Robert C. Walter

Natural Streams and the Legacy of Water-Powered Mills

Gravel-bedded streams are thought to have a characteristic meandering form bordered by a self-formed, fine-grained floodplain. This ideal guides a multibillion-dollar stream restoration industry. We have mapped and dated many of the deposits along mid-Atlantic streams that formed the basis for this widely accepted model. These data, as well as historical maps and records, show instead that before European settlement, the streams were small anabranching channels within extensive vegetated wetlands that accumulated little sediment but stored substantial organic carbon. Subsequently, 1 to 5 meters of slackwater sedimentation, behind tens of thousands of 17th- to 19th-century milldams, buried the presettlement wetlands with fine sediment. These findings show that most floodplains along mid-Atlantic streams are actually fill terraces, and historically incised channels are not natural archetypes for meandering streams.

Geology, geochronology, and rift basin development in the central sector of the Main Ethiopia Rift

Based on stratigraphic relationships and K/Ar dating of volcanic rocks from both of the escarpments, flanking plateaus, and from the rift floor of the central sector of the Main Ethiopian Rift, six major volcanic episodes are recognized in the rift9s development over a time span from the late Oligocene to the Quaternary. Using the K/Ar data, correlation of volcanic units from the six periods of activity throughout the study area forms the basis for establishing six time-stratigraphic chronozones for the central sector that are related to volcanism in the Ethiopian Cenozoic volcanic province. The oldest basalt and rhyolite flows exposed along the rift margins of the central sector are time correlative to, or older than, those in river canyons (for example, Blue Nile) on the adjacent northwest plateau. A thinned Mesozoic stratigraphic sequence along the Guraghe western rift margin suggests that doming may have preceded volcanism and rifting of the Cenozoic. By late Miocene time, at least by 8.3 Ma and 9.7 Ma, the eastern and western faulted margins, respectively, of the rift had formed at Guraghe and at Agere Selam as indicated by containment of flows of that age within the rift wall during eruption. A paroxysm of calc-alkaline ignimbrite activity produced voluminous flows nearly fully contained within the rift during the Pliocene epoch. The Munesa Crystal Tuff (3.5 Ma), a prominent marker tuff exposed on both rift margins, is present at depth in a geothermal well beneath the rift floor and indicates a minimum of 2 km of downthrow in the central sector since its eruption. Structural and stratigraphic relationships in the central sector indicate a two- stage rift development. This is characterized by an early phase (late Oligocene or early Miocene) of a series of alternating opposed half-grabens along the rift with alternating polarity, such as that in the present Gregory and Western Rifts of East Africa and symmetrical rifts that evolved from these grabens in late Miocene or early Pliocene time. Thus, evolution from alternating half-graben to a full symmetrical graben with a medially located neovolcanic zone that is bifurcated to marginal grabens in the northern part of the study area may be a fundamental part of the rifting process. The study indicates that there are major petrologic and tectonic differences between the Main Ethiopian Rift and the Gregory (Kenyan) Rift.

Intercalibration of astronomical and radioisotopic time

The 40Ar/39Ar radioisotopic dating technique is one of the most precise and versatile methods available for dating events in Earths history, but the accuracy of this method is limited by the accuracy with which the ages of neutron-fluence monitors (dating standards) are known. Calibrating the ages of standards by conventional means has proved difficult and contentious. The emerging astronomically calibrated geomagnetic polarity time scale (APTS) offers a means to calibrate the ages of 40Ar/39Ar dating standards that is independent of absolute isotopic abundance measurements. Seven published 40Ar/39Ar dates for polarity transitions, nominally ranging from 0.78 to 3.40 Ma, are based on the Fish Canyon sanidine standard and can be compared with APTS predictions. Solving the 40Ar/39Ar age equation for the age of the Fish Canyon sanidine that produces coincidence with the APTS age for each of these seven reversals yields mutually indistinguishable estimates ranging from 27.78 to 28.09 Ma, with an inverse variance-weighted mean of 27.95 ± 0.18 Ma. Normalized residuals are minimized at an age of 27.92 Ma, indicating the robustness of the solution.

Early human occupation of the Red Sea coast of Eritrea during the last interglacial

The geographical origin of modern humans is the subject of ongoing scientific debate. The ‘multiregional evolution’ hypothesis argues that modern humans evolved semi-independently in Europe, Asia and Africa between 100,000 and 40,000 years ago, whereas the ‘out of Africa’ hypothesis contends that modern humans evolved in Africa between 200 and 100 kyr ago, migrating to Eurasia at some later time. Direct palaeontological, archaeological and biological evidence is necessary to resolve this debate. Here we report the discovery of early Middle Stone Age artefacts in an emerged reef terrace on the Red Sea coast of Eritrea, which we date to the last interglacial (about 125 kyr ago) using U–Th mass spectrometry techniques on fossil corals. The geological setting of these artefacts shows that early humans occupied coastal areas and exploited near-shore marine food resources in East Africa by this time. Together with similar, tentatively dated discoveries from South Africa this is the earliest well-dated evidence for human adaptation to a coastal marine environment, heralding an expansion in the range and complexity of human behaviour from one end of Africa to the other. This new, widespread adaptive strategy may, in part, signal the onset of modern human behaviour, which supports an African origin for modern humans by 125 kyr ago.

Late Eocene–Recent volcanism and faulting in the southern main Ethiopian rift

Few constraints on the timing, amount and distribution of lithospheric extension associated with flood-basalt magmatism were available from the southern Main Ethiopian rift system, where the base of the Cenozoic volcanic succession is exposed by faulting. New structural observations, together with K–Ar and 40Ar/39Ar geochronology data from a transect of the Chamo basin–Amaro horst–Galana basin, show that basins are bounded by faults with steep dips at the surface, and the stratal dips of Eocene–Recent volcanic and sedimentary units are generally less than 20°. Little or no extension accompanied the extrusion of a 0.5 to 1 km thick sequence of transitional tholeiitic flood basalts between 45 and 35 Ma. Stratigraphical correlations with basins to the north and southwest suggest that felsic eruption(s) at c. 37 Ma blanketed much of the southern Ethiopian plateau region with a felsic tuff unit. A second, less widespread, episode of alkali basalt and trachyte volcanism occurred between 18 and 11 Ma, and Recent alkali basalt volcanism occurs within the Chamo basin. The attitude, distribution, and diversity of Neo–gene–Recent volcanic and sedimentary strata within the Chamo and Galana basins indicate that crustal extension, basin subsidence, and rift flank uplift began during or after the second flood-basalt phase. Based on cross-sectional reconstruction to the top of the Oligocene tuff, we estimate a minimum of 12 km crustal extension (β ≈ 1.12), and infer that maximum extension across the southern Ethiopian rift is less than 25 km. Extension is primarily accommodated by slip along the border faults bounding the asymmetric basins, with small amounts of extension occurring within the hanging walls. Crude estimates of original basalt layer thickness prior to erosion in the Amaro region suggest that roughly comparable volumes of basaltic material erupted during the two episodes of flood-basalt magmatism (45–35 Ma and 18–11 Ma). The small amounts of lithospheric extension and the large volumes of magma estimated in this study of the southern Main Ethiopian rift suggest a very hot plume and/or efficient thinning of the mantle lithosphere from below by mantle plume processes during the two discrete episodes of flood-basalt volcanism.

Stratigraphy, palaeoenvironments and model for the deposition of the Abdur Reef Limestone:: context for an important archaeological site from the last interglacial on the Red Sea coast of Eritrea

Stone tools discovered within uplifted marine terraces along the Red Sea coast of Eritrea at the Abdur Archaeological Site, dated to 125±7 ka (the last interglacial, marine isotope stage 5e), show that early humans occupied coastal areas by this time [Walter et al. (2000) Nature 405, 65–69]. In the present paper the stratigraphy, facies types and faunal composition from 25 measured sections of the tool-bearing Abdur Reef Limestone (ARL) are documented in detail and interpreted to provide a palaeoenvironmental context for the stone artefacts and a model for the deposition of the ARL. The ARL represents a complex marine terrace sequence. Erosional surfaces indicative of interrupted sedimentation are locally observed at two levels within the ARL. They subdivide the complex into three subunits, named 5e1, 5e2, and 5e3, representing different stages of the marine isotope stage 5e sea level highstand, comprising six depositional phases (I–VI) of the ARL. Subunit 5e1 begins with the initial transgression of the 5e sea level highstand leading to the deposition of widespread lag gravels on which rich oyster beds developed in shallow water (phase I). It further records rapid deepening accompanied by the deposition of low-energy carbonates with scarce corals (phase II), and later shoaling characterised by local development of a fringing reef tract in a sedimented environment (phase III). Subunit 5e1 is capped locally by a burrowed hardground that is laterally equivalent to depositional discontinuities, interpreted as caused by a globally recognised mid-5e sea level low stand (phase IV). Extensive reef build-up in response to sea level rise and improved conditions for coral growth characterises subunit 5e2 (phase V). A possible second sea level drop during the 5e highstand is inferred from the oyster-encrusted upper surface of subunit 5e2. Subunit 5e3 encompasses restricted coral patches that developed on the upper surface of the underlying subunit during the last stage of the 5e marine high stand (phase VI). Two different toolkits are found in the ARL. One consists of bifacial hand axes and cores of the Acheulian industry, typically associated with the oyster beds encrusted on the transgressive lag deposits. The other consists of Middle Stone Age (MSA)-type obsidian flakes and blades, mainly found in the nearshore and beach environments alongside debris from marine invertebrates and large land mammals. The distribution of these tools suggests that foraging activities of early humans varied with environmental setting. The Abdur Archaeological Site represents a late example of the Acheulian/MSA transition, seen as a benchmark for early modern human behaviour, and is, to date, the earliest well-dated example of early human adaptation to marine food resources.

New data from Hadar (Ethiopia) support orbitally tuned time scale to 3.3 MA

Support for the astronomically calibrated geomagnetic polarity time scale is provided by new 40Ar/39Ar dating and magnetostratigraphic data from the Hadar Formation, Ethiopia. Three tuffs and a basalt flow at Hadar span the Mammoth subchron of the Gauss chron, and range in age from 3.18±0.01 to 3.40 ±0.03 Ma. Interpolation of sediment accumulation rates in two magnetostratigraphic sections yields an estimated age range of 3.30±0.02 to 3.21±0.01 Ma for the Mammoth subchron, closely coinciding with orbitally based predictions of 3.33 to 3.22 Ma rather than with previous estimates of 3.15 to 3.05 Ma.

A proboscidean from the late oligocene of eritrea, a "missing link" between early elephantiformes and elephantimorpha, and biogeographic implications

We report on a late Oligocene proboscidean species from Eritrea, dated to 26.8 ± 1.5 Mya. This “missing link” between early elephantiformes and Elephantimorpha is the oldest known nongomphothere proboscidean to probably display horizontal tooth displacement, typical of elephants [Elephantimorpha consists of Mammutida (mastodons) and Elephantida, and Elephantida includes gomphotheres, stegodons, and elephants]. Together with the newly discovered late Oligocene gomphotheres from Chilga, Ethiopia, the Eritrean taxon points to the importance of East Africa as a major area for the knowledge of the early evolution of Elephantimorpha before the faunal exchange between Eurasia and Africa.

Tephrochronology of Bed I, Olduvai Gorge: An application of laser-fusion 40Ar39Ar dating to calibrating biological and climatic change

Abstract New geochronological data indicate that hominid-bearing deposits of middle to upper Bed I at Olduvai Gorge comprise an extremely brief interval of time, from about 1.80 to 1.75 Ma. Dates for lower Bed I suggest that the age of the lower boundary of the Olduvai subchron is >1.98 Ma, over 100 ka older than the currently accepted value. The results of this study enable rates of biological, archaeological, geological, and climatic change during Bed I times to be determined with great precision. The new date for the base of the Olduvai subchron has important implications for calibrating the age of marine and continental deposits that rely on the Olduvai subchron for chronologic control.

Petrogenesis of a basalt-rhyolite tephra from the west-central Afar, Ethiopia

The Cindery Tuff is an unusual tephra fall deposit that contains evidence for the mixing of basaltic and rhyolitic liquids prior to eruption. It contains clear rhyolitic glass shards together with brown basaltic glass spheres and a broadly bimodal phenocryst assemblage. Brown glasses are ferrobasaltic in composition and are similar to the voluminous Pliocene tholeiites of the surrounding west-central Afar volcanic field; both are enriched in the light rare earth and incompatible elements and possess higher 87Sr/86Sr and lower 143Nd/144Nd than MORB. Rhyolitic glasses are subalkaline and, compared to the basaltic glasses, are strongly depleted in the compatible elements and enriched in the incompatible elements. Both glass types have similar incompatible element and isotopic ratios, and with the rhyolite glass showing a 2-fold parallel enrichment in rare earth element abundances over the basaltic glass. These observations suggest that the two glasses are genetically related.Rare glasses with intermediate compositions occur as phenocryst melt inclusions, as mantles on phenocrysts and as free pumice clasts. Their major element contents do not point to an origin by simple hybrid mixing of the basaltic and rhyolitic melts. Rather, major element mixing calculations indicate formation of the intermediate and rhyolite melts by fractionation of the observed phenocryst assemblage, using a starting composition of the observed basaltic glass. Model calculations from trace element data, though lacking from the intermediate glasses, support fractional crystallization. The bimodal mineral assemblage argues against an immiscible liquid origin for the contrasting glass compositions.