira Wagler 1827
Rhynchotus rufescens von Spix 1825
Nothoprocta perdicaria Sclater & Salvin 1873
Nothocercus julius Bonaparte 1856
Crypturus cinereus Illiger 1811
Cryptura majora Vieillot 1816
Tinamus soui Hermann 1783

Compared to the earlier TiF version of the Tinamous (versions 3.03, March 18, 2018 and earlier) which had the same genera as version 13.2 of the IOC list, Taoniscus has been absorbed by Nothura, Tinamus is renamed Cryptura, Berlepsch's Tinamou, Crypturellus berlepschi and Cinereous Tinamou, Crypturellus cinereus have been moved to Crypturus, and the remainder of Crypturellus is now called Tinamus.

What about the Chaco Nothrua?

Hayes et al. (2018) showed that there is no reason to consider the Chaco Nothura, Nothura chacoensis, distinct from the Spotted Nothura, Nothura maculosa. As a result, I now consider the Chaco Nothura to be a subspecies of the Spotted Nothura, Nothura maculosa.

Tinamidae: Tinamous G.R. Gray, 1840

9 genera, 47 species HBW-1

Eudromiinae: Steppe Tinamous Bonaparte 1854

  1. Puna Tinamou, Tinamotis pentlandii
  2. Patagonian Tinamou, Tinamotis ingoufi
  3. Quebracho Crested-Tinamou, Eudromia formosa
  4. Elegant Crested-Tinamou, Eudromia elegans
  5. White-bellied Nothura, Nothura boraquira
  6. Dwarf Tinamou, Nothura nanus
  7. Lesser Nothura, Nothura minor
  8. Darwin's Nothura, Nothura darwinii
  9. Spotted Nothura, Nothura maculosus
  10. Brushland Tinamou, Rhynchotus cinerascens
  11. Red-winged Tinamou, Rhynchotus rufescens
  12. Huayco Tinamou, Rhynchotus maculicollis
  13. Curve-billed Tinamou, Nothoprocta curvirostris
  14. Ornate Tinamou, Nothoprocta ornata
  15. Brown Andean Tinamou, Nothoprocta oustaleti
  16. Taczanowski's Tinamou, Nothoprocta taczanowskii
  17. Gray Andean Tinamou, Nothoprocta pentlandii
  18. Chilean Tinamou, Nothoprocta perdicaria

Tinaminae: Forest Tinamous G.R. Gray, 1840

  1. Tawny-breasted Tinamou, Nothocercus julius
  2. Highland Tinamou, Nothocercus bonapartei
  3. Hooded Tinamou, Nothocercus nigrocapillus
  4. Great Tinamou, Cryptura majora
  5. Gray Tinamou, Cryptura tao
  6. Solitary Tinamou, Cryptura solitaria
  7. White-throated Tinamou, Cryptura guttata
  8. Black Tinamou, Cryptura osgoodi
  9. Berlepsch's Tinamou, Crypturus berlepschi
  10. Cinereous Tinamou, Crypturus cinereus
  11. Tepui Tinamou, Crypturus ptaritepui
  12. Brown Tinamou, Tinamus obsoletus
  13. Tataupa Tinamou, Tinamus tataupa
  14. Small-billed Tinamou, Tinamus parvirostris
  15. Variegated Tinamou, Tinamus variegatus
  16. Little Tinamou, Tinamus soui
  17. Bartlett's Tinamou, Tinamus bartletti
  18. Barred Tinamou, Tinamus casiquiare
  19. Rusty Tinamou, Tinamus brevirostris
  20. Undulated Tinamou, Tinamus undulatus
  21. Yellow-legged Tinamou, Tinamus noctivagus
  22. Black-capped Tinamou, Tinamus atrocapillus
  23. Pale-browed Tinamou, Tinamus transfasciatus
  24. Thicket Tinamou, Tinamus cinnamomeus
  25. Slaty-breasted Tinamou, Tinamus boucardi
  26. Choco Tinamou, Tinamus kerriae
  27. Red-legged Tinamou, Tinamus erythropus
  28. Gray-legged Tinamou, Tinamus duidae
  29. Brazilian Tinamou, Tinamus strigulosus

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