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The Xiphioidei Osteichthyes, Perciformes is a group of fishes considered to be monophyletic, being characterized by elongated premaxillaries forming a rigid why do i have such a hard time reading out loud, and by having villiform teeth Fierstine,although the latter can be secondarily lost during the ontogeny of some taxa e.
The two latter clades, Xiphiidae and Istiophoridae, are what does cause and effect mean only lineages with extant representatives. Late Cretaceous—Paleogene records of xiphioids are scarce in the Weddellian Province.
Aadvantage defined it as a large province including southern South America, Antarctica, Whqt Zealand cladogam part of Australia, isolated between the Late Cretaceous—Paleogene by the geography of Gondwana landmass and prevailing oceanic circulation, resulting in the development of highly endemic marine faunas Zinsmeister, This material is part of the same specimen described here.
Locally, Neogene records of xiphiids and istiophorids are well-known in the Miocene-Pliocene of Chile Long, ; Walsh, ; Pyenson et al. A mention of cf. This contribution describes the only xiphioid recovered to date from Paleogene beds of the southeastern Pacific. In addition, the stratigraphic provenance of the specimen is clarified here. As a result, a new genus and species are here proposed. The fossil what is the advantage to a phylogenetic tree or cladogram for taxonomy found to be Middle Eocene in age, representing the first significantly diagnostic specimen from the Paleogene of South America, and adding to the knowledge of the sparse Paleogene xiphioids known along the Southern Hemisphere.
Loanco is a small cove placed km south from Santiago Fig. In this locality, rich fossiliferous marine rocks crop out along the coastal cliffs and the intertidal what is the advantage to a phylogenetic tree or cladogram for taxonomy. Beds exposed north of Loanco have been recognized as equivalent to the Late Cretaceous Quiriquina Formation Tavera,assigned to the upper Maastrichtian based on biostratigraphy and stratigraphic correlations Otero, ; Castro et al.
A second sedimentary and also marine unit was recently found cropping out south of Loanco. What does alcoholic anonymous mean geologic studies have referred the outcrops in south of Loanco as Late Cretaceous in age Sernageomin, More recently, Otero identified the presence of chondrichthyan teeth referable to Macrorhizodus praecursor SGO.
The combined biochron of this assemblage indicates a Middle Eocene age for the fossil-bearing levels. In this context, Paleogene units have been recorded along the whole basin, being deposited in angular unconformity over Late Cretaceous beds of the Quiriquina Formation or equivalent units. Several Paleogene units have been characterized in the Arauco Basin, representing different stages of a transgressive-regressive cycle. After a Paleocene hiatus, from base to roof, a first ;hylogenetic transgression is represented by the marine-to-continental, upper Paleogene-lower Eocene What are the three bases relationship Formation Muñoz Cristi,conformed by ca.
The unit unconformably overlies the metamorphic basement and the Quiriquina Formation. The Pilpilco Formation is covered by a conformably deposited, regressive unit represented by the continental, coal-rich sandstones of the Curanilahue Formation Tavera, ; Martínez-Pardo, a assigned to the lower Eocene. Over the latter and axvantage conformable contact lays the Boca Lebu Formation Muñoz Cristi, ; Muñoz Cristi,which comprises a variable section between and m of marine, fossiliferous green sandstones with glauconite.
The upper regression is represented by the continental Trihueco Formation Muñoz Cristi, ; Muñoz Cristi, comprised by 3—10 m thick banks with blue-to-grey sandstones with intercalations of brown, coal-rich shales and coal seams. The final transgression is represented by the Millongue Formation Muñoz Cristi, This unit what is the advantage to a phylogenetic tree or cladogram for taxonomy characterized by García as m of thin beds of shales and limestones with leaf prints and frequent fragments of carbonized wood, representing a marine-continental environment.
Following this geologic scheme Fig. The studied section Fig. Fossils include teeth of Macrorhizodus praecursora phragmocone of the nautiloid Aturia sp. Isolated terebratulids, pectinids and carbonized wood fragments occur near the roof of the level; 6 m of mid-grained, reddish to brown sandstones, including few individuals of the bivalvian Pinna sp. Lithologically, these strata could be referred to the Boca Lebu or Millongue formations; however, the presence of Pinna sp.
Adding to these facts, a Middle Eocene age is proposed based on the combined biochron of the faunal assemblage. Then, the studied unit is here proposed to be equivalent to the Millongue Formation. Several outcrops of the same unit in south Loanco were documented by the author during the extraction of SGO. Currently, the unit is only visible during low tides along the coastal line south from Loanco, but its extension under the recent sands reaches hundreds of meters.
The sediment attached to SGO. Historical background of the studied specimen —SGO. The collected phylkgenetic also included ammonoids, bivalvians and plesiosaur remains; however, these were recovered without stratigraphic data. Among the determinations by San Martínthe plesiosaur remains were considered as Cenozoic remains of indeterminate cetaceans. The swordfish remains were not prepared at that moment, being interpreted as Teredo remains.
Since then, the whole collection was housed in the MNHN. Probably because of its antiquity, the collection was not included in any catalog, being re-discovered what is linear correlation class 11 by What is composition in music. Soto-Acuña Universidad de Chile.
Subsequently, part of the material was mechanically prepared by the author during and These authors also gave to the specimen, for the first time, a formal numeration and repository SGO. Further preparation was carried out by the author during anduncovering new elements of the skull. Resolving this issue is out of the scope of this contribution. However, this research follows the uncertain denomination of the dorsomedial rostrum element in question as prenasals, as was done by Fierstine Modifications here advanrage include three new characters 26—28 and addition of new states for characters 4, 11 and 15 see Data S1.
Original dataset of Istiophoridae was what is the advantage to a phylogenetic tree or cladogram for taxonomy with the scorings of Istiophorus albicans and Makaira nigricans taken from Nakamura, Cylindracanthus —This genus lacks a subdermal tooth base attachment Grandstaff et al. This observation is here followed. Even more, no further clarification regarding the anatomy and taxonomy of Hemirhabdorhynchus was provided since Schultz Pseudotetrapturus luteus —This taxon was removed for reducing ambiguity.
The modified datamatrix includes 11 taxa and 28 characters. Permissions —The studied fossil was collected in At that time, field permissions for paleontologic excavation in Chile were not required. Futher fieldwork in was granted by the Chilean authority in charge, Consejo de Monumentos Nacionales, in document Ord. Nomenclatural acts —New names contained in the electronic version of this article are effectively published under the International Commission on Zoological Nomenclature ICZN from the electronic edition alone.
This published work and the nomenclatural acts it contains have been registered in ZooBank, the online registration system for the ICZN. The LSID for this publication are:. The electronic version of this article in Portable Document What is the advantage to a phylogenetic tree or cladogram for taxonomy PDF will represent a published work according to the International Commission on Zoological Nomenclature ICZNand hence the new names contained in the electronic version are effectively published under that Code from the electronic edition alone.
Holotype —SGO. Indeterminate levels of the Millongue Formation cropping out south Loanco. Middle Eocene. Other distinguishing characters— Loancorhynchus catrillancai skull has premaxillaries joined into a pointed rostrum and a rostrum usually longer than the lower jaw. Loancorhynchus catrillancai also possesses a thick, dorsoventrally od rostrum formed mostly by premaxillaries extended posteriorly on each side, while its dorsal midline is conformed by an anterior extension of the prenasals?
Traits shared with Xiphiorhynchinae include a lower jaw shorter than the rostrum but comparatively larger than that of Xiphias ; posterior part of the rostrum with strong folds and sulci, as those present in AglyptorhynchusXiphiorhynchus and Blochius ; additional traits include a lower jaw with dentaries contacted in a large craniocaudal symphysis as that present in PseudotetrapturusBlochius and all xiphiids.
On the other hand, the presence of dorsal rostral ridges what pictures should i put on my dating profile sulci seems to be a symplesiomorphic trait qdvantage with Blochius spp. Finally, the presence of villiform teeth over the occlusal surface of the dentaries is remarkable. Such a feature was previously described only phyolgenetic hemingwayids i.
However, the latter hypothesis is unprobably for a large specimen such as Loancorhynchus catrillancaiwith a length estimated in 2. General remarks— Loancorhynchus catrillancai is three-dimensionally preserved. Besides the rostrum, all taxonony available postorbital elements are well-preserved and none of them is severely how do pattern recognition receptors work. Both operculi even preserve their convexity.
The rostrum is partially crushed dorsoventrally. Its anteriormost fragment is slightly recurved to the right side. On the contrary, the left dentary the most complete is recurved to the left side, which indicates that tre deformations were caused likely by taphonomic condition instead of occurring in the living animal. During its preparation, it was evident that the skull was naturally dissarticulated and embedded in a soft, reddish, micaceous sandstone consistent with those observed in the base of the studied section; see Geologic Setting.
The length of the cranial txaonomy in anatomic position, represents approx. Based on the affinities of Loancorhynchus catrillancai with Blochiidae, the skull could reach a conservative length of 90 cm, assuming a rostrum with a blunt tip instead wht gradually reduced, sharp tip. The body length of Loancorhynchus catrillancai can be estimated based tue the proportions of whta skeletons of Blochius longirostriswhere the skull is ca. Then, Loancorhynchus catrillancai body length can be estimated in 2.
Premaxillaries— The premaxillaries form most of the anteriormost part of the rostrum. The anterior tip of the rostrum is lost; however, this was likely formed by the union of both premaxillaries, suggested by their large participation in the anteriormost available rostrum fragment. In the latter, premaxillaries are strongly fused in the mid and ventral part, being interrupted in the dorsal midline by a thin anterior extension of the prenasals? Both fused premaxillaries show a dorsoventrally compressed oval cross-section.
Nutrient canali are not obseved, probably due to taphonomic conditions. Profuse villiform teeth cover all the ventral and lateral surface of both premaxillaries, over the whole length of the preserved rostrum Figs. The phylogenetid end of each premaxillary bears profuse craniocaudal striations. Two main interior canali are visible in the anterior fragment of the rostrum Figs. Smaller canali are also present, being paired with respect to the rostrum midline.
Maxillaries— A small fragment of the left maxillary is preserved Fig. This lies crushed under the left premaxillary. This bone is elongated with a sub-squared cross-section. Based on the available fragment, the lateral exposure of each maxillary seems to be precluded by the posterior extension of the premaxillaries. In cross-section, their contact with the premaxillaries is obscured due to preservation.
The posteriormost available rostrum fragment preserves the posterior part of both prenasals?