Tringa

''Tringa'' is a genus of waders, containing the shanks and tattlers. The genus name ''Tringa'' is the Neo-Latin name given to the green sandpiper by the Italian naturalist Ulisse Aldrovandi in 1599. They are mainly freshwater birds, often with brightly coloured legs as reflected in the English names of six species, as well as the specific names of two of these and the green sandpiper. They are typically associated with northern hemisphere temperate regions for breeding. Some of this group—notably the green sandpiper—nest in trees, using the old nests of other birds, usually thrushes.

The willet and the tattlers have been found to belong in ''Tringa''; these genus changes were formally adopted by the American Ornithologists' Union in 2006.

The present genus in the old, more limited sense was even further subdivided into ''Tringa'' proper and '' Totanus'', either as subgenera or as full genera. The available DNA sequence data suggests however that neither of these is monophyletic and that the latter simply lumps together a number of more or less closely related apomorphic species. Therefore, it seems unwarranted to recognize ''Totanus'' even as a subgenus for the time being.

Taxonomy

The genus ''Tringa'' was introduced in 1758 by the Swedish naturalist Carl Linnaeus in the tenth edition of his '' Systema Naturae''. The name ''Tringa'' is the Neo-Latin name given to the green sandpiper by the Italian naturalist Ulisse Aldrovandi in 1603 based on Ancient Greek ''trungas'', a thrush-sized, white-rumped, tail-bobbing wading bird mentioned by Aristotle. The type species is the green sandpiper (''Tringa ochropus'').

Species

The genus contains 13 species.

Systematics and evolution

The shanks' and tattlers' closest relatives are sandpipers of the genera '' Actitis'' and '' Xenus''. Together with these, they are related to the phalaropes, as well as the turnstones and calidrids.van Tuinen ''et al.'' (2004) The large genus ''Tringa'' and the two very small genera which are most closely related form a phylogeny similar to the situation found in many other shorebird lineages such as calidrids, snipes and woodcocks, or gulls.

The same study has indicated that some morphological characters such as details of the furcula and pelvis have evolved convergently and are no indicators of close relationship. Similarly, the leg/foot color wildly varies between close relatives, with the spotted redshank, the greater yellowlegs, and the common greenshank for example being more closely related among each other than to any other species in the group; the ancestral coloration of the legs and feet was fairly certainly drab buffish as in e.g. the green sandpiper. On the other hand, the molecular phylogeny reveals that the general habitus and size as well as the overall plumage pattern are good indicators of an evolutionary relationship in this group.

The Nordmann's greenshank, a rare and endangered species, was not available for molecular analyses. It is fairly aberrant and was formerly placed in the monotypic genus ''Pseudototanus''. It appears closest overall to the ''semipalmata-flavipes'' and the ''stagnatilis-totanus-glareola'' groups, though it also has some similarities to the greater yellowlegs and common greenshank.

Fossil recordMlíkovský (2002)

Fossil shanks are known since the Miocene, possibly even since the Eo-/Oligocene some 33-30 million years ago (mya) which would be far earlier than most extant genera of birds. However, it is uncertain whether ''Tringa edwardsi'' indeed belongs into the present-day genus or is a distinct, ancestral form. The time of the ''Tringa''-'' Actitis''-'' Xenus''-'' Phalaropus'' divergence has been tentatively dated at 22 mya, the beginning of the Miocene; even if the dating is largely conjectural, it suggests that ''T. edwardsi'' does indeed not belong into the modern genus. Molecular dating—which is not too reliable, however—indicates that the diversification into the known lineages occurred between 20 and 5 mya. The fossil record contains species formerly separated in ''Totanus'' from the Early Miocene onwards. Although these are usually known from very scant remains, the fact that apparently apomorphic ''Tringa'' as well as a putative phalarope are known from about 23-22 mya indicates that the shank-phalarope group had already diverged into the modern genera by the start of the Miocene. The biogeography of living and fossil species—notably, the rarity of the latter in well-researched North American sites—seems to suggest that ''Tringa'' originated in Eurasia. Time and place neatly coincide with the disappearance of the last vestiges of the Turgai Sea, and this process may well have been a major factor in the separation of the genera in the shank-phalarope clade. Still, scolopacids are very similar osteologically, and many of the early fossils of presumed shanks require revaluation.
* ?''Tringa edwardsi'' (Quercy Late Eocene/Early Oligocene of Mouillac, France)
* ?''Tringa gracilis'' (Early Miocene of WC Europe) – calidrid?
* ?''Tringa lartetianus'' (Early Miocene of Saint-Gérand-le-Puy, France)
* ''Tringa'' spp. (Early Miocene of Ravolzhausen, Germany – Early Pleistocene of Europe)Apparently at least three species at Stránská skála (Czech Republic, Early Pleistocene) for example: Mlíkovský (2002)
* ?''Tringa grivensis'' (Middle Miocene of Grive-Saint-Alban, France)
* ?''Tringa majori'' (Middle Miocene of Grive-Saint-Alban, France)
* ?''Tringa minor'' (Middle Miocene of Grive-Saint-Alban, France) – includes ''"Erolia" ennouchii''; calidriid?
* ?''Tringa grigorescui'' (Middle Miocene of Ciobăniţa, Romania)
* ?''Tringa scarabellii'' (Late Miocene of Senigallia, Italy)
* ''Tringa'' sp. 1 (Late Miocene/Early Pliocene of Lee Creek Mine, USA)
* ''Tringa'' sp. 2 (Late Miocene/Early Pliocene of Lee Creek Mine, USA)
* ?''Tringa numenioides'' (Early Pliocene of Odesa, Ukraine)
* ''Tringa antiqua'' (Late Pliocene of Meade County, USA)
* ''Tringa ameghini'' (Late Pleistocene of Talara Tar Seeps, Peru)

''"Tringa" hoffmanni'' is now in '' Ludiortyx''. While its relationships are disputed, it was not a charadriiform.

See also

* Hybridisation in shorebirds

References

Sources

* Ballmann, Peter (1969): Les Oiseaux miocènes de la Grive-Saint-Alban (Isère) he Miocene birds of Grive-Saint-Alban (Isère) '' Geobios'' 2: 157–204. rench with English abstract
* Banks, Richard C.; Cicero, Carla; Dunn, Jon L.; Kratter, Andrew W.; Rasmussen, Pamela C.; Remsen, J.V. Jr.; Rising, James D. & Stotz, Douglas F. (2006)
Forty-seventh Supplement to the American Ornithologists' Union Check-list of North American Birds
'' Auk'' 123(3): 926–936. DOI: 10.1642/0004-8038(2006)123 26:FSTTAO.0.CO;2
* Mlíkovský, Jirí (2002):
Cenozoic Birds of the World, Part 1: Europe
'. Ninox Press, Prague.
* Olson, Storrs L. (1985): Section X.D.2.b. Scolopacidae. ''In:'' Farner, D.S.; King, J.R. & Parkes, Kenneth C. (eds.): ''Avian Biology'' 8: 174–175. Academic Press, New York.
* Paton, Tara A.; Baker, Allan J.; Groth, J.G. & Barrowclough, G.F. (2003): "RAG-1 sequences resolve phylogenetic relationships within charadriiform birds." '' Mol. Phylogenet. Evol.'' 29(2): 268–278.
* Pereira, Sérgio Luiz & Baker, Alan J. (2005)
Multiple Gene Evidence for Parallel Evolution and Retention of Ancestral Morphological States in the Shanks (Charadriiformes: Scolopacidae)
'' Condor'' 107(3): 514–526. DOI: 10.1650/0010-5422(2005)107 514:MGEFPE.0.CO;2
* van Tuinen, Marcel; Waterhouse, David & Dyke, Gareth J. (2004)
Avian molecular systematics on the rebound: a fresh look at modern shorebird phylogenetic relationships
'' J. Avian Biol.'' 35(3): 191–194.

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Bird genera
Taxa named by Carl Linnaeus
Taxa described in 1758