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Small Ducks (Aves: Anatidae) from the Early–Middle Miocene of Eurasia. 1. (1 Viewer)

Fred Ruhe

Well-known member
Netherlands
Nikita Zelenkov, 2023

Small Ducks (Aves: Anatidae) from the Early–Middle Miocene of Eurasia. 1. A revision of Anas velox Milne-Edwards, 1868 and Anas soporata Kurochkin, 1976

Paleontological Journal, 2023, Vol. 57, No. 4, pp. 452–462

Abstract and free pdf: https://www.researchgate.net/public...Edwards_1868_and_Anas_soporata_Kurochkin_1976

A revision of small ducks (the size of the modern teal Anas crecca or smaller) from the middle Miocene of France (Sansan locality) and Mongolia (Sharga locality) clarified the taxonomic status and systematic position of the well-known species Anas velox Milne-Edwards, 1868 and Anas soporata Kurochkin, 1976. It is shown that three small members of the family Anatidae are present in the fauna of the Sansan locality: Anas velox is a diving duck, partly similar to modern Histrionicus, but smaller–here this species is transferred to the fossil genus Protomelanitta Zelenkov, 2011 (basal Mergini). A somewhat smaller taxon from Sansan belongs to the ecological group of dabbling ducks, and is identified as Anas soporata, a species that was previously described from Mongolia and here transferred to the genus Mioquerquedula Zelenkov et Kurochkin,
2012. In addition, yet another very small duck of unclear systematic position is present in the fauna of Sansan. New materials on Mioquerquedula soporata comb. nov. and M. minutissima Zelenkov et Kurochkin, 2012 are also described from the middle Miocene of Mongolia.

Enjoy,

Fred
 
SYSTEMATIC PALEONTOLOGY

Order Anseriformes
Family Anatidae Leach, 1820
Tribe Mergini Rafinesque, 1815
Genus Protomelanitta Zelenkov, 2011
Protomelanitta: Zelenkov, 2011, p. 74; Zelenkov and Kurochkin, 2015, p. 165; Stidham and Zelenkov, 2017, p. 223.

Type species. Protomelanitta gracilis Zelenkov, 2011, middle Miocene of Mongolia

Diagnosis. See Zelenkov (2011).

Composition. In addition to the type species, also P. bakeri Stidham et Zelenkov, 2016 from the mid-
dle Miocene of the USA and, provisionally, P. velox (Milne-Edwards, 1868) from the middle Miocene of
France

Remarks. The genus Protomelanitta was erected from the middle Miocene of the Sharga locality (Mongolia) as a probable basal representative of Mergini, the only member of this group of anatids in the fauna of that locality (Zelenkov, 2011). The similarity of Anas velox with modern Mergini, on the one
hand, as well as the presence of common taxa of anatids in the faunas of the early–middle Miocene of Central Asia and France (Zelenkov et al., 2018; Zelenkov, 2020), on the other hand, make it possible to provisionally assign the small diving duck from Sansan to this genus. For A. velox, the morphology of the coracoid is most diagnostic (see above), however, for Protomelanitta, only the humeri and tarsometatarsi were previously recorded (Zelenkov, 2011; Stidham and Zelenkov, 2017). Meanwhile collections from Sharga contain several coracoids of diving ducks which were not originally identified to species (Zelenkov, 2011). At least one incomplete right coracoid (specimen PIN, no. 4869/247) is close in proportions and absolute size to Histrionicus histrionicus and could thus belong to Protomelanitta gracilis (the holotype of this species, the humerus, also corresponds to Histrionicus histrionicus in absolute dimensions). However, PIN, no. 4869/247 is distinguished from Histrionicus and other Mergini by a flattened processus acrocoracoideus, the apex of which in cranial view (viewed from the end of the bone), is oriented more medially (in Mergini it is oriented ventrally). This confirms the stem-group position of this form in relation to modern Mergini, which also follows from the morphology of the humerus (Zelenkov, 2011). PIN, no. 4869/247 differs from the paralectotype of Anas velox in having a
smaller cotyla scapularis, a somewhat thicker shaft, and a slightly blunter angulus medialis—none of these differences go beyond intrageneric ones. At the same time, the general proportions of the bone (the length and degree of medial protrusion of the processus acrocoracoideus, the size and orientation of the processus procoracoideus, the ratio of the lengths of the omal icular part to the length from cotyla scapularis to facies articularis sternalis) are similar in both specimens.
Ocyplonessa shotwelli Brodkorb, 1961 from the lower upper Miocene of the United States was described from fragmentary tarsometatarsus and carpometacarpus as a form metrically and morphologically similar to Histrionicus (Brodkorb, 1961). S. Olson and P. Rasmussen (Olson and Rasmussen, 2001) reexamined the holotype of this species (distal tarsometatarsus) and assigned it to modern Histrionicus, considering the differences insignificant; carpometacarpus morphology was not discussed by these authors. The carpometacarpus of Ocyplonessa shotwelli has reliable differences relative to that of Histrionicus and other Mergini in the morphology of processus extensorius, which warrants a separate generic status for this fossil North American form. However, this carpometacarpus does have a lower processus extensorius (aadvanced character similar to Mergini), well-pronounced depressions on the ventral surface of the proximal end, and a deep fovea carpalis caudalis (Brodkorb, 1961), which constitute differences from the lectotype of Anas velox. Thus, assigning A. velox to the genus Ocyplonessa would be less justified than to Protomelanitta. However, the genus affinity of Anas velox still needs to be confirmed after a comprehensive revision of the larger diving ducks of the middle Mio-
cene of Eurasia.

Protomelanitta velox (Milne-Edwards, 1868), comb. nov.
Anas velox: Milne-Edwards, 1867-68, p. 150, pl. 26, figs. 1–18; Fraas, 1870, p. 280; Lydekker, 1891, p. 116; Paris, 1912, p. 290; Lambrecht, 1933, p. 359; Howard, 1964, p. 294; Cheneval, 1987, p. 142, pl. 1, figs. 2–4 (part.); Cheneval, 2000, p. 329 (part.); Mlíkovský, 2002, p. 118 (part.).
Nettion velox: Brodkorb, 1964, p. 224.
Mioquerquedula velox: Zelenkov and Kurochkin, 2012, p. 91

Lectotype. MNHN, no. SA 1230, right carpometacarpus; Sansan locality, France; middle Miocene (zone
MN 6) (Cheneval, 1987).

Material. In addition to the lectotype, from the type locality: MNHN, nos. SA 1232, right coracoid
(paralectotype; Cheneval, 1987); SA 14003, right coracoid; SA 1231, proximal fragment of left ulna
(paralectotype; Cheneval, 1987); SA 1404, proximal fragment of right carpometacarpus.

Fred
 
Genus Mioquerquedula Zelenkov et Kurochkin, 2012
Mioquerquedula minutissima Zelenkov et Kurochkin, 2012

Holotype. PIN, no. 4869/193, left coracoid; Mongolia, Gobi-Altai aimag, Shargain-Gobi, Sharga
locality; uppermost middle Miocene.

Description. In the humerus, the distal end expands noticeably relative to the shaft; in dorsal view,
the end does not bend cranially; the impressio m. pronator superficialis is large, close to the tuberculum
supracondylare ventrale; the tuberculum supracondylare ventrale protrudes distinctly from the adjacent
part of the shaft; the impressio brachialis is narrow and virtually does not expand dorsoproximally; the epicondylus dorsalis narrow; the condylus ventralis, in cranial view, is not large, its proximal edge is slightly inclined relative to the long axis of the bone. For a description of the coracoid, see Zelenkov and Kurochkin (2012). The size is small, comparable to that of an extant Nettapus auritus.

Variability. Three fragmentary coracoids are known from the Sharga locality, comparable to the holotype in absolute size and, on this basis, attributed to this species. Specimens PIN 4869/191, 239 are
characterized by a straighter shaft at the level of the facies articularis humeralis compared to the holotype, the absence of a notch on the caudal margin of the facies articularis clavicularis (present in the holotype), and the absence of a pit in the cranial part of the sulcus m. supracoracoidei (the facies articularis clavicularis in these specimens does not overhang the sulcus). It seems unlikely that two taxa of pygmy anatids of the same size would be present in Sharga, so these variations are treated as intraspecific variability. They are consistent with the increased variability of the coracoid (except for the general proportions) in modern dabbling ducks (Zelenkov, 2022).

Comparison. Differs from other species of the genus in small size.

Remarks. The humerus from Sharga (PIN, no. 4869/56), previously designated as Anatidae indet., can be attributed to this species based on the relative size (the size of N. auritus) and morphology similar to the larger specimen attributed to M. soporata (see below). PIN, no. 4869/56 has a somewhat thinner
shaft, and the distal end is somewhat more strongly expanded relative to the shaft—this character can be either individual or characteristic of M. minutissima. Shaft width is the most variable parameter in modern dabbling ducks (Zelenkov, 2022). Malacorhynchus has an even more expanded distal end and a larger epicondylus dorsalis. Extant Anatini, on the other hand, have a very robust shaft.

Material. In addition to the holotype, from the type locality: PIN, no. 4869/56, distal fragment of the
left humerus; 4869/191, 239, cranial fragments of right coracoids.

Fred
 
Mioquerquedula soporata (Kurochkin, 1976), comb. nov.

Anas soporata: Kurochkin, 1976, p. 61, text-fig. 8; 1985, p. 43, text-fig. 18, pl. 5, figs. 1–6 (part.); Zelenkov and Kurochkin, 2012, p. 92, text-figs. 1b, 1c, pl. 17, fig. 3; 2015, p. 171, pl. 15, figs. 23–25.
Dendrocygna soporata: Mlíkovský and Švec, 1986, p. 262. Anatinae gen. indet.: Zelenkov and Kurochkin, 2012, p. 94.
Anas velox (part.): Cheneval, 1987, p. 142, non pl. 1, figs. 2–4; 2000, p. 32; Mlíkovský, 2002, p. 118.

Holotype. PIN, no. 2614/95, cranial half of right coracoid; Mongolia, Gobi-Altai aimag, Shargain-Gobi, Sharga locality; uppermost middle Miocene, Oshin Formation

Description. In the humerus, the tuberculum dorsale is subtriangular and slightly elevated above the
plane of the bone; the caudal shaft ridge is not strongly pronounced and is oriented towards the tuberculum dorsale; the proportions of the humerus are shortened; bone shaft moderately gracile; the fossa brachialis is close to the tuberculum supracondylare ven- trale; the epicondylus dorsalis is well defined, but not large. The coracoid has a groove passing from the medial edge of the shaft to the ventral surface of the sternal expansion; the impressio m. supracoracoidei is moderately expressed; general proportions shortened; see also the description of the coracoid in Zelenkov and Kurochkin (2012).

Comparison. It differs from M. minutissima in the slightly larger size (corresponding to modern Nettapus coromandelianus or the smallest specimens of Anas crecca), craniocaudally somewhat more elongated (advanced character), and medially significantly more strongly protruded (plesiomorphic character) processus acrocoracoideus of the coracoid.

Remarks. Anas soporata is assigned here to the genus Mioquerquedula on the basis of the similar structure of the processus acrocoracoideus, cotylascapularis, processus procoracoideus and generally
similar coracoid proportions to M. minutissima. Previously, only fragmentary coracoids were reported for Anas soporata (Zelenkov and Kurochkin, 2012, 2015); however, the revision made it possible to attribute several fairly complete specimens from the type locality of Sharga to this species. Based on these coracoids (as well as the almost complete specimen MNHN, SA 10283 from Sansan), it can be seen that the coracoid of Anas soporata was shortened compared to that of modern Anatini, somewhat like that of Nettapus. While the length of the glenoid articular part (facies articularis humeralis + cotyla scapularis) is similar, the length of the bone (from the apex of the processus procoracoideus to the angulus medialis) is noticeably shorter in Mioquerquedula than in Anas s.l. In extant Nettapus, the coracoid is shortened somewhat more than in Mioquerquedula; an even shorter coracoid occurs in Malacorhynchus, which M. soporata resembles somewhat in the morphology of the processus acrocoracoideus. Previously, one of the distinguishing features of M. soporata was considered to be the presence of a pneumatic opening under the facies articularis clavicularis (Zelenkov and Kurochkin, 2012). We attribute the presence of this opening in the M. soporata holotype to variability (probably intrageneric), since individual variability in the development of pneumatization was found in extant Nettapus (our data). It should be noted that significant variability of the acrocoracoid part also characterizes the coracoids of M. minutissima (see above). It is possible that M. soporata may actually represent a separate anatid genus (this may be indicated by a slightly longer processus acrocoracoideus, an advanced character for Anatinae), but the general morphological similarity of
M. soporata and M. minutissima and their identical age indicates at least their equal evolutionary grade, and likely close affinity. A judgement about the generic independence of M. soporata would still be premature, but can be later confirmed by additional evidence for oth species. First and foremost, it seems important to note the incorrectness of assigning M. soporata to the Anas s.l. group, as was done earlier (Kurochkin, 1985; Zelenkov and Kurochkin, 2012, 2015).
The proximal humerus from Sharga (PIN, no. 4869/107) is here assigned to this species. Although poorly preserved, it reliably differs from Anas in the subtriangular tuberculum dorsale, as in primitive ducks (in Anas, this tubercle is always elongated). The short and raised tuberculum dorsale also characterizes Mioquerquedula sp. from the Rudabánya locality (Zelenkov, 2017). In these humeri, a slightly pronounced caudal shaft ridge is visible, oriented towards the tuberculum dorsale, while in Anas s.l. this
ridge is not expressed. An incomplete humerus from Sharga (PIN, no. 4869/54), also assigned to M. soporata here, corresponds in size to N. coromandelianus, as does the holotype. PIN, no. 4869/54 differs from Anas s.l. in the noticeably less robust shaft (a plesiomorphic feature for Anatinae) and its shortening: while absolute dimensions of the distal end are similar to those of small specimens of extant A. crecca, this humerus is shorter (the distance from the distal margin to the distal point of the crista deltopectoralis is 10% shorter in M. soporata).
Further, a number of bones from the Sansan locality are here attributed to M. soporata, including the
coracoid (MNHN, no. SA 10283) that is almost identical to the holotype of A. soporata both in morphology and in size. This specimen is characterized, among other things, by the presence of a groove passing onto the ventral surface of the bone, as in M. minutissima. The only difference between MNHN, no. SA 1232 and the holotype of M. soporata is the shape of the base of the processus acrocoracoideus in ventral view: in the holotype of M. soporata, the angle between the impressio bicipitalis and the adjacent part of the shaft at the level of the facies articularis humeralis is smoothed out, while in MNHN, no. SA 10283 it is cut, resulting in an angular notch. This difference most likely is a feature of intraspecific variability, as variations in the shape of the caudal edge of the processus acrocoracoideus are characteristic of the coracoids of M. soporata from Sharga and extant anatids.
The scapula (PIN, no. 4869/80) corresponds in size to that of extant N. coromandelianus and A. crecca.
This specimen is characterized by a relatively short acromion, as in modern Nettapus, and, apparently, unpronounced curvature (however, the latter feature is difficult to assess due to the incomplete preservation of the bone shaft). Almost complete (without os metacarpale minus) carpometacarpi from Sharga (PIN, no. 4869/242) and Sansan (MNHN, no. SA 1250) are tentatively attributed here to M. soporata: they are very similar in size and proportions, in the orientation of the processus extensorius, the length of the distal symphysis, and other features. The weathered nature of PIN, no. 4869/242, apparently explains the somewhat smaller proximal width of this specimen compared to MNHN, no. SA 1250. In the size of the proximal end, PIN, no. 4869/242 corresponds to extant N. coromandelianus, but is somewhat elongated and has a slightly thinner os metacarpale major. The general proportions of carpometacarpus are similar to those of Anatini. This specimen is similar to Nettapus and Anas and
differs significantly from Oxyurinae in the high processus extensorius and the elongated symphysis distalis. Advanced features indicating its attribution to Anatinae include the presence of a well-defined notch in the dorsal margin of the trochlea carpalis in caudal view and a proximodistally shortened base of the os metacarpale alulare (in Oxyurinae, in particular, the base of the os metacarpale alulare is elongated, the processus extensorius is low, and the notch in the dorsal margin of the trochlea carpalis is unpronounced). Importantly, the dorsal margin of the trochlea carpalis protrudes proximally only slightly more than the ventral one (this is clearly seen when viewed caudally and ventrally), as in Anas s.l. and unlike the Mergini, but more than in Mionetta. This specimen also differs from Mionetta in a number of features: the ventral surface of the processus extensorius and the proximal end is not concave (concave in Mionetta), on the caudal surface of the os metacarpale minus near its base there is a fossa (unpronounced in Mionetta), the fossa infratrochlearis caudalis is barely expressed and small (deep in Mionetta, Oxyurinae and Mergini). All these characters make this specimen similar to Anatinae.
Several bones were previously incorrectly identified as Anas/Mioquerquedula (Zelenkov and Kurochkin, 2012). The femur (PIN, no. 4869/5) belongs to the Strigidae; another femur (PIN, no. 4869/99) also does not belong to Anatidae and, apparently, represents Phasianidae. PIN, no. 4869/19, fragment of an ulna, also does not belong to Anatidae.

Range. Middle Miocene of France (Sansan; MN 6) and Mongolia (Sharga; MN 7+8).

Material. From the type locality, in addition to the holotype: PIN, nos. 4869/71, 102, 144, 189, 192, 240, 243, 244, incomplete left coracoids; 4869/156, 159, 246, incomplete right coracoids; 4869/80, left incomplete scapula; 4869/107, proximal ends of right humeri; 4869/54, incomplete left humerus; 4869/25, distal epiphysis of the right humerus; 2614/119, proximal half of right ulna; 4869/242, right carpometacarpus; 4869/241, distal fragment of the right carpometacarpus. From Sansan, France: MNHN, no. SA 10283, right coracoid; SA 1250, right carpometacarpus; SA 1213, distal half of the left tibiotarsus.

Fred
 

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