An Evaluation of the Organic Geochemical Potential to Reconstruct Mid-Pleistocene Paleoclimate Adjacent to an Established Hominin Site: Lake Magadi, Kenya

The paleo-Lake Magadi was one of five sites selected by the Hominin Sites and Paleolakes Drilling Project (HSPDP), with the goal of establishing high resolution, multi-proxy reconstructions of climate and environmental change adjacent to established hominin sites. The overall goal of the HSPDP is to provide a context of climate and environmental change for many of the milestones in hominin adaptation and evolution, spatially adjacent to where hominins lived, and temporally resolved to evolutionary (orbital to sub-millennial) timescales. The core recovered from Lake Magadi is estimated to represent the past 1.08 Ma, during which several significant hominin adaptation and evolutionary events occurred. Based on initial chronology efforts by HSPDP collaborators, the Magadi core can be separated into four sections: 0-26 kyr, 26-165 kyr, 165-242.8 kyr, and 242.8 kyr to 1.08 Ma. We estimate the future biomarker potential for the four sections, and determine Lake Magadi to have particularly exciting promise for the 0-26 kyr and 26-165 kyr sections. To that end, 68 pilot samples were analyzed for leaf waxes (n-alkanes and fatty acids) and glycerol dialkyl glycerol tetraethers (GDGTs), to evaluate the potential to reconstruct vegetation regime, precipitation, and temperature from Magadi. The n-alkanes were determined to have a better potential to yield compound specific carbon and hydrogen isotope data than fatty acids due to better chemical separation, and approximately 70% of samples analyzed for n-alkanes recorded a robust terrestrial signal. The TetraEther indeX with 86 carbon atoms (TEX86) temperature proxy was established for ~90% of samples analyzed for isoprenoid GDGTs, however the Methane Index and Ring Index suggest that the TEX86 is not applicable to temperature reconstruction at Magadi. Additionally, no samples contained the complete suite of branched GDGTs necessary to construct the Methylation of Branched Tetraethers and Cyclisation of Branched Tetraethers (MBT/CBT) temperature proxy. Initial reconstruction of Lake Magadi paleoclimate shows an oscillating vegetation regime from mid-Pleistocene to present, but a directional trend towards a cooler and drier climate. Plotted alongside 18O data from the GRIP-2 ice core, our climate data demonstrate a potentially interesting correlation between climate at Lake Magadi and ice volume in the Arctic

Deep drilling at the Chalco lake:A technical report

En este artículo se presenta un resumen de las actividades realizadas para la recuperación de la totalidad de la secuencia lacustre del lago de Chalco. Mediante estudios geofísicos se determinó la distribución y espesor de los sedimentos lacustres con base en lo cual se seleccionó el sitio de perforación. Con datos de los espectros H/V de sísmica pasiva se hizo un mapa de isofrecuencias que definieron una región con sedimentos lacustres y material volcánico granulado de hasta 300 m de espesor. El uso de métodos electromagnéticos mostró cambios en la resistividad eléctrica relacionados con variaciones en la composición de la columna sedimentaria; entre 100 – 120 m de profundidad hay un primer aumento en la resistividad asociado al incremento de materiales volcaniclásticos, y entre 330 – 400 m de profundidad un segundo aumento asociado a la presencia de coladas de basalto. Fueron perforados tres pozos con recuperación continua, llegando a profundidades de 420 m en el pozo A, 310 m en el B y 520 en el C. Durante el trabajo de perforación se tomaron muestras para el análisis geomicrobiológicos y de metagenómica. Durante el proceso de perforación se recuperó un total de 1152 m de sedimentos con una profundidad máxima de 520 m. El porcentaje de recuperación de la columna sedimentaria varió entre 88 a 92 % en los tres sondeos. Los resultados del análisis de susceptibilidad magnética en las tres secuencias indica que los primeros 260 m son sedimentos lacustres, entre 260 y 300 m los sedimentos son más gruesos y debajo de los 300 m son predominantemente volcaniclásticos. El análisis de la secuencia sedimentaria del lago de Chalco de los últimos ~300000 años, permitirá documentar y ampliar el conocimiento acerca de la variabilidad climática de la zona, la historia paleoambiental, la historia del cierre de la cuenca, el desarrollo del sistema lacustre y la recurrencia de la actividad volcánica en la cuenca. Además, el estudio de las propiedades físicas de esta secuencia sedimentaria es importante para la modelación de la propagación de ondas sísmicas y de la estructura de la cuenca, así como para mejorar la capacidad de modelación del proceso de subsidencia del terreno que experimenta esta región. This paper presents a short description of the coring operations undertaken to recover the full lacustrine sedimentary sequence from Chalco. Geophysical techniques were used to determine the distribution and thickness of the sediments in order to select the drilling site. Resonance frequencies determined from H/V spectral ratios were used to determine an area where lake sediments reached 300 m thickness. Electromagnetic survey showed two changes in electric resistivity which were related to changes in sediment composition, the first from 100 to 120 m, related to an increase in volcanoclastic sediments and the second from 330 to 400 m related to the presence of a basaltic flows. Three wells were drilled with continuous recovery, reaching depths of 420 m in well A, 310 in B and 520 in C. Samples for geomicrobiological and metagenomics studies were collected during drilling operations. A total of 1152 m of core sediments were recovered reaching a maximum depth of 520 m. Recovery percentages were between 88 and 92 % in the three wells. Magnetic susceptibility analyses in the three sequences show that the first 260 m are mostly lake sediments, between 260 and 300 m sediments are coarser and below 300 m they are mostly volcaniclastic. Analysis of the sedimentary sequence of Lake Chalco that covers the last ~300000 years will allow documenting and extending the knowledge of climate variability in area, the paleoenvironmental history, basin closure history, lacustrian system development and volcanic activity recurrence. Studies of the physical properties of this sequence will be important for seismic propagation and basin structure modeling, and also will improve modeling of the subsidence process that this region experiences

Microbial biomarkers reveal a hydrothermally active landscape at Olduvai Gorge at the dawn of the Acheulean, 1.7 Ma

Landscape-scale reconstructions of ancient environments within the cradle of humanity may reveal insights into the relationship between early hominins and the changing resources around them. Many studies of Olduvai Gorge during Pliocene–Pleistocene times have revealed the presence of precession-driven wet–dry cycles atop a general aridification trend, though may underestimate the impact of local-scale conditions on early hominins, who likely experienced a varied and more dynamic landscape. Fossil lipid biomarkers from ancient plants and microbes encode information about their surroundings via their molecular structures and composition, and thus can shed light on past environments. Here, we employ fossil lipid biomarkers to study the paleolandscape at Olduvai Gorge at the emergence of the Acheulean technology, 1.7 Ma, through the Lower Augitic Sandstones layer. In the context of the expansion of savanna grasslands, our results represent a resource-rich mosaic ecosystem populated by groundwater-fed rivers, aquatic plants, angiosperm shrublands, and edible plants. Evidence of a geothermally active landscape is reported via an unusual biomarker distribution consistent with the presence of hydrothermal features seen today at Yellowstone National Park. The study of hydrothermalism in ancient settings and its impact on hominin evolution has not been addressed before, although the association of thermal springs in the proximity of archaeological sites documented here can also be found at other localities. The hydrothermal features and resources present at Olduvai Gorge may have allowed early hominins to thermally process edible plants and meat, supporting the possibility of a prefire stage of human evolution

Enabling State Adoption of Non-Targeted Analysis (NTA) to Address Pressing Public Health Needs: Maryland, Minnesota, and California Leading the Way

Poster for SETAC on Nov. 12-16, 2023 in Louisville, KYScience Inventory, CCTE products: https://cfpub.epa.gov/si/si_public_search_results.cfm?advSearch=true&showCriteria=2&keyword=CCTE&TIMSType=&TIMSSubTypeID=&epaNumber=&ombCat=Any&dateBeginPublishedPresented=07/01/2017&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&DEID=&personName=&personID=&role=Any&journalName=&journalID=&publisherName=&publisherID=&sortBy=pubDate&count=25</p