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Mioquerquedula palaeotagaica sp. nov; Tagayanetta palaeobaikalensis gen. et sp. nov.,; Selenonetta lacustrina gen. et sp. nov. (1 Viewer)

Fred Ruhe

Well-known member
Netherlands
Nikita V. Zelenkov, 2023

SMALL DUCKS (AVES: ANATIDAE) FROM THE EARLY–MIDDLE MIOCENE OF EURASIA. 2. THE FAUNA OF TAGAY LOCALITY (BAIKAL AREA; EASTERN SIBERIA)

Paleontological Journal. 57 (5): 82–93 (Russian version)

Abstract: https://www.elibrary.ru/item.asp?id=54238524

Remains of small ducks are described from the boundary early–middle Miocene deposits of Tagay (Baikal area), the only locality in Asia with a representative bird fauna of the Miocene climatic optimum. New taxa Mioquerquedula palaeotagaica sp. nov. and Tagayanetta palaeobaikalensis gen. et sp. nov., corresponding in size to modern Anas crecca, as well as an even smaller duck Selenonetta lacustrina gen. et sp. nov. are described. A revision of the genus Mioquerquedula is undertaken; “Anasintegra Miller, 1944 from the Lower Miocene of North America is here transferred to this genus. Tagayanetta gen. nov. is here considered as an evolutionarily more advanced genus than Mioquerquedula, probably close to Anatini. Selenonetta gen. nov. is considered as a taxon close to the divergence between Mergini and other Anatinae. A similar form (possibly the same species) is present in the Sansan locality (France).

More to come when the English version is out

Enjoy,

Fred
 
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You can find the free pdf at: https://www.researchgate.net/public..._Tagay_Locality_Baikal_Region_Eastern_Siberia

Reference for the English editiuon: Paleontological Journal, 2023, Vol. 57, No. 5, pp. 560–572.


SYSTEMATIC PALEONTOLOGY

CLASS AVES
Order Anseriformes
Family Anatidae Leach, 1820
Genus Mioquerquedula Zelenkov et Kurochkin, 2012

Type species: Mioquerquedula minutissima Zelenkov et Kurochkin, 2012.

Diagnosis (emended). In the coracoid, the plane of the ventral surface of the processus acrocora-
coideus is subparallel to the plane of the extremitas sternalis; facies articularis clavicularis is nonconcave,
overhanging sulcus m. supracoracoidei; groove between the processus procoracoideus and ventral
margin of the coracoid shaft caudally extends to the ventral surface of the bone; a shallow but well-defined depression (impressio m. supracoracoidei) is developed on the ventral surface of the extremitas sternalis; the ventral margin of the facies articularis humeralis forms a pronounced ventrocaudal angle (facies profile is unevenly oval); extremitas sternalis expands gradually; the medial margin of the shaft is slightly concave at the transition to the extremitas sternalis.

Species composition. M. integra (Miller, 1944) comb. nov., Early Miocene of the United States; M. palaeotagaica sp. nov., the end of the Early Miocene of the Baikal Region; M. soporata (Kurochkin,
1976), Middle Miocene of France and Mongolia; M. minutissima Zelenkov et Kurochkin, 2012, Middle
Miocene of Mongolia.

Remarks. The genus Mioquerquedula was erected for the tiny duck M. minutissima from the Middle Miocene of the Sharga locality in Mongolia. Initially, Anas velox from the Middle Miocene of France
was also tentatively included in the genus (Zelenkov and Kurochkin, 2012); however, a direct study of
materials on the French species made it possible to exclude A. velox from Mioquerquedula (Zelenkov and Kurochkin, 2015). Based on the results of this revision, A. velox was transferred to Mergini; however, a number of materials from Sansan are indeed identified as Mioquerquedula (Zelenkov, 2023). Small ducks from the Middle Miocene of the North Caucasus and the lowermost Upper Miocene of Hungary (Zelenkov, 2017a, b) and Germany (Mayr et al., 2022) were also tentatively identified as Mioquerquedula sp. It was pointed out that the fauna of the Sharga locality contained another unnamed species of the genus; these materials have now been reidentified as Mioquerquedula soporata (Zelenkov, 2023). At least two species of Mioquerquedula were mentioned for the fauna of the Tagay locality (Zelenkov and Martynovich, 2013; Zelenkov and Kurochkin, 2015); here one of them is described as M. palaeotagaica sp. nov.
Mioquerquedula has a slightly shorter coracoid than modern Anas s.l. and comparable with that of Nettapus: at a similar length of the glenoid articular part (facies articularis humeralis + cotyla scapularis), the bone length (from the top of the processus procoracoideus to the angulus medialis) is noticeably smaller in Nettapus and Mioquerquedula (even smaller in Malacorhynchus) than in Anas s.l. Modern Anas s.l. also have a more elongated processus acrocoracoideus than Mioquerquedula and Nettapus. At the same time, the coracoid of Mioquerquedula is somewhat longer than that of Nettapus. The length of the coracoid is one of the most stable parameters of the postcranial skeleton in modern dabbling ducks, which we associate with the general requirements of the flying apparatus (our data; Zelenkov, 2022). The relatively short coracoid of Mioquerquedula (partially resembling that of the modern tropical Nettapus) indicates a distinct flying specialization of these ducks and may be linked to a somewhat limited flight ability compared to modern Anas. Apparently, representatives of the genus Mio-
querquedula
were not capable of long-distance migrations, which may explain their disappearance due to climate cooling in the temperate zone of Eurasia in the second half of the Late Miocene.
The small duck Anas integra Miller, 1944, described from a coracoid from the Lower Miocene of the United States, is very similar to M. soporata in the structure of the humeral part of the coracoid (proces-
sus acrocoracoideus is relatively elongated and set back medially and overhangs the sulcus m. supracoracoidei; the surface of the sulcus is concave; and cotyla scapularis is subtriangular and laterally displaced), but differs in a noticeable expansion of the bone at the transition to the extremitas sternalis; therefore, the coracoid was similar to that of Mionetta natator (Miller, 1944) in general proportions. At the same time, the North American form differs from Mionetta natator in the reduced cotyla scapularis (an apomorphic state within Anatidae) (as in the other species of Mioquerquedula) and is treated here as Mioquerquedula integra (Miller, 1944) comb. nov. The similarity with M. natator in the structure of the extremitas sternalis of the coracoid is interpreted as a plesiomorphy.

Mioquerquedula palaeotagaica Zelenkov, sp. nov.
Mioquerquedula sp.: Zelenkov and Martynovich, 2012, p. 14; 2013, p. 80; Zelenkov and Kurochkin, 2015, p. 170.

Etymology. From the Tagay location and Greek παλαιός (ancient).

Holotype. PIN, no. 2614/177, cranial fragment of the right coracoid; Russia, Lake Baikal, Olkhon Island, Tagay locality (horizon A; Sizov and Klement’ev, 2015); uppermost Lower Miocene, Tagay Formation.

Material. In addition to the holotype, specimens from the type locality: specimen PIN, nos. 2614/447,
fragmentary right coracoid; 2614/199, incomplete left scapula; 2614/454, and incomplete right scapula, all from horizon “E”; 2614/458, proximal fragment of the left carpometacarpus, presumably horizon “A”;
2614/390, proximal fragment of the right carpometacarpus, horizon “E”; 2614/388, distal fragment of the left carpometacarpus, horizon “C”; 2614/397, distal fragment of the right carpometacarpus; 2614/386, distal fragment of the left tibiotarsus, both from horizon “E”; 2614/339, right tarsometatarsus, horizon “C”.

Comparison. The coracoid corresponds in size to M. soporata (they have a similar size of the articular
glenoid part), but is more massive; however, it has a shorter and less medially protruding processus acrocoracoideus; the shaft expands evenly caudally, starting from the central part (in M. soporata, the caudal expansion of the shaft is less pronounced). When viewed from the lateral side, impressio lig. acrocoracohumeralis noticeably shorter than facies articularis humeralis (while they are comparable in M. soporata). It is noticeably larger than M. minutissima. Differs from M. integra in the expansion of the shaft, starting from the central part (in M. integra, the central part of the shaft is even, without expansion). This comparison constitutes the diagnosis of the new species.

Remarks. Materials on small ducks from Tagay, which are comparable with modern Nettapus coro-
mandelianus
and Middle Miocene M. soporata in proportions and absolute sizes, are assigned to M. palaeotagaica sp. nov. The morphological similarity of Mioquerquedula with Nettapus (Zelenkov and Kurochkin, 2012) suggests at least close proportions of limb elements in these two genera; based on this fact, I distinguished the materials between two similarly-sized species from Tagay: M. palaeotagaica and Tagayanetta palaeobaikalensis gen. et sp. nov. Both species have coracoids similar in absolute size (which is best pronounced in the length of the glenoid articular part: facies articularis humeralis + cotyla scapularis); however, the tarsometatarsus attributed to M. palaeotagaica (specimen PIN, no. 2614/339) is somewhat shorter and has a noticeably smaller size of the articular surfaces. The small tarsometatarsus relative to the bones of the shoulder girdle and forelimb is also characteristic of the modern genus Nettapus.
Similarly to the holotype, the almost complete tarsometatarsus without trochlea metatarsi IV (specimen
PIN, no. 2614/339) corresponds in absolute size to modern Nettapus coromandelianus. The arsometatar-
sus is similar to that of Nettapus in morphology and proportions and differs from Anas s.l. in general shortening, as well as in subrectangular outlines of the cotyla medialis, which is trapezoidal in Anas s.l. owing to the truncated medioplantar angle. Fossil tarsometatarsus differs from that of Nettapus in a pointed eminentia intercotylaris and a distinct proximolateral expansion of the sulcus flexorius, which partly reaches the lateral surface of the bone and forms a shallow fossa parahypotarsalis lateralis (also visible from the lateral side). In Nettapus, Anas s.l., and other ducks, fossa parahypotarsalis lateralis is absent or indistinctly pronounced.
The right scapula (specimen PIN, no. 2614/454) is comparable in size to modern Nettapus coromande-
lianus
and only slightly smaller than specimen PIN, no. 4869/80 assigned to M. soporata from Sharga, with which it is similar in the shortened acromion. The degree of preservation of this specimen suggests a rather pronounced curvature of the bone.
The fragmentary carpometacarpus (specimen PIN, no. 2614/458) is assigned to this species based on
the relative size (corresponding to N. coromandelianus) and a general structural similarity with Netta-
pus
. The fairly tall processus extensorius with a narrow base distinguishes this specimen from the carpometacarpi tentatively assigned to M. soporata. Specimen PIN, no. 2614/390 is similar to the previous specimen in deep depressio muscularis interna and dimensions. The distal fragment of the carpometacarpus (specimen PIN, no. 2614/338) is morphologically similar to the carpometacarpus of M. soporata and corresponds in size to specimen no. PIN, no. 2614/458. The distal fragment of the tibiotarsus (specimen PIN, no. 2614/386) completely corresponds in size to the tarsometatarsus assigned to this species (slightly smaller than T. palaeobaikalensis); it is characterized by a very slightly curved medially distal end, which is low in distal view (high and strongly medially curved in Nettapus); it is similar in general morphology to the tibiotarsi of Aythyini. The degree of curvature of the distal end is more significant in M. soporata from Sansan (Zelenkov, 2023); however, the distal profile of both specimens is the same.

Fred
 
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Genus Tagayanetta Zelenkov, gen. nov.

Etymology. From the Tagay Bay on the Olkhon Island (Lake Baikal) and Netta (the modern genus
of Anatinae).

Type species. Tagayanetta palaeobaikalensis sp. nov.

Diagnosis. Coracoid has a gracile outline; processus acrocoracoideus is oriented largely cranially and very slightly deviates medially; facies articularis humeralis has a rounded ventral margin and nonacute
cranial angle; facies articularis clavicularis has a welldefined notch in the caudal margin, does not overhang the cranial part of the sulcus m. supracoracoidei; in medial view, the ventral margin of the shaft is ventrally convex at the level of the processus procoracoideus and bent dorsally in the cranial part.
In tarsometatarsus, the shaft is narrowed in the central part; lateral dorsal crest is hardly pronounced;
cotyla lateralis is slightly protruding dorsally; crista medialis hypotarsi is unthickened; the dorsal part of
cotyla lateralis has no distinct transition to the dorsal surface of the bone; the proximal end is wide in proximal view; cotyla medialis is expanded and has a moderately cut mediaplantar angle; the proximal margin of the hypotarsus is obliquely oriented in medial view; the lateral margin of the shaft does not expand evenly distally, forming a slight expansion proximal to the trochlea metatarsi II.

Species composition. Type species.

Comparison. Coracoid is similar to that of Anas s.s in shaft proportions and the shape of facies articularis humeralis and facies articularis clavicularis, as well as in the orientation of the processus acrocoracoideus, but differs in a slightly shorter processus acrocoracoideus. Differs from the coracoid of Mioquerquedula in a more gracile shaft [at similar dimensions of the glenoid articular part (facies articularis humeralis + cotyla scapularis) in M. palaeotagaica sp. nov. and T. palaeobaikalensis gen. et sp. nov.], a dorsoventrally more convex facies articularis humeralis with a more rounded ventral margin and a less acute cranial angle (in Mioquerquedula, the cranial angle of the facies is pointed), a more elongated (in particular, compared to M. palaeotagaica sp. nov.) and cranially oriented processus acrocoracoideus with a more elongated impressio lig. acrocoracoidei. The apex of the acrocoracoid is oriented more ventrally than medially in cranial view (in Mioquerquedula, in particular, in M. palaeotagaica, the apex of the process is oriented more medially). Facies articularis clavicularis is larger (craniocaudally higher) than that in Mioquerquedula in medial view; it has a distinct notch in the caudal margin (as in Anas s.l.) and does not overhang the cranial part of the sulcus m. supracoracoidei (while it moderately overhangs in M. palaeotagaica); crista acrocoracoidea is thinner than that in Mioquerquedula. The ventral margin of the shaft is convex at the level of the processus procoracoideus in medial view (as in Anatini), while it is straighter in Mioquerquedula.
Tarsometatarsus is relatively shorter than that in modern Anas s. s. (taking into account the size of the
articular parts) and has a shaft narrowed in the center, which makes it similar to Mergini (in particular,
Bucephala albeola). Outside Mergini, similar narrowing of the shaft is characteristic only of the genus
Lophonetta (see below). At the same time, it differs from Mergini (and other diving ducks, Oxyurinae and
Aythyini) in the absence of a hypertrophied dorsal lateral crest in the proximal part of the tarsometatarsus and in a slightly dorsally protruding cotyla lateralis (it is similar in these features to Anatini, in particular, Anas s. s.). It also differs from Mergini and Oxyurinae in the absence of the thickened and generally enlarged crista medialis hypotarsi (which makes it similar to Aythyini); in addition, the dorsal part of its cotyla lateralis does not clearly pass to the dorsal surface of the
bone (therefore, the cotyla lateralis looks cut off in Mergini and Oxyurinae in dorsal view and is some-
what displaced distally relative to the cotyla medialis; the same feature characterizes the fossil genus
Manuherikia, but not M. minuta). It also differs from Manuherikia (including M. minuta) by the proximal
end that is markedly more expanding relative to the shaft (primarily due to the cut off of the medial margin of the shaft). The expanded shaft generally characterizes the clade Oxyurinae, which includes Manuherikia (Worthy et al., 2022). In addition, the tarsometatarsus of M. minuta is characterized by a medially displaced lateral intermuscular ridge (line) in plantar view, while it extends along the lateral margin of the plantar surface of the bone in Tagayanetta. The shift of the plantar line in M. minuta begins in the proximal part of the shaft and therefore depends insignificantly from the view angle. The position of the intermuscular line, as in Tagayanetta, characterizes, in particular, modern Anatini. At the same time, Tagayanetta differs from Anatini in a narrowed shaft and a wide proximal end in proximal view, as well as in an expanded cotyla medialis with a moderately truncated mediaplantar angle (in Anatini, cotyla medialis is narrower and its medioplantar crest is markedly more significantly truncated). Tagayanetta differs from all studied Anatidae in the pronounced oblique orientation of the proximal
margin of the hypotarsus in medial view (in other members of the family, this margin is oriented subper
pendicular to the long axis of the bone).
The lateral margin of the shaft gradually expands at the transition to the trochlea metatarsi IV in the vast majority of ducks, while it forms a slight extension proximal to the trochlea metatarsi II and then some- what narrows in Tagayanetta. A somewhat similar morphology is characteristic of Nettapus; in Mergini and Netta, the extension of the shaft is located more distally, at the level of the trochlea metatarsi II. In Lophonetta, the narrowest part of the shaft is in its distal third, while the shaft of Tagayanetta is most significantly narrowed in the middle (proximal third). Distally, the lateral margin of the shaft in Lophonetta gradually deviates laterally, as in other Anatini. The articular surface of the trochlea metatarsi IV has a less pronounced notch in Lophonetta than in Tagayanetta.

Remarks. The structure of the tarsometatarsus of the new genus combines the narrowing of the central part of the shaft, which is characteristic of Mergini diving ducks, with the features of dabbling ducks (the
absence of the dorsally protruding and distally extending cotyla lateralis, as well as the absence of both
hypertrophied dorsal lateral crest, and hypertrophied crista medialis hypotarsi). The predominance of the latter unequivocally indicates the absence of pronounced diving adaptations in Tagayanetta. The
absence of the hypertrophied crista medialis hypotarsi and the presence of the moderately developed dorsal lateral ridge characterize the modern genus Netta; however, the dorsal margin of the cotyla dorsalis extends distally along the dorsal surface of the bone even in Netta, a poorly specialized diver. This structure of the articular surface contributes to the preservation of the articulation between the tibiotarsus and tarsometatarsus in the most flexed state of the latter (i.e., when the tarsometatarsus is protracted, or “overextended”), which characterizes the specialized swimming (or diving) type of the intertarsal joint of ducks (Zelenkov, 2020b). Therefore, Tagayanetta appears to be even less specialized for diving than Netta and the presence of the narrow shaft characteristic of the new genus (as in Mergini) has not yet been explained. Ecomorphological analysis correlates the most gracile tarsometatarsus with terrestrial locomotion in Anatidae and the most robust tarsometatarsus with diving (De Mendoza and Gomez, 2022). Other Oligocene–Miocene anatids (including Pinpanetta and Manuherikia) also have a much more expanded tarsometatarsal shaft (Worthy, 2009; Worthy et al., 2022). At the same time, the narrowed shaft is characteristic of the modern genus Lophonetta, the divergence of which and related taxa is dated to no earlier than the very end of the Miocene (Mitchell et al., 2014; Sun et al., 2017).
With respect to the structure of the coracoid, Tagayanetta is close to Anatini; at the same time, the
partial similarity of Tagayanetta with diving ducks in the structure of the tarsometatarsus may indicate the origin of Anatini from at least moderately diving ducks. Tarsometatarsi similar in morphology to those of Tagayanetta are unknown from the Middle Miocene of the Sharga locality, from which three fossil genera of diving ducks are described. At the same time, a narrowed tarsometatarsus is also recorded in modern nondiving Anatini (e.g., Lophonetta).

Tagayanetta palaeobaikalensis sp. nov.

Etymology. From Lake Baikal and Greek παλαιός (ancient)

Holotype. PIN, no. 2614/337, incomplete left coracoid; Baikal Region, Tagay locality; Lower–Middle Miocene; horizon “E”.

Material. In addition to the holotype, specimens from the type locality: specimen PIN, nos. 2614/393, apex of the maxillary rostrum, horizon “E”; 2614/338, incomplete left coracoid, horizon “C”; 2614/341, incomplete left coracoid, presumably horizon “E”; 2614/459, incomplete right coracoid, horizon “A”; 2614/463, incomplete left scapula; 2614/342, proximal fragment of the left humerus; no. 2614/389, incomplete right carpometacarpus; 2614/398, distal fragment of the right carpometacarpus, all from horizon “E”; PIN 2614/340, right tarsometatarsus, presumably horizon “C”.

Remarks. To this species I refer materials on a small duck, which are comparable to medium-sized
specimens of modern A. crecca in absolute and relative dimensions. The coracoid (holotype) differs from A. crecca mainly in a somewhat shortened processus acrocoracoideus and an oblique mediocaudal angle of the cotyla scapularis; at the same time, it has a similar structure of the facies articularis clavicularis (it has a well-defined notch in the central part). The holotype is also similar in absolute dimensions to M. palaeotagaica from the same locality and differs from it in a number of morphological details, which were mentioned above in the diagnosis of the new genus. Tarsometatarsus is also similar to that of Anas crecca in the size of the articular parts, which indicates the close overall dimensions of the bird (in A. crecca, the width of the proximal end is 5.6–6.3, as in T. palaeobaikalensis); at the same time, it is shorter than that in Anas, but longer and has a larger size of the articular parts than the tarsometatarsus attributed to M. palaeotagaica (see above).
Another fragmentary coracoid (specimen PIN, no. 2614/341) is similar to the holotype in the cranial
orientation of the acrocoracoid process and is therefore assigned to this species. This specimen differs
from the holotype in the dorsoventrally narrower facies articularis clavicularis, which less significantly
overhangs the sulcus m. supracoracoidei and has a small depression in the dorsal part, which is absent in the holotype. These differences are treated as individual variations. Another fragmentary coracoid (specimen PIN, no. 2614/459) is assigned to this taxon based on a similar shape of the cotyla scapularis (the mediocaudal angle is distinctly oblique, as in the holotype; in M. palaeotagaica, it is more rounded) and processus procoracoideus (nonconvex caudal margin; convex in M. palaeotagaica).
An incomplete left coracoid from the type locality (specimen PIN, no. 2614/338) with a preserved ster-
nal part is also tentatively assigned to this species. This specimen is characterized by a very wide processus procoracoideus with a strongly convex mediocaudal margin (this feature distinguishes this specimen from the holotype of M. palaeotagaica, in which the process is noticeably smaller). The exact structure of the processus procoracoideus is unknown for the T. palaeobaikalensis holotype; however, it was apparently not as wide as that in specimen no. PIN, no. 2614/338. The difference in the structure of the procoracoid process can be attributed to individual variability (a similar morphology of the procoracoid process was found as an individual variation in Histrionicus histrionicus).
Also, specimen PIN, no. 2614/338 is somewhat more gracile than the holotype of M. palaeotagaica and has a beveled cotyla scapularis, as in the holotype of T. palaeobaikalensis. This coracoid is similar in pro-
portion to that of M. soporata (in particular, specimen PIN, no. 4869/189) and somewhat shortened compared to that of modern Anas. At the same time, it differs from the coracoid of Mioquerquedula in the oblique orientation of the facies articularis sternalis and a greater medial expansion of the extremitas sternalis. Angulus medialis has a markedly smaller base than that of Mioquerquedula. Impressio m. sternocoracoidei is much smaller than that of Mioquerquedula.
The left scapula (specimen PIN, no. 2614/463) is approximately of the same size as specimen no. PIN,
no. 2614/454, which is assigned to M. palaeotagaica, but differs from it in a shorter facies articularis humeralis, a more pronounced tuberculum brachiale, and a longer and cranially oriented acromion. The general curvature of the shaft is less pronounced than that in specimen no. PIN, no. 2614/454. This specimen is similar to Anatini in the shape and orientation of the acromion and is therefore assigned here to this species.
A proximal fragment of the humerus is known from Tagay (specimen PIN, no. 2614/342), which is here
tentatively attributed to this species. Similarly to other elements, it corresponds in absolute dimensions to the smallest specimens of modern A. crecca, from which it differs in a slightly raised, shortened, and subtriangular (with a flattened dorsal apex) tuberculum dorsale, a pronounced caudal shaft ridge oriented to this tubercle, and a moderately deep fossa tricipitalis dorsalis located ventral to the tubercle, as well as in a hardly pronounced pneumatization of the fossa pneumotricipitalis. This set of features corresponds to the basal position relative to Tadornini + Aythyini + Anatini (in which the ridge and fossa are unpronounced), which corresponds to the time of divergence of these clades (the end of the Middle Miocene) and also generally agrees with the evolutionary level of Mioquerquedula.
The caudal shaft ridge and the dorsal tricipital fossa in specimen no. PIN, no. 2614/342 look more pronounced and the shape of the tuberculum dorsale is more smoothed (distinctly less triangular as a result of the flattening of the dorsal angle and some elongation) than that in the specimen from Sharga assigned to M. soporata.
Carpometacarpi are poorly diagnostic in most anatids; therefore, it is difficult to assign specific specimens to certain taxa. The most robust of the specimens (PIN, no. 2614/389) known from Tagay is here assigned to this species. With respect to the size of the proximal end and the thickness of the large metacarpal, this specimen is also similar to the smallest specimens of modern A. crecca, as with other elements of the skeleton of T. palaeobaikalensis; however, it differs in some shortening, which can be explained by an absence of long-distance migrations and, as a consequence, a somewhat shorter manus in this Miocene species. At the same time, this specimen is longer than the carpometacarpus from Sansan, which I attribute to M. soporata. Specimen PIN, no. 2614/389 is also significantly larger than that of N. coromandelianus and can hardly be assigned to M. palaeotagaica, taking into account the osteological and proportional similarities between Mioquerquedula and Nettapus. The distal fragment (specimen PIN, no. 2614/398) corresponds in thickness to specimen no. PIN, no. 2614/389; it differs from the carpometacarpus of M. soporata in a shortened distal symphysis. Several even smaller carpometacarpi are known from Tagay; however, their assignment to T. palaeobaikalensis would assume a pronounced shortening of the manus in this taxon, which seems unlikely, taking into account the weak
degree of diving adaptations in this species, as follows from the structure of the tarsus (see the relationship between diving and flying adaptations in water birds in Zelenkov, 2015).
The slightly larger size of the carpometacarpus of T. palaeobaikalensis than that in M. palaeotagaica may
be correlated with an elongated impressio lig. acrocoracohumeralis in the former species. The acrocoraco-humeral ligament attached to the above-mentioned imprint serves as a critical component in the transmission of forces from the forelimb to the trunk (Baier et al., 2007); therefore, an increase in the imprint (and, in general, processus acrocoracoideus) may reflect an increase in the whole forelimb. For example, the modern Malacorhynchus ducks, which are similar to Nettapus in the evolutionary level of coracoid structure, have a longer processus acrocoracoideus and, accordingly, impressio lig. acrocoracohumeralis, which is correlated with the general elongation of the forelimb in this taxon.
A terminal fragment of the maxillary rostrum is known from Tagay (specimen PIN, no. 2614/393), which is comparable to modern A. crecca in size. This specimen is characterized by a flattened ventral sur-
face and a weakly convex dorsal surface; this distinguishes this rostrum from modern Nettapus (which have a narrowed, dorsally convex, and ventrally concave rostrum) and suggests its relationship with Anatini.

Fred
 
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Genus Selenonetta Zelenkov, gen. nov.

Etymology. From Selene (ancient Greek Goddess of the moon) and Netta (the modern duck genus).

Type species. Selenonetta lacustrina sp. nov.

Diagnosis. In the humerus, incisura capitis does not form a notch in the ventroproximal profile of
the bone (between the caput humeri and the ventral margin of the tuberculum ventrale); the distance from the dorsal margins of the crus dorsale fossae to the caudal shaft ridge is noticeably smaller than the dorsoventral width of the fossa pneumotricipitalis at this level; the caudal shaft ridge is fairly well defined and oriented between the tuberculum dorsale and caput humeri; the cross section of the shaft is subtriangular; tuberculum dorsale is clearly elongated; its distal corner is sharp and “lowered” to the shaft level; crista deltopectoralis is short (its length is comparable with the dorsoventral width of the proximal end); its dorsal surface is moderately concave; crus dorsale fossae is dorsoventrally oriented and tuberculum ventrale is caudally oriented; fossa pneumotricipitalis is nonpneumatized; caput humeri moderately overhangs the dorsal surface of the shaft.

Species composition. Type species.

Comparison. The humerus of Selenonetta is characterized by the combination (unique to Anatidae) of an elongated tuberculum brachiale, the absence of the notch of the incisura capitis in the ventroproximal profile of the bone, as well as by a nonpneumatized fossa pneumotricipitalis and a narrow distance between the crus dorsale fossae and caudal shaft ridge (narrow dorsal tricipital fossa). The absence of the incisura capitis notch is apparently a plesiomorphic feature for Anatidae, which is characteristic, in particular, of the Oligocene genus Pinpanetta (Worthy, 2009). At the same time, Pinpanetta has a long crista deltopectoralis and a short and high (caudally protruding) tuberculum dorsale (as in modern Dendrocygninae), while the crista deltopectoralis in Selenonetta is shortened and its tuberculum dorsale is elongated and has a pointed and lowered distal angle. The latter feature is an advanced one characterizing Anatinae. With respect to the width of the dorsal tricipital fossa and the whole outline of the proximal end, Selenonetta is closest to Nettapus, from which it differs in the non-pneumatized fossa pneumotricipitalis (pneumatized in Nettapus) and the above-mentioned absence of the incisura capitis notch. The caudal shaft ridge is noticeably less pronounced in Nettapus than in
Selenonetta. Selenonetta differs from the fossil genus Helonetta (which is also similar to Nettapus Emslie,
1992)) in the absence of the incisura capitis notch and an elongated tuberculum dorsale. As can be judged from the description (Emslie, 1992), Helonetta does not differ from Nettapus in the structure of the fossa pneumotricipitalis.
The combination of an elongated tuberculum dorsale and a non-pneumatized fossa pneumotricipitalis
is present in modern Mergini (except Mergus, in which this fossa is pneumatized), from which Selenonetta differs in a narrow dorsal tricipital fossa, the absence of the notch of the incisura capitis, and the caudal orientation of the tuberculum ventrale (in Mergini, this tubercle is oriented more distally and overhangs the fossa pneumotricipitalis). It also differs from the fossil genus Protomelanitta (supposed basal Mergini; Zelenkov, 2011; Stidham and Zelenkov, 2017) in a narrow dorsal tricipal fossa and the absence of the incisura capitis notch, an expanded caput humeri, and an elongated tuberculum dorsale.

Remarks. The diagnosis of the genus is based on the proximal end of the humerus, which is a highly diagnostic element of the skeleton of Anatidae and, in particular, has a characteristic morphology in Selenonetta. See the description of other bones below in the description of the type species.
The humerus of Selenonetta demonstrates a combination of plesiomorphic and progressive traits, which
is not characteristic of other modern and fossil ducks, thereby making it difficult to assess the phylogenetic position of this taxon. The combination of the elongated tuberculum brachiale and closed (non-pneumatized) fossa pneumotricipitalis brings Selenonetta close with Mergini and Aythya; however, the absence of the notch of the incisura capitis indicates the basal position of this fossil genus not only with respect to Mergini but also with respect to all Anatinae. The absence of the pneumatization of the fossa pneumotricipitalis may also prove to be a plesiomorphic feature characterizing, in addition to Mergini (apparently, the basal representatives of Anatinae; Sun et al., 2017), also Oxyurinae and Malacorhynchus. At the same time, the general structural similarity with Nettapus can be considered as an advanced feature indicating the attribution of Selenonetta to the basalmost radiation of Anatinae. The humerus of Mioquerquedula minutissima, the type species of the genus Mioquerquedula, is unknown (Zelenkov, 2023); however, the humerus of the somewhat larger species M. soporata morphologically significantly differs in the presence of a distinct notch of the incisura capitis (an advanced feature with respect to Selenonetta) and a short subtriangular tuberculum dorsale (a primitive
character with respect to Selenonetta).
Very small coracoids from Tagay, which are here assigned to Selenonetta lacustrina, differ from similarly
sized M. minutissima in general outlines. As in modern Anatini, the caudal (sternal) expansion of the shaft in M. minutissima is moderately developed, while it is distinct in S. lacustrina, which is expressed in a noticeable concavity of both margins (in particular, the medial one) of the central part of the coracoid. The outlines of the coracoid shaft indicate that, with respect to the morphology of the sternal expansion, the coracoid of S. lacustrina was closer to Malacorhynchus and early Miocene “Mionetta” natator than to Anatini and Mioquerquedula soporata. In turn, this indicates a distinct evolutionary level of the Selenonetta coracoid and confirms the separate generic status of the smallest duck from Tagay. The structure of the carpometacarpus also distinguishes Selenonetta from Mioquerquedula.

Selenonetta lacustrina Zelenkov sp. nov.
Mioquerquedula sp.: Zelenkov, Martynovich, 2012, p. 14; 2013, p. 80; Gorobets, 2013, p. 72; Zelenkov and Kurochkin, 2015, p. 170.

Etymology. From Latin lacustris (lacustrine).

Holotype. NMNHU-P No Av-52, proximal fragment of the left humerus; Baikal Region, Tagay locality; Lower–Middle Miocene; material collected by N.A. Logachev, 1957–1958.

Material. In addition to the holotype, specimens from the type locality: specimen PIN, nos. 2614/198, proximal fragment of the right humerus, horizon “E”; 2614/181, 193, two incomplete coracoids; 2614/180, left scapula (all from horizon “A”); 2614/385, proximal fragment of the right carpometacarpus, horizon “E”; 2614/396, proximal fragment of the left carpometacarpus, horizon “A”; 2614/392, distal end of the right tibiotarsus, horizon “E”; and 2614/365, fragmentary shaft of the left tarsometatarsus, horizon “C”.

Species composition. The genus Selenonetta includes one species.

Remarks. The remains of the tiniest duck among the small ducks from Tagay (on the lower size limit for the family Anatidae) were assigned to this species. With respect to the absolute dimensions, this form is comparable to modern Nettapus auritus or Spatula hottentota, but distinctly smaller than Anas crecca and, apparently, slightly smaller than M. minutissima. This form was previously designated as Mioquerquedula sp. 2 (Zelenkov and Martynovich, 2013; Zelenkov and Kurochkin, 2015); however, the morphology of the humerus and coracoids of the smallest duck from Tagay indicates its separate generic status (see above).
In addition to the holotype, another very small proximal humerus is known from Tagay (specimen
PIN, no. 2614/198), which is assigned here to S. lacustrina. In specimen PIN, no. 2614/198, tuberculum
dorsale is incompletely preserved; however, one can clearly see its general elongation, a progressive feature that is characteristic of the holotype and distinguishes S. lacustrina from Mioquerquedula soporata (examplified by specimen PIN, no. 4869/107 from Sharga) and specimen PIN, no. 2614/342, assigned to T. palaeobaikalensis. The ventral margin of the tubercle in specimen PIN, no. 2614/198 is largely oriented along the long axis of the bone, while it is oriented approximately at an angle of 45° in specimen PIN, no. 4869/107 and specimen PIN, no. 2614/342. Modern Nettapus also have a slightly more shortened tuberculum. The dorsal surface of the crista deltopectoralis is nonconcave (also a progressive feature); there is a moderately pronounced caudal ridge on the caudal surface of the shaft. The degree of development of this ridge is comparable to that in specimen PIN, no. 4869/107 from Sharga, which is assigned to Mioquerquedula, but somewhat lower than that in Tagayanetta. The base of the crus dorsale fossae is preserved, which shows that the area between the crus and caudal ridge was very narrow, as in the holotype and in contrast to the wide area (“dorsal tricipital fossa”) in Malacorhynchus, Oxyurinae, and Mergini. The width of this area corresponds to the configuration in Nettapus and Anatini, although the latter have an indistinct caudal crest. The cross section of the shaft at the level of the distal part of the crista deltopectoralis is subtriangular. The inner (dorsal) wall of the fossa pneumotricipitalis is solid and non-pneumatized; a medium-sized pneumatic foramen is visible in its deep part. This region is morphologically most similar to that of modern Aythya, which have no defined pneumatization of the fossa pneumotricipitalis and, at the same time, may also have foramens in the solid dorsal wall of the fossa. While the absolute thickness of the shaft is similar to that of N. auritus, the crista deltopectoralis is longer; its distal part is oriented more cranially than dorsally (unlike Nettapus but similarly to Anatini).
Two incomplete coracoids (specimen PIN, nos. 2614/181, 193) were also assigned to this taxon; they
are similar to the coracoids of M. minutissima in general dimensions and, at the same time, differ from
them in smaller facies articularis humeralis (at a similar length of the glenoid articular part and with the
same size of the cotyla scapularis) and the presence of a ventrally defined fossa inside the sulcus m. supracoracoidei (in Mioquerquedula, the surface of the sulcus is flat or slightly concave, but without a defined fossa). A characteristic feature of these coracoids that distinguishes them from M. minutissima is the narrowing of the middle part of the shaft, which is formed by the concavity of its lateral and medial margins. In Mioquerquedula, the margins of the shaft have a more parallel orientation in the middle part. These coracoids are also characterized by a convex medial margin of the shaft at the level of the facies articularis humeralis (between the processus procoracoideus and proc. acrocoracoideus), which is absent in Mioquerquedula. These coracoids are very similar to those of the smallest duck, Anatidae gen. indet., from Sansan (Zelenkov, 2023).
The left scapula (specimen PIN, no. 2614/180) corresponds in size to N. auritus and is also assigned here to this taxon. This specimen is smaller than the other scapula fragments from Tagay; it is characterized
by an elongated acromion, which, in contrast to specimen PIN, no. 2614/463 (assigned to T. palaeobai-
kalensis
), is oriented noticeably more cranially than dorsally. Facies articularis humeralis is elongated; the
general curvature of the bone is weakly pronounced. Morphologically, specimen PIN, no. 2614/180 is close to modern Anatini.
Two fragmentary carpometacarpi from Tagay (specimens PIN, nos. 2614/385, proximal fragment of the right carpometacarpus, and 2614/396, proximal fragment of the left carpometacarpus) are assigned to
this taxon; they differ from M. palaeotagaica in a small size and a lower processus exensorius, as well as in an unpronounced depressio muscularis externa, a rather large and concave fossa infratrochlearis (in Anatini, this fossa is usually very small and forms a punctate depression), a proximally protruding dorsal semitrochlea of the trochlea carpalis, and a distinct fovea carpalis cranialis. On the whole, these carpometacarpi are closer to modern Mergini. They differ from the smallest carpometacarpus from Sansan in a somewhat smaller size, the presence of a distinct saddle-shaped notch in the distocranial contour of the os metacarpale alulare, a lower processus extensorius, and a shortened proximal part of the proximal end (proximal to the processus pisiformis).
Other materials are represented by the distal end of the right tibiotarsus (specimen PIN, no. 2614/392)
and the fragmentary shaft of the left tarsometatarsus of a subadult individual (specimen PIN, no. 2614/365), corresponding in size to modern N. auritus. In the tibiotarsus, the condylus medialis is oriented subparallel to the condylus lateralis (as in Nettapus) and is medially not inclined (unlike Anatini). Tibiotarsus is craniocaudally low in distal view; it is somewhat lower than that in Anatini and noticeably lower than in Nettapus; incisura intercondylaris is narrow at its base, as in Nettapus. Tarsometatarsus has a uniform thickness of the shaft; i.e. it is not narrowed in the central part.

Fred


Coracoids (1–8), tibiotarsus (9), maxillary rostrum (fig. 10), carpometacarpus (11–14), scapulae (15–17), humeri (18–20)), and tarsometatarsi (21–23) of Early–Middle Miocene and modern Anatidae in dorsal (1, 2, 3a–8a, 10b, 21a, 22a, 23b), ventral (3b‒8b, 10c, 11–14, 21b, 22b), distal (fig. 9a), cranial (9b, 20b), lateral (10a, 15–17, 21c–23c), caudal (18, 19, 20a), and medial (3c, 4c, 21d) views.
Figs. 1 and 19. Mioquerquedula soporata (Kurochkin, 1976): (1) specimen MNHN, no. SA 10283; France, Sansan locality; Middle Miocene; (19) specimen PIN, no. 4869/107; Mongolia, Sharga locality; Middle Miocene.
Figs. 2, 3, 10, 14, 16, 18, and 21. Tagayanetta palaeobaikalensis gen. et sp. nov.: (2) specimen PIN, no. 2614/338; (3) holotype PIN, no. 2614/337 (reflected); (10) specimen PIN, no. 2614/393; (14) specimen PIN, no. 2614/389; (16) specimen PIN, no. 2614/463; (18) specimen PIN, no. 2614/342; (21) specimen. PIN, no. 2614/340; Baikal Region, Tagay locality; uppermost Lower Miocene.
Figs. 4, 9, 13, 15, and 22. Mioquerquedula palaeotagaica sp. nov.: (4) holotype PIN, no. 2614/177; (9) specimen PIN, no. 2614/386; (13) specimen PIN, no. 2614/458; (15) specimen PIN, no. 2614/454 (reflected); (22) specimen PIN, no. 2614/339; Baikal Region, Tagay locality; uppermost Lower Miocene.
Fig. 5. Mioquerquedula integra (Miller, 1944) comb. nov., specimen UCMP, no. 37370; United States, South Dakota, Flint Hill locality; Lower Miocene.
Figs. 6, 12, 17, 20, and 23. Selenonetta lacustrina gen. et sp. nov.: (6) specimen PIN, no. 2614/181; (12) specimen PIN, no. 2614/385; (17) specimen PIN, no. 2614/180; (20) holotype NMNHU-P No Av-52; (23) specimen PIN, no. 2614/365 (reflected); Baikal Region, Tagay locality; uppermost Lower Miocene.
Fig. 7. Mioquerquedula minutissima Zelenkov et Kurochkin, 2012, holotype PIN, no. 4869/193; Mongolia, Sharga locality; Middle Miocene.
Fig. 8. Anatidae gen. indet. (?Selenonetta lacustrina gen. et sp. nov.), specimen MNHN, no. SA 14006; France, Sansan locality; Middle Miocene.
Fig. 11. Nettapus coromandelianus Gmelin, 1789, specimen from the osteological collection of PIN RAS, no. 40-7-1, modern. Designations: ca, crista acrocoracoidea; cdp, crista deltopectoralis; ch, caput humeri; cl, cotyla lateralis; clh, crista lateralis hypotarsi; cm, cotyla medialis; cs, cotyla scapularis; csr, caudal shaft ridge of the humerus; dtf, dorsal tricipital fossa; eic, eminentia intercotylaris; fac, facies articularis clavicularis; fah, facies articularis humeralis; fas, facies articularis sternalis; fic, fossa infracotylaris; fpl, fossa parahypotarsalis lateralis; fpt, fossa pneumotricipitalis; iic1, developed notch of the incisura capitis in the ventroproximal profile of the humerus; iic2, undeveloped notch of the incisura capitis in the ventroproximal profile of the humerus; mm, medial margin of the coracoid shaft; pa, processus acrocoracoideus; pp, processus procoracoideus; sms, sulcus m. supracoracoidei; td, tuberculum dorsale.
Scale bar, 10 mm; (21d and 22d) out of scale.

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