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Pardirallus lacustris
Taxonomy
Porzana lacustris was named by Brodkorb (1958). Its type specimen is UMMP 33916, a limb element (right humerus), and it is a 3D body fossil. Its type locality is Hagerman west 1, which is in a Pliocene lacustrine - large horizon in the Hagerman Formation of Idaho.
It was recombined as Pardirallus lacustris by Olson (1977).
It was recombined as Pardirallus lacustris by Olson (1977).
Synonymy list
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Pardirallus lacustris Brodkorb 1958
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| P. Brodkorb 1958 | Differs from living Porzana carolina (Linnaeus), Porzana guti (Brodkorb, 1952), and Porzana auffenbergi Brodkorb (1954), the latter two both from the Illinoian stage of the Pleistocene of Florida, as follows: entepicondyle straighter, wider, not oming to a rounded point; ectepicondylar process more rounded and less produced; size larger. Distal width, 6.0; width of shaft, 2.7 mm.
Larger than Rallus prenticei Wetmore (1944) from the upper Pliocene of Kansas, besides differing in generic characters. The humerus of Porzana differs from that of Rallus in having the entepicondyle produced, with a notch separating it from the internal condyle; external condyle scarcely bent. The new species is much smaller than other American fossil rails. |
Measurements
No measurements are available
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| Source: subo = suborder, o = order | |||||
| References: Benton 1983, Kiessling 2004, Marsh 1875 | |||||
Age range: Late/Upper Pliocene or 3.60000 to 2.58000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Pliocene | USA (Idaho) | Porzana lacustris (type locality: 176409) |