scholarly journals A review on paleoenvironment suitability for hominid fossils and other early vertebrate faunas: a case from Pucangan and Kabuh Formations, Central and East Java, Indonesia

Author(s):  
Dasapta Erwin Irawan ◽  
Rubiyanto Kapid

Abstract The northern part of the East Java Basin has become a focus of research by earth scientists, among others, because of the existence of hominid fossils and remains of other vertebrate taxa within the Quaternary sedimentary sequence. Fossil-bearing layers are found in the Kendeng Zone, mostly within the well-known Pucangan and Kabuh Formations, which are distributed from Central to East Java. However, not all formations contain vertebrate fossils as well as hominid elements. It is important to consider what factors may have influenced the concentration of vertebrate fossils in those formations. In this study, we describe sedimentary facies at three key field locations: Sangiran, Ngawi, and Mojokerto. Our study indicates that vertebrate remains and hominid fossils mainly accumulated in continental sediments associated with lacustrine and fluvial systems. In this regard, Sangiran and Ngawi B offer the greatest prospect for yielding hominid remains, owing to their unique paleoenvironmental and paleogeographical settings as a highland during the Early–Middle Pleistocene period. Certain parts of the Kabuh Formation in the Mojokerto region also hold high potential, especially those displaying evidence of continental deposition.

2019 ◽  
Vol 131 (9-10) ◽  
pp. 1744-1760 ◽  
Author(s):  
Xiaofei Hu ◽  
Dianbao Chen ◽  
Baotian Pan ◽  
Jinjun Chen ◽  
Jian Zhang ◽  
...  

AbstractWe studied the magnetostratigraphy and sedimentary facies of a 550-m-long drill core from the Jiudong Basin in the NE Tibetan Plateau. Our aims were to reconstruct the late Cenozoic sedimentary evolution of this foreland basin, and to determine the spatiotemporal pattern of growth of the Qilian Shan. The magnetostratigraphy indicates that the sedimentary sequence was deposited during ca. 7–0 Ma. From ca. 6.7–3.0 Ma, the sediment accumulation rate increased gradually from ∼30 mm/k.y. to 120 mm/k.y., which was associated with the gradual evolution of sedimentary facies from a shallow lake/delta front to braided rivers. The progradation of the depositional system from 7 Ma to 3 Ma probably reflects the growth of the relief of the Qilian Shan caused by tectonic uplift. The occurrence of a continuous braided river environment from 3 Ma to the present suggests that the high relief of the Qilian Shan developed before 3 Ma. An abrupt decrease of the sedimentation rate to ∼46 mm/k.y. during 3.0–1.8 Ma, and the deposition of coarse-grained sediments, indicates the uplift of the basin center. We interpret this to reflect the propagation of the thrust system of the Qilian Shan into the basin along a southward-dipping décollement from ca. 3 Ma. Climatic changes may have influenced the sedimentary sequence by introducing long-distance-transported thin coarse sand/gravel layers which are sandwiched within the sequence, and likely were a response to cooling events or climatic transitions. The widespread occurrence of deformation within the basin region in the NE Tibetan Plateau at ca. 3 Ma indicates that this date marks the basinward growth of the deformation system.


2002 ◽  
Vol 53 (3) ◽  
pp. 313-322 ◽  
Author(s):  
Lionel E. Jackson ◽  
Charles Tarnocai ◽  
Robert J. Mott

AbstractFour paleosols were intersected in a core drilled into the colluvial fill of a largely buried meltwater channel that was last active during the youngest of the pre-Reid glaciation (0.99-0.78 Ma) in the Dawson Range, Yukon Territory. The paleosols are classified as Podzols. The sedimentary sequence and paleosols indicate that at least two middle Pleistocene glacial and interglacial periods are represented in the core. The mean annual temperature exceeded 0° C for thousands of years in the upland environment of the Dawson Range at 61° N during these interglacial periods.


2017 ◽  
Vol 166 ◽  
pp. 204-226 ◽  
Author(s):  
Pedro P. Cunha ◽  
António A. Martins ◽  
Jan-Pieter Buylaert ◽  
Andrew S. Murray ◽  
Luis Raposo ◽  
...  

2021 ◽  
Author(s):  
Laura Pioli ◽  
Margherita Mussi ◽  
Rita T. Melis

<p>The Upper Awash valley runs across a volcano-sedimentary sequence dated from Late Miocene to about 500 my ago. The volcano sedimentary sequence in the Upper Awash valley developed within a closed basin at the western margin of the Main Ethiopian Rift branch and was affected by tephra sedimentation from nearby sources but also from volcanoes from the rift floor, and local fissural/dome eruptions. Dynamic interaction between rift tectonics, volcanic activity, tephra erosion and redeposition created a complex sedimentary environment constituting an exceptional fossil trap. In the area of Melka Kunture, the sediments host numerous fossils and archeological remains of Early-Middle Pleistocene (Oldowan and Acheulean) and Upper Pleistocene age. This is one of the most relevant African locations for researching human evolution.</p><p>The valley sequence formed after deposition of the large ignimbrite sheet of the Munesa tuff, within a paleo fluvial system which developed within lateral rift faults. Sedimentation rates significantly decreased after 500 my ago, probably due to decline of the volcanic activity in the area.</p><p>The basin stratigraphy consists of a composite sequence of primary (fall and flow) volcanic facies interbedded with reworked sediments emplaced in a low energy floodplain environment. The sequence is dominated by the deposit of one large pyroclastic density current (Kella Tuff) which is a main marker layer dated at 1.2 My. Deposition of the Kella Tuff had deep impact on the area leading to a complete reorganization of the drainage system and river channel migration and development of a disconformity in the southern Melka Kunture area.</p><p>Stratigraphic correlation is based on the interpretation of the basin history and evolution and has a crucial relevance not only for the reconstruction of the paleoenvironment but also for the interpretation of the paleontological and archeological data.</p><p> </p>


1968 ◽  
Vol 33 ◽  
pp. 367-376 ◽  
Author(s):  
Phillip V. Tobias

For over 40 years South Africa and for over 25 years East Africa have been yielding fossilized remains of creatures identified on their bony structure as lowly members of the Hominidae or human family. From five sites in the Republic of South Africa (Taung, Sterkfontein, Kromdraai, Makapansgat and Swartkrans) and from three sites in the Republic of Tanzania (Garusi, Olduvai and Peninj) have emerged a considerable number of hominid fossils of the Lower and Middle Pleistocene. Most of them have been classified as members of an extinct hominid genus called by R. A. Dart, the discoverer of the first specimen, Australopithecus. Although variable among themselves, the structural features which aligu these fossils with the Hominidae, rather than with the family of the apes or Pongidae, are as follows:—(1) Australopithecus showed modifications of his skeleton—especially the pelvis, femur, ankle and foot—which permit us to infer that he walked upright, even though such modifications had not progressed as far as in hominids of the genus Homo.(2) The calvaria or brain-case of Australopithecus was characterized by a number of hominid features, such as marked flexion of the axis of the cranial base; forward displacement of the occipital condyles by which the skull articulates with the vertebral column; a small, low nuchal area at the back of the base of the cranium, for the attachment of those muscles which tether the back of the cranium to the trunk—the last two features suggesting a different, more man-like poise of the cranium on the spine; the consistent development, early in life, of a pyramidal mastoid process as in man, and unlike the apes in which this process develops inconsistently and then only later in life (Schultz 1950).(3) The canine teeth of Australopithecus, like those of Homo, lacked the enlargement and marked interlocking which characterizes the upper and lower teeth of the apes—correspondingly, Australopithecus lacked the diastemata or gaps which, in apes, lodge the projecting tips of the enlarged canines.(4) Another dental characteristic shared by Australopithecus with Homo was the bicuspid structure of the first lower premolar tooth: in apes, this tooth does not possess two sub-equal cusps but is a cutting or sectorial tooth with one predominating cusp, like a canine tooth.(5) Although the brain-size of Australopithecus (as inferred from the volumetric capacity of the brain-case) was no bigger than that of some largerbrained apes, the shape or morphology of the brain, as preserved in endocranial casts, approached more closely to that of early Homo than to that of the apes. We have, however, no direct evidence whether these external observable differences between the brains of Australopithecus and of apes were paralleled by internal, microscopic, structural differences such as those which have been demonstrated between modern man and modern apes.(6) Many other detailed morphological features of the skull, the teeth and other bones of Australopithecus showed human resemblances.


2022 ◽  
Author(s):  
Elizabeth L. Miller ◽  
Mark E. Raftrey ◽  
Jens-Erik Lund Snee

ABSTRACT In a reconnaissance investigation aimed at interrogating the changing topography and paleogeography of the western United States prior to Basin and Range faulting, a preliminary study made use of U-Pb ages of detrital zircon suites from 16 samples from the Eocene–Oligocene Titus Canyon Formation, its overlying units, and correlatives near Death Valley. The Titus Canyon Formation unconformably overlies Neoproterozoic to Devonian strata in the Funeral and Grapevine Mountains of California and Nevada. Samples were collected from (1) the type area in Titus Canyon, (2) the headwaters of Monarch Canyon, and (3) unnamed Cenozoic strata exposed in a klippe of the Boundary Canyon fault in the central Funeral Mountains. Red beds and conglomerates at the base of the Titus Canyon Formation at locations 1 and 2, which contain previously reported 38–37 Ma fossils, yielded mostly Sierran batholith–age detrital zircons (defined by Triassic, Jurassic, and Cretaceous peaks). Overlying channelized fluvial sandstones, conglomerates, and minor lacustrine shale, marl, and limestone record an abrupt change in source region around 38–36 Ma or slightly later, from more local, Sierran arc–derived sediment to extraregional sources to the north. Clasts of red radiolarian-bearing chert, dark radiolarian chert, and quartzite indicate sources in the region of the Golconda and Roberts Mountains allochthons of northern Nevada. Sandstones intercalated with conglomerate contain increasing proportions of Cenozoic zircon sourced from south-migrating, caldera-forming eruptions at the latitude of Austin and Ely in Nevada with maximum depositional ages (MDAs) ranging from 36 to 24 Ma at the top of the Titus Canyon Formation. Carbonate clasts and ash-rich horizons become more prevalent in the overlying conglomeratic Panuga Formation (which contains a previously dated 15.7 Ma ash-flow tuff). The base of the higher, ash-dominated Wahguyhe Formation yielded a MDA of 14.4 Ma. The central Funeral Mountains section exposes a different sequence of units that, based on new data, are correlative to the Titus Canyon, Panuga, and Wahguyhe Formations at locations 1 and 2. An ash-flow tuff above its (unexposed) base provided a MDA of 34 Ma, and the youngest sample yielded a MDA of 12.7 Ma. The striking differences between age-correlative sections, together with map-based evidence for channelization, indicate that the Titus Canyon Formation and overlying units likely represent fluvial channel, floodplain, and lacustrine deposits as sediments mostly bypassed the region, moving south toward the Paleogene shoreline in the Mojave Desert. The profound changes in source regions and sedimentary facies documented in the Titus Canyon Formation took place during ignimbrite flareup magmatism and a proposed eastward shift of the continental divide from the axis of the Cretaceous arc to a new divide in central Nevada in response to thermal uplift and addition of magma to the crust. This uplift initiated south-flowing fluvial systems that supplied sediments to the Titus Canyon Formation and higher units.


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