Pleistocene Mammals Research Articles

Diet and habitat of the late Middle Pleistocene mammals from the Casal de’ Pazzi site (Rome, Italy) using stable carbon and oxygen isotope ratios

The late Middle Pleistocene archaeological site of Casal de’ Pazzi (MIS 7, ∼240–200 ka) in central Italy provided a complex of paleontological (both fauna and flora) and archaeological evidence, as well as a cranial fragment of Homo heidelbergensis.Here, we investigated the stable carbon and oxygen isotopic ratios of tooth enamel from six herbivore species (Palaeoloxodon antiquus, Hippopotamus amphibius, Bos primigenius, Stephanorhinus kirchbergensis, Equus ferus, and Dama Dama) to contribute to the understanding of the paleoenvironment of the site through the reconstruction of the diet and habitat of Pleistocene mammals. Our results indicate that the analyzed taxa fed on C3 plants and exploited both closed and open environments. This is consistent with the macro-botanical remains (leaf fossil impressions of Zelkova sp., Laurus nobilis, and Cercis siliquastrum) found at Casal de’ Pazzi and pollen evidence from the nearby lake of Valle di Castiglione. The area around the site was characterized by diversified Mediterranean evergreen forest tree species, accompanied by mesophilic elements of the mixed deciduous oak and beach forest, alternating with diversified wooded/forested vegetation and xeric vegetation. This was the environmental context in which the late Middle Pleistocene Homo lived. Comparisons with published isotopic data from other European archaeological localities between ∼600 and 125 ka evidenced considerable environmental differences through time and space, according to the general climate trends and local factors, such as latitude, temperature, and vegetation composition.

A regional assessment of the deglaciation history of the Swiss Plateau based on newly obtained and re-evaluated Be-10 cosmic-ray exposure ages

During marine oxygen isotope stage (MIS) 2, the Swiss Plateau temporarily hosted large piedmont lobe glaciers that retreated after their maximum advance back to the fringe of the Alps. The presence of moraines in this region indicates that overall glacier recession was punctuated by repeated phases of ice-marginal stability and re-advances. The timing of these events in the region formerly covered by the eastern lobe of the Rhône (or Valais) glacier has been controversial and remains poorly constrained due to the lack of chronological data. To fill this gap, 10Be cosmic-ray exposure (CRE) dating was applied to erratic boulders inside the assumed MIS 2 maximum extent of this piedmont lobe. An erratic boulder at an ice-marginal position upstream from the suspected MIS 2 maximum extent gave an age of about 19 ka. Erratic boulders at a presumably younger ice-marginal position (Brästenberg position) yielded an average age of ca. 20 ka. However, several erratic boulders beyond the Brästenberg position gave internally consistent, but stratigraphically too young ages of ca. 17 ka. We cannot rule out that glacier recession from the Brästenberg position began no later than 17 ka. CRE dating of a moraine of a presumably younger ice-marginal position (Solothurn position) gave unrealistically old ages and an incredibly young age (86 ka, 40 ka, and 4 ka). Carbon-14 CRE dating should be applied to provide additional information on the last deglaciation of the Swiss Plateau. Nevertheless, despite outlying ages, the presented chronological data contribute to an overall consistent and increasingly refined chronology of the last deglaciation of the Swiss Plateau when compared with 59 previously published CRE ages.

Xenarthrans of the collection of Santiago Roth from the Pampean Region of Argentina (Pleistocene), in Zurich, Switzerland

The present work concerns xenarthrans from the collection of Santiago (Kaspar Jakob) Roth (1850–1924) housed at the Palaeontological Institute and Museum of the University of Zurich, one of the most important collections of Pleistocene mammals from Argentina in Europe. Roth was a paleontologist originally from Switzerland who prospected and collected a large amount of Pleistocene megafauna of the Pampean Region of Argentina. The xenarthrans are the main representatives of this collection in Zurich, with 150 specimens. Since 1920, this material has not been revised and is under studied. The present investigation corresponds to a taxonomic revision resulting in 114 reassignments, leading to document xenarthran diversity and discuss their paleoecologies. The high diversity reflects the paleoecology of the Pampean Region during the Pleistocene, with the various abiotic events that impacted the paleoenvironment of this region. Within the Cingulata, the Pampean Region fauna was probably dominated by glyptodonts with a high representation of Glyptodontinae and Neosclerocalyptinae while within the sloths the highest diversity and abundance is found in the Mylodontinae and Scelidotheriinae. These four clades represent both species with high ecological tolerance (e.g., Glyptodon munizi; Catonyx tarijensis) and ecologically highly specialized species (e.g., Neosclerocalyptus paskoensis; Scelidotherium leptocephalum). The presence of such ecological diversity underlines the status of the Pampean Region as a major interest for paleoecological and paleoenvironmental reconstruction.

Bone modifications by the giant hyaena Pachycrocuta brevirostris on large-sized ungulate carcasses from the Lower Pleistocene site of Tsiotra Vryssi (Mygdonia Basin, Greece)

ABSTRACT The Early Pleistocene mammal communities of Europe are characterised by a great diversity of large carnivorans. Among them, the largest ever hyaenid, Pachycrocuta brevirostris, a fierce predator with great bone-cracking adaptations that has left its taphonomic signature on several fossiliferous sites. Here, we perform a rigorous taphonomic analysis focusing on bone surface modifications and damage patterns on large-sized ungulate bones from the site Tsiotra Vryssi (1.78 to ~1.5 Ma; Mygdonia Basin, Greece), aiming to identify the main biotic agent responsible for the modifications. Results reveal significant carnivore ravaging of the assemblage, and selective consumption of bones/bone portions related to nutrient value. Comparisons with modifications on similar-sized ungulate carcasses produced by extant and extinct predators, and similarities with Pachycrocuta-modified assemblages, indicate that Pachycrocuta was the principal agent of modification. Overall, this study not only provides taphonomic evidence for the interpretation of Tsiotra Vryssi, but also offers insights into the palaeobiology, and particularly carcass consumption behaviour of the giant hyaena. Hence, it advances our knowledge on carnivoran guild dynamics and prey–predator relationships during this epoch and has important implications for the investigations of the subsistence behaviour of the meat-eating hominins, who entered Eurasia at ~1.8 Ma, roughly synchronously with Pachycrocuta.

A coherent biogeographical framework for Old World Neogene and Pleistocene mammals

AbstractIn order to understand mammalian evolution and compute a wide range of biodiversity indices, we commonly use the ‘bioregion’, a spatial division adapted to ecological and evolutionary constraints. While commonly conducted by neontologists, the establishment of bioregions in palaeontology is generally a secondary analysis, shaped on subjective time scales and areas specific to the investigated questions and groups. This heterogeneity, coupled with the scale‐dependency of biodiversity indices, prevents the clear identification of macroecological and macroevolutionary trends for large taxonomic groups like extinct mammals. Here we tackle this issue by providing a coherent framework for Neogene and Pleistocene mammals of the Old World following two steps: (1) a temporal scale adapted to mammalian evolutionary history (i.e. evolutionary fauna) is defined by poly‐cohort analysis; (2) bioregions are then computed for each evolutionary fauna by clustering, ordination and intermediate approaches at multiples spatial scales (i.e. continental to regional) for Eurasia and Africa. Additionally, providing a coherent framework for a wide range of mammalian datasets, our results show: (1) the synchronous emergence and fall of five mammalian evolutionary faunas identified at chronological scales varying from the epoch to the geological stage; (2) a transition from a longitudinal to a latitudinal biogeographical structuring between the Miocene and Pliocene, especially in Europe; (3) the long‐term affinity of southern Asian with African faunas, in sharp contrast with the modern Palaearctic bioregion extension; and (4) the establishment of a vast Mediterranean bioregion from fragmented areas in the Late Miocene to its full extent in the Pleistocene.

Preserving the Nieuwdonk collection, a hidden Pleistocene mammal assemblage from the Flemish Valley (Berlare - Belgium)

In the midst of the coronavirus pandemic, the municipality of Berlare (East Flanders, Belgium) acquired an important collection of Late-Pleistocene remains from the former Nieuwdonk quarry (near Uitbergen and Overmere, province of East Flanders). This previously private collection comprises a diverse assemblage of Pleistocene mammals from the Flemish valley and covers an important part of Belgium's Quaternary fossil record, offering a window into the regional biodiversity of the last Ice Age and Interglacials (ca. 10 Ka - 126 Ka). Within the collection, various remains (318 specimens) of roughly 20 different taxa are represented, as well as reworked Tertiary ichnofossils and Stone Age artefacts, including a bone tool. Although sampling bias occurred during collecting in the 1970s, it still counts as one of the most complete Pleistocene collections from this classic location within the Scheldt basin and Unesco Global Geopark (Schelde Delta). As a result of years of poor storage conditions, almost all of the specimens suffered from desiccation and pyrite decay. A restoration project was set up during the coronavirus pandemic with restrictions imposed by the Belgian government on daily activities. In this article, we focus on the lessons we learned from both the restoration and inventorisation project during the pandemic, as well as the challenges faced in transitioning a former private collection into a public one.

MIS 3–1 fauna from Krosinko: Implications for the past biogeography, chronology and palaeoenvironments of Poland

A faunal assemblage was recently recovered from the Krosinko site in Poland, marking a new site in the Warsaw–Berlin ice-marginal valley. Analysis and radiocarbon dating of the remains revealed the presence of two subassemblages: one Late Pleistocene (at least MIS 3–2) and one Holocene (MIS 1), with the former being taxonomically highly diverse. By referring to previous Polish studies, the Pleistocene mammal bone assemblage allowed us to reconstruct the biogeography of its individual components: woolly mammoths, woolly rhinoceri, horses, giant deer, red deer, fallow deer, reindeer, steppe bison, aurochses, bears, and cave lions. The biogeography was later combined with radiocarbon chronology using 21 dates from Krosinko. The wide range of radiocarbon dates (48.4–26.4 ka BP) probably reflects different chronological distributions of species resulting from the changing climate and environment as well as the diverse original sources of the bones. The remains, which constituted a single, compact geological horizon, was possibly deposited in a single geological event around 26 ka BP, as inferred from the most recently produced radiocarbon date. Radiocarbon datings of woolly rhinoceros remains have shown the species to have been present around 38 ka BP, a time that it had previously been considered to have been non-existent in Europe (with no evidence having been discovered for the period 40–34 ka BP). This result alters the stratigraphic gap range for the woolly rhinoceros in Europe to 40–38 ka BP. The clear dominance of woolly mammoth and woolly rhinoceros specimens reflects the structure of the Mammuthus–Coelodonta faunal complex. The main representatives of this complex preferred the dry and cold conditions that characterized the palaeoenvironmental conditions in Krosinko in MIS 2 and thus in Central Europe, as shown by the integration of the results of the fauna and those of the sediments in which they were deposited. These palaeoenvironmental features are related to the mammoth steppe, which was a long-lived biome in Eurasia and whose diversity influenced the faunal distribution. Thus, the species-by-species review of taxa performed in this paper, against the background of previous results from Poland, illuminates the individual responses of taxa to changing environmental conditions in response to climatic ones. These changes led to the disappearance of the mammoth steppe and near or total extinction of the fauna species inhabiting it.

QUATERNARY DEPOSITS AND ECOLOGICAL MONITORING OF THE ICE AGE PARK IN CARPATHIAN REGION, UKRAINE

An international geopark "The Park of Ice Age" located near the Starunia village in Bohorodchany district of Ivano-Frankivsk region is world-famous for being a paleontological site of Pleistocene fauna of the woolly rhinoceroses and mammoth (the Eemian interglacial period- 46-10 000 years ago according to radiocarbon dating C14) and for its mud volcano which is unique in the Carpathian region, This is a geological nature monument with an area of 60 hectares where abandoned ozokerite mine and oil and gas exploratory boreholes are presented. The detailed investigations carried out in the years 2004 - 2009 by Ukrainian-Polish expeditions were focused on discoveries of possible new sites of fauna fossils and human remains of European early modern humans (EEMH). The future discoveries at the paleontological site of Starunia are extremely important. They intend to carry out ecological assessment of soil, surface and stream waters, atmospheric air, snow, ashes of meadow grasses, radiological screening, and geo-radar sensing to find new locations of extinct mammals. The Starunia area meets all the requirements of a geopark according to UNESCO standards and concepts. The first research findings (1907) are connected with the remains of woolly rhinoceros, mammoth, horse, roe deer and other Pleistocene mammals which had been found in the ozokerite mine at the depth of 12 m near Starunia (Bohorodchany district, Ivano-Frankivsk region). In 1914 the scientists from Lviv (Ukraine) and Krakow (Poland) fully appreciated these discoveries and published a set of articles and a monograph. In 1929 the members of the expedition of Skill Academy (Krakow, Poland) found the remains of three more woolly rhinoceroses in the ozokerite mine at the depth of 17 m. Numerous bones of vertebrates (rodents), remains of mussels, a lot of species of insects, beetles, parasitic worms, fleas, butterflies, spiders, snails, vascular plants, mosses, seeds and branches of dwarf birch (Betula Nana), alder (Alnus glutinosa), and other fossil of tundra flora were also discovered. Polish scientists organized detailed investigations of flora and fauna around Starunia, their results were published in articles but the World War II suspended this process. The investigations around Starunia intensified the comprehensive study of stratigraphy, paleontology, paleogeography, geochronology and other aspects of the Quaternary Period. In 1932 there was established the International Geological Congress (the International Union of Quaternary Study) by INQUA in Leningrad. The main methodological principals of this study dealt with the investigations around Starunia.

The fossil vertebrates of Guatemala

The fossil vertebrates of Guatemala are almost exclusively fossils of mammals and are of late Miocene (Hemphillian) and late Pleistocene (Rancholabrean) age. The only lower vertebrates are the crocodile fossil Crocodilus moreletti collected in the Río La Pasión area, a turtle from El Trifinio and fishes from Río Carboneras. The late Miocene mammals are the proboscidean Gomphotherium, an aceratheriine rhinoceros and the horse Neohipparion from the Río Carboneras in Izabal; the holotype of “Serridentinus guatemalensis” (nomen dubium) from Chinautla in the Department of Guatemala is also a specimen of Gomphotherium of likely late Miocene age. Late Pleistocene vertebrates are known from at least 36 localities in Guatemala, but only six of these yield at least four documented genera of mammals—Chivacabé, Ciudad Real. El Rosario, Estanzuela, Río La Pasión and San Rafaelito. The combined list of Guatemalan late Pleistocene mammal genera is Canis, Cuvieronius, Dicotyles, Equus, Eremotherium, Euceratherium, Glyptotherium, Holmesina, Mammuthus, Mazama, Megalonyx, Mixotoxodon, Neochoerus, Odocoileus, Pachyarmatherium, Palaeolama, Paramylodon, and Tapirus. The late Pleistocene mammals from Guatemala resemble broadly correlative mammal assemblages from throughout Central America in being dominated by the fragmentary remains of large herbivorous mammals and in having a mixture of immigrants from both North and South America. They thus well reflect a substantial taphonomic megabias in the Central American Pleistocene mammal record towards large mammals with large and durable skeletal parts that are easily preserved and readily discovered. This megabias renders problematic direct biological inferences from the Guatemalan Pleistocene mammal record. Mammoth records from Guatemala are relatively numerous for a Central American country but so few that inferring extensive grasslands or positing migration routs of mammoths from these records are questionable. There is no demonstrable association of humans with extinct Pleistocene megamammals in Guatemala despite claims to the contrary. The suggestion that during the late Pleistocene Guatemala was north of a biogeographic juncture between North and South America lacks any support. The Guatemalan fossil vertebrate record needs extensive augmentation, with an appropriate stratigraphic context, especially of lower vertebrates and micromammals, to provide further insight into vertebrate history in Central America during the last 10 million years.

Diversity of Pleistocene megamammals from southern Amazon, Mato Grosso state, Brazil

The Amazon region is a key area to understand the South America history, displaying a significant importance in the study of Pleistocene mammal fossils. Here, we present the taxonomic account of the first megafaunal records of the Quaternary deposits from bed and alluvial terraces from the Teles Pires River and its tributaries, in northern Mato Grosso state, southern Brazilian Amazon. Teeth, partial dentaries and postcranial fossil specimens have been described and identified as immature to senile individuals of Notiomastodon platensis, cf. Eremotherium and Toxodon platensis. These species were well-dispersed along the Pleistocene in South America, including the Amazon region. This paper brings up the paleontological potential of the upper Teles Pires basin, midwest Brazil, for South American Pleistocene megafauna. Further studies are necessary in order to obtain more information regarding the location and genesis of the fossiliferous assemblages, and the paleoecological and taphonomic aspects of the megamammal paleocommunities in the southern Amazon.

Isolated petrosal of the extinct sloth Glossotherium tropicorum (Xenarthra, Folivora, Mylodontidae) from the island of Trinidad

This report is the first to identify the presence of the extinct ground sloth Glossotherium tropicorum from Pleistocene-aged tar pit deposits in Trinidad. G. tropicorum is known primarily from extensive skeletal material recovered from the Pleistocene of western Ecuador and Peru. Our identification is based on an isolated left petrosal bone, which exhibits a variety of derived diagnostic features of mylodontid sloths in general, e.g., the presence of an epitympanic recess, and the genus Glossotherium in particular, including a reduced anteroventral process of the tegmen tympani. This represents only the second published record of the genus Glossotherium from outside continental South America, and is a substantial range extension for the species G. tropicorum. The present study also represents the first published description of a mylodontid sloth fossil from Trinidad. The specimen is part of a collection that was initially documented in an unpublished Master’s thesis, and that includes additional sloths and other Pleistocene mammals. This fauna confirms the presence of extensive savanna-type habitats on Trinidad during the Pleistocene, and is consistent with the presence of a land bridge connection between the island and mainland South America at that time.

Infectious spondylitis with pathology mimicking that of tuberculosis in a cervical vertebra of a plesiosaur from the Upper Cretaceous of Patagonia, Argentina

Paleopathological studies have been used to understand the history of injury and disease in extinct populations, their putative causes and, on this basis, to infer paleoecology and behavioral aspects. The most common pathologies reported in the zoological/paleontological record are traumatic injuries, post-traumatic malformations, inflammatory arthritis, infection and congenital defects. Although pathologies in plesiosaurs are recognized since the 1870s, reports of infectious disease are comparatively scarce. Here we report the pathological cervical vertebra of a plesiosaur recovered from the Upper Cretaceous of Argentina. The anterior external surface shows an elliptical, subchondral erosion with new bone formation and slight adjacent filigree reaction. The right anteroventral surface of the centrum bears erosive processes with bone reaction and alterations that have the appearance produced by space-occupied masses. On the left anteroventral surface of the centrum, there are abnormal vascular channels, associated with a groove just ventral to the articular surface. The combination of these features indicates that the pathological aspect of the vertebra is due to an infection. The pattern of bone abnormalities is compatible with those described in Pleistocene mammals affected by the granulomatous tuberculosis infection and with the abnormal ribs and cervical vertebrae of an eosauropterygian from the Triassic. The case reported herein represents the first record of tuberculosis-like infection in a plesiosaur. As the vertebra was not part of an associated skeleton, we cannot infer if the cause of death could have been related to the compromised hunting ability (due to limited neck mobility) or the result of infection-related organ failure.

The early hunting dog from Dmanisi with comments on the social behaviour in Canidae and hominins

The renowned site of Dmanisi in Georgia, southern Caucasus (ca. 1.8 Ma) yielded the earliest direct evidence of hominin presence out of Africa. In this paper, we report on the first record of a large-sized canid from this site, namely dentognathic remains, referable to a young adult individual that displays hypercarnivorous features (e.g., the reduction of the m1 metaconid and entoconid) that allow us to include these specimens in the hypodigm of the late Early Pleistocene species Canis (Xenocyon) lycaonoides. Much fossil evidence suggests that this species was a cooperative pack-hunter that, unlike other large-sized canids, was capable of social care toward kin and non-kin members of its group. This rather derived hypercarnivorous canid, which has an East Asian origin, shows one of its earliest records at Dmanisi in the Caucasus, at the gates of Europe. Interestingly, its dispersal from Asia to Europe and Africa followed a parallel route to that of hominins, but in the opposite direction. Hominins and hunting dogs, both recorded in Dmanisi at the beginning of their dispersal across the Old World, are the only two Early Pleistocene mammal species with proved altruistic behaviour towards their group members, an issue discussed over more than one century in evolutionary biology.

Prospects for new sites of wooly rhinoceros and mammoths on the territory of paleontological site in Starunia, Carpathian region

An international geopark “Park of the Ice Age” located near the Starunia village in Bohorodchany district of Ivano-Frankivsk region is world-famous for being a paleontological site of Pleistocene fauna of the woolly rhinoceroses and mammoth (the Eemian interglacial period, 46–10 000 years ago according to radiocarbon dating C14) and for its mud volcano which is unique in the Carpathian region. This is a geological nature monument with an area of 60 hectares where abandoned ozokerite mine and oil and gas exploratory boreholes are presented. The detailed investigations carried out in the years 2004–2009 by Ukrainian-Polish expeditions were focused on discoveries of possible new sites of fauna fossils and human remains of European early modem humans (EEMH).The future discoveries at the paleontological site of Starunia are extremely important. They intend to carry out ecological assessment of soil, surface and stream waters, atmospheric air, snow, ashes of meadow grasses, radiological screening, and geo-radar sensing to find new locations of extinct mammals. The Starunia area meets all the requirements of a geopark according to UNESCO standards and concepts. The first research findings (1907) are connected with the remains of woolly rhinoceros, mammoth, horse, roe deer and other Pleistocene mammals which had been found in the ozokerite mine at the depth of 12 m near Starunia (Bohorodchany district, Ivano-Frankivsk region). In 1914 the scientists from Lviv (Ukraine) and Krakow (Poland) fully appreciated these discoveries and published a set of articles and a monograph. In 1929 the members of the expedition of Skill Academy (Krakow, Poland) found the remains of three more woolly rhinoceroses in the ozokerite mine at the depth of 17 m. Numerous bones of vertebrates (rodents), remains of mussels, a lot of species of insects, beetles, parasitic worms, fleas, butterflies, spiders, snails, vascular plants, mosses, seeds and branches of dwarf birch (Betula Nana), alder (Alnus glutinosa), and other fossil of tundra flora were also discovered. Polish scientists organized detailed investigations of flora and fauna around Starunia, their results were published in articles but the World War II suspended this process. The investigations around Starunia intensified the comprehensive study of stratigraphy, paleontology, paleogeography, geochronology and other aspects of the Quaternary Period. In 1932 there was established the International Geological Congress (the International Union of Quaternary Study) by INQUA in Leningrad. The main methodological principals of this study dealt with the investigations around Starunia.

A new addition to Pleistocene megalonychid sloth diversity in the northern Neotropics

We report here a new record of a megalonychid sloth from a late Pleistocene mammal assemblage from Cueva de Iglesitas (Mi.50), Caracas, Venezuela. This new site, the first with a Pleistocene fauna found in the vicinity of Caracas, is in a pristine geological and stratigraphic area and preserves previously untouched sediments containing fossils that provide important information about the late Pleistocene paleofauna and paleoenvironment of Caracas and the southwestern Caribbean region. A preliminary assessment of the relationship of this new sloth to other members of the Megalonychidae is presented.

First direct evidence of conservative foraging ecology of early Gigantopithecus blacki (~2Ma) in Guangxi, southern China.

Gigantopithecus blacki, the largest hominoid known, is one of the representative Pleistocene mammals in southern China and northern Southeast Asia. Here we investigate the feeding ecology of G. blacki in its core habitat (Guangxi, Southern China) during the early Early Pleistocene, which was the early period in its evolution. The stable isotopic (C, O) analysis of tooth enamel of the fauna associated with G. blacki (n=58), including the largest number of G. blacki teeth (n=12) to date from the Liucheng Gigantopithecus Cave (~2Ma), Guangxi, China, is undertaken. The δ13 C values of Liucheng fauna range from -12.9 to -19.0‰ with an average of -16.1 ± 1.3‰ (n=58) and the δ18 O values range from -4.3 to -9.6‰ with an average of -6.9 ± 1.2‰ (n=58). The δ13 C values of G. blacki range from -15.9‰ to -17.0‰ with an average of -16.5 ± 0.4‰ (n=12), and the δ18 O values vary from -5.9‰ to -7.5‰ with an average of -6.6 ± 0.5‰ (n=12). The isotopic data show Guangxi was characterized by closed C3 forest and humid climate in the early Early Pleistocene. Niche partitioning is found among G. blacki, Sinomastodon, Ailuropoda and Stegodon, the typical megafauna in South China in the early Early Pleistocene. This could be one of the important factors for them to co-exist until the Middle Pleistocene. Smallest isotopic variations of G. blacki are found compared with those of contemporary animals, indicating a conservative foraging ecology i.e., limited foraging area and/or narrow dietary flexibility. Furthermore, the more confined foraging ecology of G. blacki is also seen in comparison with fossil and extant large-bodied primates. However, the unique dietary pattern of G. blacki does not seem to have hindered its survival. The environment in Guangxi during the early Early Pleistocene offered the suitable conditions for G. blacki to become one of the typical species in the faunal assemblages.

Ancient enamel peptides recovered from the South American Pleistocene species Notiomastodon platensis and Myocastor cf. coypus

We used two fossil teeth from South American Pleistocene mammals to obtain subsuperficial acid etching samples. We employed samples from the species Notiomastodon platensis and Myocastor cf. coypus for the enamel etchings. The controls included an extant rodent (rat). After the first etching was discarded, a second 20-s etching (i.e., subsuperficial) was directly collected with a ZipTip and injected into an LTQ Orbitrap Velos for MS analysis. The peptides were identified with different software programs that used Peptide Spectrum Match (PSM) and de novo sequencing including similarity search strategies. Most of the peptides that were recovered from the enamel of the fossils belonged to enamel-specific proteins. To our knowledge, this is the first study that has described the recovery of enamel peptide molecules from extinct South American taxa, indicating that enamel peptide data from late Pleistocene fossils can be employed as an additional parameter for phylogenetic analysis, and that the sample can be obtained by a very conservative acid etching, with almost no damage to the fossils. SignificanceThis study shows that it is possible to obtain information based on plenty of ancient peptides recovered from subsuperficial enamel of fossil teeth from South American Pleistocene. The quality of the data suggests that peptides are likely the best preserved biomolecules under certain harsh environmental conditions. The recovery procedure only lasted 20 s and was minimally destructive to the fossils. This opens a myriad of new possibilities for the study of the past.

MAMÍFEROS PLEISTOCENOS DEL OESTE DE LA REGIÓN PAMPEANA, ARGENTINA

En el extremo meridional de América del Sur, la mayor parte del conocimiento paleomastozoológico proviene del sector este de la región Pampeana, más precisamente del ámbito de la provincia de Buenos Aires. En esta contribución se da a conocer un conjunto de mamíferos pleistocenos provenientes del extremo oeste de la región Pampeana (San Francisco, provincia de Córdoba). En el conjunto de taxones estudiados (compuesto por elementos pampeano-patagónicos adaptados a los climas áridos y fríos del Pleistoceno más tardío) resulta significativa la presencia del Equidae Equus (Amerhippus) neogeus y del Glyptodontidae Neosclerocalyptus paskoensis, ya que permite acotar la antigüedad al Lujanense (ca. 130-8 ka AP). Esta asociación es congruente con el desarrollo de un período glacial. Taxonómicamente, este conjunto de mamíferos resulta compatible con aquel conocido para el sector oriental de la región Pampeana, intensamente estudiada desde mediados del siglo XIX.

The Santa Vitória Alloformation: an update on a Pleistocene fossil-rich unit in Southern Brazil

The Santa Vitória Formation is a lithostratigraphic unit known for its fossil assemblage of Pleistocene mammals, established in 1973 from sediments exposed along the banks of Chuí Creek, in the southern coastal plain of the state of Rio Grande do Sul (CPRS), Brazil. The original description was presented in a Masters’ dissertation and never formally described in a peer-reviewed publication. Moreover, surveys and fossil collecting efforts developed in the last decade have led to a better understanding of its origin and nature. An updated description of this unit is presented here, which outcrops in areas occupied by barrier-lagoon depositional systems originated by eustatic oscillations. The formation encompasses Middle-Upper Pleistocene fluvial and eolian depositional systems and paleosols formed chiefly of fine to medium quartz sand, with subordinate clay, concentrations of iron and manganese oxides, and caliche nodules of pedogenic origin. It conformably overlies upper shoreface-foreshore marine deposits, and is overlain by loess deposited during the last glacial period. Here is proposed to re-define it as Santa Vitória Alloformation, considering that the use of an allostratigraphic framework to characterize this unit has the practical purpose of grouping depositional systems genetically unrelated to the barrier-lagoon systems.

Late Pleistocene Mammals from Kibogo, Kenya: Systematic Paleontology, Paleoenvironments, and Non-Analog Associations

ABSTRACT We report on the Late Pleistocene (36–12 ka) mammals from Kibogo in the Nyanza Rift of western Kenya, providing (1) a systematic description of the mammal remains, (2) an assessment of their paleoenvironmental implications, and (3) an analysis of the biogeographic implications of non-analog species associations. Kibogo has yielded one of the largest paleontological assemblages from the Late Pleistocene of eastern Africa, and it is dominated by grassland ungulates (e.g., equids and alcelaphin antelopes), including an assortment of extralimital (e.g., Equus grevyi, Ceratotherium simum, Redunca arundinum) and extinct species (Syncerus antiquus, Damaliscus hypsodon, Megalotragus sp.). The composition of the fauna, in conjunction with the soils and topography of the region, indicate the local presence of edaphic grassland situated within a broader environment that was substantially grassier and likely drier than at present. In contrast to non-analog faunas from higher latitudes (e.g., North America and western Eurasia), the climatic niches of non-analog species associations strongly overlap, indicating that non-analog climate regimes during the Late Pleistocene of eastern Africa are not necessary to account for the former association of presently allopatric species. The Kibogo faunas add to a growing body of evidence implying that the composition of present-day African herbivore communities is distinct from those of the geologically recent past.