FLUVIAL CONDITIONS DURING THE HOLOCENE AS EVIDENCED BY ALLUVIAL SEDIMENTS FROM ABOVE HOWISON'S POORT, NEAR GRAHAMSTOWN, SOUTH AFRICA

1998 ◽  
Vol 53 (1) ◽  
pp. 53-67 ◽  
Author(s):  
C. A. Lewis ◽  
P. M. Illgner
Author(s):  
Antônio Magalhães Jr ◽  
Allaoua Saadi

The study of fluvial dynamics of the Rio das Velhas in the section connecting the Quadrilátero Ferríferoand the Bambuí basin, relying on a compilation of geomorphological, sedimentological and structuraldata indicates a Cenozoic morphogenesis controlled by uplift of regional scale with interference of faultslocated at the contacts of morphostructural compartments. These compartments are strongly adapted tothe Precambrian litostructural domains controlling the geomorphological configuration of the differentparts of the river valley.The initial chronological datum is marked by remainders of the Sulamericana Surface (Neogene).During the Plio-Pleistocene period three levels of stepped terraces were formed. During the Holocene ainner floodplain developed in the Lower Terrace.The level of the Upper Terrace (Pliocene) corresponds to the end of dissection phase which reaches adepth of 150 m and shows a equilibrated longitudinal profile over the whole area. The sediments of theMiddle and Lower Terraces have been deposited after new dissection phases with minimum depths of 60and 10 m, respectively. These data of dissections depths and the stamped position of the floodplain confirmsthe gradual decreasing of the regional uplift intensity during the Pleistocene times.The last three events of the valley formation indicate a superimposition of the Rio das Velhas onto thestructures of the Quadrilátero Ferrífero with formation of a water-gap at the passage of the Serra do curral,named “Fecho de Sabará”. In consequence occurs a strong local retention of alluvial sediments causing aimportant alteration of river dynamics.The decreasing uplift during Holocene times is accompanied by the transition from braided channelssystems, prevailing during the Pleistocene, to a meandering channel type. The effects of historic miningactivity induce the return to the braided system.Tectonic activity by faulting is demonstrated by dislocations in the alluvial sequences of the LowerTerrace and in the longitudinal profile of the Middle and Upper Terraces with a total off-set of 50 m aswell as by river capture younger than the Middle Terrace.


2020 ◽  
Vol 97 ◽  
pp. 1-41 ◽  
Author(s):  
Erich C. Fisher ◽  
Hayley C. Cawthra ◽  
Irene Esteban ◽  
Antonieta Jerardino ◽  
Frank H. Neumann ◽  
...  

AbstractWaterfall Bluff is a rock shelter in eastern Pondoland, South Africa, adjacent to a narrow continental shelf that limited coastline movements across glacial/interglacial cycles. The archaeological deposits are characterized by well-preserved stratigraphy, faunal, and botanical remains alongside abundant stone artifacts and other materials. A comprehensive dating protocol consisting of 5 optically stimulated luminescence ages and 51 accelerator mass spectrometry 14C ages shows that the record of hunter-gatherer occupations at Waterfall Bluff persisted from the late Pleistocene to the Holocene, spanning the last glacial maximum and the transition from the Pleistocene to the Holocene. Here, we provide detailed descriptions about the sedimentary sequence, chronology, and characteristics of the archaeological deposits at Waterfall Bluff. Remains of marine mollusks and marine fish also show, for the first time, that coastal foraging was a component of some hunter-gatherer groups’ subsistence practices during glacial phases in the late Pleistocene. The presence of marine fish and shellfish further demonstrates that hunter-gatherers selectively targeted coastal resources from intertidal and estuarine habitats. Our results therefore underscore the idea that Pondoland's coastline remained a stable and predictable point on the landscape over the last glacial/interglacial transition being well positioned for hunter-gatherers to access resources from the nearby coastline, narrow continental shelf, and inland areas.


Radiocarbon ◽  
2017 ◽  
Vol 59 (4) ◽  
pp. 1067-1086 ◽  
Author(s):  
Michaela Ecker ◽  
James Brink ◽  
Michael Chazan ◽  
Liora Kolska Horwitz ◽  
Julia A Lee-Thorp

AbstractWonderwerk Cave has yielded one of the longest and most complete Holocene Later Stone Age (LSA) records for the arid interior of South Africa. This paper presents the results of a new radiocarbon dating program for Excavation 1 that is explored within a Bayesian model of all existing Wonderwerk Cave radiocarbon (14C) dates for the Holocene. The proposed model, usingPhaseswithin an OxCalSequencemodel, provides robust age estimates for changes in the technological and paleoenvironmental record at the site. The more precise dates allow a comparison of the timing of climate shifts across the interior of southern Africa and begin to allow us to identify whether hiatuses in human occupation, or cultural shifts, are synchronous across broader areas of the subcontinent, or not.


2016 ◽  
Vol 404 ◽  
pp. 183 ◽  
Author(s):  
K.L. Kirsten ◽  
T. Haberzettl ◽  
M. Wündsch ◽  
L.J. Quick ◽  
T. Kasper ◽  
...  
Keyword(s):  

1988 ◽  
Vol 43 (147) ◽  
pp. 68
Author(s):  
H. J. Deacon ◽  
R. R. Inskeep
Keyword(s):  

1995 ◽  
Vol 69 (1) ◽  
pp. 171-181 ◽  
Author(s):  
John Pether

Small holes of irregular outline and mainly 0.2 to 1.5 mm in diameter are present in the exteriors of molluscan shells obtained from the latest Quaternary transgressive sequence on the Orange Shelf, Benguela region, off southwestern Africa. In shell interiors, the shell surrounding the holes is broken out to form flaring, conical spalls. The holes are clearly not borings, but are punctures caused by a small, pointed object having been forcefully driven into the shell. The holes in bivalves occur preferentially in small, thin-shelled tellinids and are nonrandomly placed in the central portions of valves. It is proposed that the holes are praedichnia produced by the rapid, ballistic-like raptorial strikes of spearing stomatopods, the pointed dactyl tips having penetrated the shells. Associated evidence of shell smashing, consisting of large holes in valves and gastropod whorls, supports the suggestion of stomatopod activity. The only stomatopod that inhabits the Benguela ecosystem, the spearer Pterygosquilla armata capensis Manning, 1969, is the probable tracemaker. Although shell nearly 1 mm thick has been pierced, the apparent selection of thin-shelled tellinids (0.14 to 0.34 mm thick) may reflect the requirement of shelling smashing in order to access the tissues. Nevertheless, the spearing of shelled prey is atypical for stomatopods and therefore confirmatory zoological observations are required, particularly to clarify the context of shell spearing. The ichnogenus Belichnus is proposed to accommodate these unique traces of pointed impacts, with ichnospecies B. monos (single punctures) and B. dusos (combined punctures) to accommodate the main morphological varieties observed.


2020 ◽  
Vol 116 (1/2) ◽  
Author(s):  
Hugo G. Nami ◽  
Carlos A. Vasquez ◽  
Lyn Wadley ◽  
Paloma de la Peña

Palaeomagnetic data from a sedimentary section spanning the Holocene and terminal Pleistocene (~13 kya) from Rose Cottage Cave, eastern Free State (South Africa), are reported. The palaeomagnetic analysis took into account rock magnetism and directional analysis. The former reveals that most samples show stable single domain and superparamagnetic particles of Ti-poor magnetite and haematite. Natural remanent magnetisation directions were determined by progressive alternating field demagnetisation methodology. Directional analysis shows normal directions between samples 18 to 39 and 85 to 92; however, during the Early and Late Holocene in samples principally from RC40 to 84 ‘anomalous’ directions occurred. There is a significant westward shift in declination of ~80°, and a conspicuous fluctuating inclination in the lower part of the section during the Early Holocene at ≥9.5 kya and before ~12.0/13.0 kya. This palaeomagnetic record might become a chronostratigraphical marker for latest Pleistocene/Holocene sedimentary deposits in South Africa. Our two new accelerator mass spectrometry radiocarbon dates for the sampled deposit are 9500±50 BP and 1115±30 BP.


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