Late Pleistocene Homo sapiens in a tropical rainforest fauna in East Java

2005 ◽  
Vol 49 (4) ◽  
pp. 536-545 ◽  
Author(s):  
Paul Storm ◽  
Fachroel Aziz ◽  
John de Vos ◽  
Dikdik Kosasih ◽  
Sinung Baskoro ◽  
...  
Author(s):  
Francisco J. Ayala ◽  
Camilo J. Cela-Conde

This chapter analyzes the transition of the hominins from the Middle Pleistocene to the Late Pleistocene. Two alternative models are explored, the “Multiregional Hypothesis” (MH) and the “Replacement Hypothesis,” and how each model evaluates the existing relationships between the taxa Homo neanderthalensis and Homo sapiens. Next is the investigation of the transitional (or “archaic,” if this grade is taken into account) exemplars found in Europe, Africa, and Asia and their evolutionary significance. In particular, the comparison between H. erectus and H. sapiens in China and Java is investigated, as the main foundation of the MH. The chapter ends with the surprising discovery of Homo floresiensis and its description and interpretations concerning its taxonomic and phylogenetic significance. The correlation between brain development and technological progress is at odds with the attribution of perforators, microblades, and fishing hooks to a hominin with a small cranial volume, similar to that of Australopithecus afarensis.


1990 ◽  
Vol 15 (3) ◽  
pp. 345-347 ◽  
Author(s):  
M. S. HOPKINS ◽  
A. W. GRAHAM ◽  
R. HEWETT ◽  
J. ASH ◽  
J. HEAD

Author(s):  
Tony Hallam

We saw in Chapters 5 and 7 that the Quaternary was a time of low extinction rates despite a succession of strong environmental changes induced ultimately by climate. This began to change from a few tens of thousands of years ago with the arrival on our planet of Homo sapiens sapiens, which can be translated from the Latin as the rather smug ‘ultrawise Man’. It is widely accepted today that the Earth is undergoing a loss of species on a scale that would certainly rank in geological terms as a catastrophe, and has indeed, been dubbed ‘the sixth mass extinction’. Although the disturbance to the biosphere being created in modern times is more or less entirely attributable to human activity, we must use the best information available from historical, archaeological, and geological records to attempt to determine just when it began. Towards the end of the last ice age, known in Europe as the Würm and in North America as the Wisconsin, the continents were much richer in large mammals than today: for example, there were mammoths, mastodonts, and giant ground sloths in the Americas; woolly mammoths, elephants, rhinos, giant deer, bison, and hippos in northern Eurasia; and giant marsupials in Australia. Outside Africa most genera of large mammals, defined as exceeding 44 kilograms adult weight, disappeared within the past 100,000 years, an increasing number becoming extinct towards the end of that period. This indicates that there was a significant extinction event near the end of the Pleistocene. This event was not simultaneous across the world, however: it took place later in the Americas than Australia, and Africa and Asia have suffered fewer extinctions than other continents. There are three reasons for citing humans as the main reason for the late Pleistocene extinctions. First, the extinctions follow the appearance of humans in various parts of the world. Very few of the megafaunal extinctions that took place in the late Pleistocene can definitely be shown to pre-date the arrival of humans. There has, on the other hand, been a sequence of extinctions following human dispersal, culminating most recently on oceanic islands. Second, it was generally only large mammals that became extinct.


2015 ◽  
Vol 84 (3) ◽  
pp. 368-381 ◽  
Author(s):  
Emily J. Beverly ◽  
Steven G. Driese ◽  
Daniel J. Peppe ◽  
L. Nicole Arellano ◽  
Nick Blegen ◽  
...  

The effect of changing environment on the evolution of Homo sapiens is heavily debated, but few data are available from equatorial Africa prior to the last glacial maximum. The Karungu deposits on the northeast coast of Lake Victoria are ideal for paleoenvironmental reconstructions and are best studied at the Kisaaka site near Karunga in Kenya (94 to > 33 ka) where paleosols, fluvial deposits, tufa, and volcaniclastic deposits (tuffs) are exposed over a ~ 2 km transect. Three well-exposed and laterally continuous paleosols with intercalated tuffs allow for reconstruction of a succession of paleocatenas. The oldest paleosol is a smectitic paleo-Vertisol with saline and sodic properties. Higher in the section, the paleosols are tuffaceous paleo-Inceptisols with Alfisol-like soil characteristics (illuviated clay). Mean annual precipitation (MAP) proxies indicate little change through time, with an average of 764 ± 108 mm yr− 1 for Vertisols (CALMAG) and 813 ± 182 to 963 ± 182 mm yr− 1 for all paleosols (CIA-K). Field observations and MAP proxies suggest that Karungu was significantly drier than today, consistent with the associated faunal assemblage, and likely resulted in a significantly smaller Lake Victoria during the late Pleistocene. Rainfall reduction and associated grassland expansion may have facilitated human and faunal dispersals across equatorial East Africa.


2020 ◽  
Vol 2 (7A) ◽  
Author(s):  
David Minnikin

The evolution of tubercle bacilli correlates closely with changes in cell envelope surface lipid composition (Donoghue et al. Diversity 2017, 9:46; Jankute et al. Scientific Reports 2017, 7:1315). Smooth, hydrophilic “Mycobacterium canettii” is the first recognisable member of the Mycobacterium tuberculosis complex, but it has reduced pathogenicity and poor aerosol transmission. In contrast, rough M. tuberculosis is very hydrophobic and readily spread in aerosols. Starting from hydrophilic surface lipids in environmental Mycobacterium kansasii, intermediate “M. canettii” adds hydrophobic lipids but retains overall cell hydrophilicity. Eliminating hydrophilic lipooligosaccharides (LOSs) and phenolic glycolipids (PGLs) from “M. canettii” leads to M. tuberculosis with a refined selection of hydrophobic lipids, namely phthiocerol dimycocerosates (PDIMs), pentaacyl trehaloses (PATs) and sulfoglycolipids (SGLs). The relative hydrophobicity of M. tuberculosis is double that of representatives of M. kansasii and “M. canettii”. The above changes have implications both for the onset of tuberculosis and pinpointing evolutionary hosts. Tuberculosis has not been found in Homo sapiens during the Late Pleistocene, but megafauna are the most likely hosts; characteristic bone lesions have been validated by TB DNA amplification and lipid biomarkers in bison metacarpals up to 17,000 years old. Late Pleistocene enhanced TB hydrophobicity and aerosolisation may have produced megafaunal pandemics, with extinction of bison, mastodons and contemporary taxa. The oldest H. sapiens tuberculosis is from the “Fertile Crescent” back to 9-11ka BP at the start of the Holocene. Naïve humans arriving “Out of Africa” may have encountered newly virulent tubercle bacilli of megafaunal origin, recently refined through a distinct “bottleneck”.


1999 ◽  
Vol 22 (4) ◽  
pp. 461-469 ◽  
Author(s):  
Walter A. Neves ◽  
Joseph F. Powell ◽  
Andre Prous ◽  
Erik G. Ozolins ◽  
Max Blum

Several studies concerning the extra-continental morphological affinities of Paleo-Indian skeletons, carried out independently in South and North America, have indicated that the Americas were first occupied by non-Mongoloids that made their way to the New World through the Bering Strait in ancient times. The first South Americans show a clear resemblance to modern South Pacific and African populations, while the first North Americans seem to be at an unresolved morphological position between modern South Pacific and Europeans. In none of these analyses the first Americans show any resemblance to either northeast Asians or modern native Americans. So far, these studies have included affirmed and putative early skeletons thought to date between 8,000 and 10,000 years B.P. In this work the extra-continental morphological affinities of a Paleo-Indian skeleton well dated between 11,000 and 11,500 years B.P. (Lapa Vermelha IV Hominid 1, or "Luzia") is investigated, using as comparative samples Howells' (1989) world-wide modern series and Habgood's (1985) Old World Late Pleistocene fossil hominids. The comparison between Lapa Vermelha IV Hominid 1 and Howells' series was based on canonical variate analysis, including 45 size-corrected craniometric variables, while the comparison with fossil hominids was based on principal component analysis, including 16 size-corrected variables. In the first case, Lapa Vermelha IV Hominid 1 exhibited an undisputed morphological affinity firstly with Africans and secondly with South Pacific populations. In the second comparison, the earliest known American skeleton had its closest similarities with early Australians, Zhoukoudian Upper Cave 103, and Taforalt 18. The results obtained clearly confirm the idea that the Americas were first colonized by a generalized Homo sapiens population which inhabited East Asia in the Late Pleistocene, before the definition of the classic Mongoloid morphology.


Author(s):  
Patrick Roberts

Popular philosophical associations of tropical forests, and forests in general, with an inherent ancestral state, away from the stresses, pollution, and technosphere of modern life, are nicely summarized by Murakami’s quote above (2002). Given the probable origins of the hominin clade in tropical forests, this quote is also apt from an evolutionary standpoint. Yet, somewhat surprisingly, tropical forests have frequently been considered impenetrable barriers to the global migration of Homo sapiens (Gamble, 1993; Finlayson, 2014). As was the case with the focus on ‘savannastan’ in facilitating the Early Pleistocene expansion of Homo erectus discussed in Chapter 3 (Dennell and Roebroeks, 2005), the movement of H. sapiens into tropical regions such as South Asia, Southeast Asia, and Australia has tended to be linked to Late Pleistocene periods when forests contracted and grasslands expanded (Bird et al., 2005; Boivin et al., 2013). Alternative narratives have focused on the importance of coastal adaptations as providing a rich source of protein and driving cultural and technological complexity, as well as mobility, in human populations during the Middle and Late Pleistocene (Mellars, 2006; Marean, 2016). The evidence of early art and symbolism at coastal cave sites such as Blombos in South Africa (Henshilwood et al., 2002, 2011; Vanhaeren et al., 2013) and Taforalt in North Africa (Bouzouggar et al., 2007) is often used to emphasize the role of marine habitats in the earliest cultural emergence of our species. Indeed, for the last decade, the pursuit of rich marine resources (Mellars, 2005, 2006) has been a popular explanation for the supposed rapidity of the ‘southern dispersal route’, whereby humans left Africa 60 ka, based on genetic information (e.g., Macaulay et al., 2005), to reach the Pleistocene landmass that connected Australia and New Guinea (Sahul) by c. 65 ka (Clarkson et al., 2017). In both of these cases, the coast or expanses of grassland have been seen as homogeneous corridors, facilitating rapid expansion without novel adaptation.


2016 ◽  
Vol 113 (23) ◽  
pp. 6388-6396 ◽  
Author(s):  
Nicole L. Boivin ◽  
Melinda A. Zeder ◽  
Dorian Q. Fuller ◽  
Alison Crowther ◽  
Greger Larson ◽  
...  

The exhibition of increasingly intensive and complex niche construction behaviors through time is a key feature of human evolution, culminating in the advanced capacity for ecosystem engineering exhibited by Homo sapiens. A crucial outcome of such behaviors has been the dramatic reshaping of the global biosphere, a transformation whose early origins are increasingly apparent from cumulative archaeological and paleoecological datasets. Such data suggest that, by the Late Pleistocene, humans had begun to engage in activities that have led to alterations in the distributions of a vast array of species across most, if not all, taxonomic groups. Changes to biodiversity have included extinctions, extirpations, and shifts in species composition, diversity, and community structure. We outline key examples of these changes, highlighting findings from the study of new datasets, like ancient DNA (aDNA), stable isotopes, and microfossils, as well as the application of new statistical and computational methods to datasets that have accumulated significantly in recent decades. We focus on four major phases that witnessed broad anthropogenic alterations to biodiversity—the Late Pleistocene global human expansion, the Neolithic spread of agriculture, the era of island colonization, and the emergence of early urbanized societies and commercial networks. Archaeological evidence documents millennia of anthropogenic transformations that have created novel ecosystems around the world. This record has implications for ecological and evolutionary research, conservation strategies, and the maintenance of ecosystem services, pointing to a significant need for broader cross-disciplinary engagement between archaeology and the biological and environmental sciences.


2015 ◽  
Vol 112 (9) ◽  
pp. 2682-2687 ◽  
Author(s):  
Christian A. Tryon ◽  
Isabelle Crevecoeur ◽  
J. Tyler Faith ◽  
Ravid Ekshtain ◽  
Joelle Nivens ◽  
...  

Kenya National Museums Lukenya Hill Hominid 1 (KNM-LH 1) is a Homo sapiens partial calvaria from site GvJm-22 at Lukenya Hill, Kenya, associated with Later Stone Age (LSA) archaeological deposits. KNM-LH 1 is securely dated to the Late Pleistocene, and samples a time and region important for understanding the origins of modern human diversity. A revised chronology based on 26 accelerator mass spectrometry radiocarbon dates on ostrich eggshells indicates an age range of 23,576–22,887 y B.P. for KNM-LH 1, confirming prior attribution to the Last Glacial Maximum. Additional dates extend the maximum age for archaeological deposits at GvJm-22 to >46,000 y B.P. (>46 kya). These dates are consistent with new analyses identifying both Middle Stone Age and LSA lithic technologies at the site, making GvJm-22 a rare eastern African record of major human behavioral shifts during the Late Pleistocene. Comparative morphometric analyses of the KNM-LH 1 cranium document the temporal and spatial complexity of early modern human morphological variability. Features of cranial shape distinguish KNM-LH 1 and other Middle and Late Pleistocene African fossils from crania of recent Africans and samples from Holocene LSA and European Upper Paleolithic sites.


AMERTA ◽  
2020 ◽  
Vol 29 (2) ◽  
pp. 1-17
Author(s):  
Truman Simanjuntak

Abstract. The Life of Early Modern Human in Indonesia: A Preliminary Synthesis. The Late Pleistocene period or, in broader sense, the second half of the Upper Pleistocene, was in general related to the emergence and development of Early Modern Human (EMH) in Indonesia. Archaeological evidences have more or less confirmed their existence - with records of their unique behavior - within the period. In spite of the still obscure date of their initial occupation, the available radiometry dating reveals that this early Homo sapiens had inhabited Indonesia, and Southeast Asia in general, at least since ca. 45 kya up to the end of the Ice Age. Some of the most prominent behavior phenomena, which distinct modern human to early men's behavior who inhabited Indonesia since millions of years previously, are: (I) exploitation of wider geographical area within the archipelago; (2) change of activity orientation from open-air areas to natural niches, such as caves and rock shelters; (3) development of lithic technology that produced flake tools, replacing the chopper/chopping tool groups; and (4) more advanced and diverse systems of subsistence with more varied animals to hunt. The entire phenomena of behavior are the main focus of this paper. Abstrak. Rentang waktu Plestosen Akhir atau paruh kedua Plestosen Atas pada umumnya merupakan periode yang mengait dengan kemunculan dan perkembangan Manusia Modern Awal (MMA) di Indonesia. Bukti-bukti arkeologi sedikit banyaknya telah meyakinkan keberadaannya, berikut rekaman perilakunya yang khas, dalam periode tersebut. Terlepas dari pertanggalan kolonisasi awal yang belum diketahui pasti dari manusia modern awal ini, pertanggalan radiometri yang tersedia menampakkan bahwa mereka telah menghuni Indonesia, dan Asia Tenggara pada umumnya, paling tidak sejak sekitar 45 ribu tahun lalu hingga akhir kala Plestosen.Beberapa fenomena perilaku yang paling menonjol, yang membedakannya dari perilaku manusia purba yang mendiami Indonesia sejak jutaan tahun sebelumnya, adalah: (1) ekploitasi geografi yang semakin luas di kepulauan; (2) perubahan lokasi hunian dari bentang alam terbuka ke relung-relung alam seperti gua dan ceruk; (3) pengembangan teknologi litik yang menghasilkan alat-alat serpih menggantikan alat-alat yang tergolong kelompok kapak perimbas/penetak; dan (4) sistem mata pencaharian yang lebih maju dan beragam dengan eksploitasi lingkungan (flora dan fauna) yang lebih bervariasi. Keseluruhan fenomena perilaku tersebut akan menjadi pokok bahasan tulisan ini.


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