Academic literature on the topic 'YR 3000'

AbstractSediments began accumulating in nine mires on Barrington Tops, on the Northern Tablelands of New South Wales, before 11,000 yr B.P., and peat became common in the region by 8600 yr B.P. Sedimentation rates were low, but increased markedly about 3000 yr B.P. and again around 500 yr B.P. as a result of regional climatic change. A comparison of the results with other environmental data from the region suggests that conditions in the early Holocene were warmer and moister than at present, but that cooler and drier environments developed about 3000 yr B.P. In the last 500 yr a slight warming and either increased precipitation or cloudiness has become evident.

AbstractArchaeological materials in several prairie mounds in the northern Western Lowlands of southeastern Missouri indicate that mounds began forming prior to ca. 5000-3000 yr B.P. The mounds subsequently were inundated and built up to their modern configuration by aggradational and reworking processes. Human use of the mounds may have been tied to exploitation of aquatic animals residing in backwater habitats during periods of prolonged flooding. Principal features of the sampled portion of the mound field include preoccupation topographic highs, early occupation (ca. 5000-3000 yr B.P.) layers that drape the topographic highs, and later occupation (ca. 3000-950 yr B.P.) layers that drape earlier occupation layers and extend onto intermound areas.

AbstractA 5000-yr stratigraphic record containing fossil pollen, charcoal, and bones of the extinct Quaternary megafauna from Andolonomby, a hypersaline pond in arid southwestern Madagascar, shows evidence for climatic desiccation beginning about 3000 yr B.P. Pollen spectra shift at this time from primarily arboreal taxa characteristic of forests and woodlands of more mesic western Madagascar, to wooded savanna typical of somewhat drier localities. Between 3000 and 2000 yr B.P., the site became increasingly arid. Charcoal and pollen evidence indicates that increased fire and disturbance occurred at the site beginning ca. 1900 yr B.P., probably signaling the beginning of human settlement in the area. The fossil record suggests that various human and natural factors on the island may have interacted in the subsequent millennium to culminate in the extinction of the entire endemic megafauna.

AbstractDirectly dated Cucurbita from archaeological sites near Lake Huron expand the range and human usage of adventive, cultivated wild gourds or squash into the Great Lakes region, USA, by 4000 14C yr BP. The data also show that domesticated C. pepo squash was cultivated there by 3000 14C yr BP. Although milder Hypsithermal climate may have been a contributing factor, squash and gourds expanded northward during the mid-Holocene mainly by human agency and may be the first human-introduced adventive plant in temperate North America. Even after 3000 14C yr BP, when domesticated squash generally replaced wild varieties at northern sites, squash stands were probably informally managed rather than intensively cultivated.

Sediments of Balsam Meadow have produced a 11,000-yr pollen record from the southern Sierra Nevada of California. The Balsam Meadow diagram is divided into three zones. (1) The Artemisia zone (11,000–7000 yr B.P.) is characterized by percentages of sagebrush (Artemisia) and other nonarboreal pollen higher than can be found in the modern local vegetation. Vegetation during this interval was probably similar to the modern vegetation on the east slope of the Sierra Nevada and the climate was drier than that of today. (2) Pinus pollen exceeded 80% from 7000 to 3000 yr B.P. in the Pinus zone. The climate was moister than during the Artemisia zone. (3) Fir (Abies, Cupressaceae, and oak (Quercus) percentages increased after 3000 yr B.P. in the Abies zone as the modern vegetation at the site developed and the present cool-moist climatic regime was established. Decreased fire frequency after 1200 yr B.P. is reflected in decreased abundance of macroscopic charcoal and increased concentration of Abies magnifica and Pinus murrayana needles.

AbstractClimatic changes in the Qinghai-Xizang Plateau of China were studied by analyzing the composition of peat and layers of sand and gravel distributed along the southern slopes of Nianqing-Tanggula and Gangdise Mountains, cross sections of deposits near a number of interior lakes in Xizang, past glacial variations on the southern slope of Nianqing-Tanggula Mountain, and landform changes south of the Yaluzangbu River. Such geologic evidence suggests a division of five climatic periods since the beginning of the Holocene: (1) The Wumadung interval, 10,000–7500 yr B.P., slightly cold and dry; (2) Qilongduo interval, 7500-3000 yr B.P., warm and moist; (3) the mid-Neoglacial period, 3000-1500 yr B.P., cold, except between 2500 and 200 yr B.P. when it was warmer; (4) the Dawelong interval, 1500-300 yr B.P., mild; and (5) the Little Ice Age, 300-0 yr B.P., cold. These changes progressed in a similar but not identical pattern as those in the northeastern part of China and in the northern region of Europe.

Typhoon is an important meteorological phenomenon that affects the living and development of human beings on the southern China coast. However, there is still lack of clarity in the paleo-typhoon history and its influence on the evolution of the ancient human settlement environment since the mid-Holocene. Here, we identify six typhoon-like deposits from a core retrieved from the northern South China Sea shelf, close to the Pearl River Estuary, based on accelerated mass spectrometry 14C dating, grain size, and geochemistry. The sand fractions, CaO, Sr, SiO2/TiO2, and SiO2/Al2O3 were used to indicate the typhoon-like deposits. Results show that the ages with high-frequency typhoons are present ~200–300 cal yr BP, ~800–1000 cal yr BP, ~1500–1700 cal yr BP, ~2000–2100 cal yr BP, ~2400–2500 cal yr BP, and ~2700–3000 cal yr BP. Our results are comparable to the records from adjacent regions. Significantly, the vast tides occurred in the duration of ~2700–3000 cal yr BP in southern China, which probably caused the ancestors’ migration to the inland. Further studies are needed to deeply study the paleo-typhoon history in the southern China coast to verify our results.

AbstractAnalysis of diatoms, pollen, and the carbon-isotopic composition of a sediment core from a brackish marsh in the northern part of the San Francisco Estuary has provided a paleosalinity record that covers the past 3000 yr. Changes in marsh composition and diatom frequencies are assumed to represent variations in freshwater inflow to the estuary. Three periods of relatively high salinity (low freshwater inflow) are indicated, 3000 to 2500 cal yr B.P., 1700 to 730 cal yr B.P., and ca. A.D. 1930 to the present. The most recent period of high salinity is primarily due to upstream storage and water diversion within the Sacramento–San Joaquin watershed, although drought may also have been a factor. The two earlier high-salinity periods are likely the result of reduced precipitation. Low salinity (high freshwater flow) is indicated for the period 750 cal yr B.P. to A.D. 1930.

Sedimentological, malacological, and pollen analyses from 14C-dated alluvial sections from the Luján River provide a detailed record of environmental changes during the Holocene in the northeastern Pampas of Argentina. From 11,200 to 9000 14C yr B.P., both sedimentary and biological components suggest that the depositional environment was eutrophic, alkaline, and freshwater to brackish shallow water bodies without significant water circulation. During this time, bioclastic sedimentation was dominant and the shallow water bodies reached maximum development as the climate became more humid, suggesting an increase in precipitation. Short-term fluctuations in climate during the last stage of this interval may have been sufficient to initiate changes in the water bodies, as reduction of the volume alternated with periods of flooding. The beginning of the evolution of shallow swamps in the wide floodplain or huge wetlands was contemporaneous with a sea level lower than the present one. From 9000 and 7000 14C yr B.P., mesotrophic, alkaline, brackish, probably anoxic swamps existed. Between 7000 and 3000 14C yr B.P., anoxic calcareous swamps were formed, with subaerial exposure and development of the Puesto Berrondo Soil (3500–2900 14C yr B.P.). A trend to a reduction of water bodies is recorded from 9000 to ca. 3000 14C yr B.P., with a significant reduction after ca. 7000 14C yr B.P. A shift to subhumid–dry climate after 7000 14C yr B.P. appears to be the main cause. During this time, an additional external forcing toward higher groundwater levels was caused by Holocene marine transgression causing changes in the water bodies levels. The climate became drier during the late Holocene (ca. 3000 yr B.P.), when clastic sedimentation increased, under subhumid–dry conditions. Flood events increased in frequency during this time. From ca. A.D. 1790 to present, the pollen record reflects widespread disturbance of the vegetation during the European settlement.

Störung des G1-Restriktionspunkts des Zellzyklus und Verlust der Wachstumskontrolle in Folge der Inaktivierung des Rb-Signalwegs ist ein häufiges Ereignis in malignen Tumoren. Gemeinsam mit der Hemmung von Apoptose-Signalwegen sind solche genetischen Ereignisse zentrale pathogenetische Faktoren der Tumorentstehung. Diese Veränderungen prägen aber auch entscheidend die Tumorbiologie und bestimmen somit intrinische und erworbene Therapieresistenz und konsequenterweise auch die klinische Prognose der Tumorerkrankung. In der vorliegenden Arbeit wurden Veränderungen im Rb- und im p53-Signalweg in Plattenepithelkarzinomen des Ösophagus untersucht. Diese retrospektive Studie wurde an Tumorproben von 53 mit kurativer Intention R0-resezierten Patienten durchgeführt. Proteinexpression wurde mittels Immunhistochemie und Mutationen mittels SSCP-PCR analysiert. Aktivierende Punktmutationen des K-ras Onkogens wurden mittels mutationsselektiver genomischer PCR und eines sequenzspezifischen Festphasen-Hybridisierungstests nachgewiesen. Die Analyse der individuellen Gene zeigte, dass Expressionsverlust der Rb-Signalwegskomponenten p16INK4a, p21CIP/WAF-1, p27KIP1 und von Rb selbst, sowie die Überexpression von Cyclin D1 bzw. Verlust des pro-apoptotischen Bcl-2 Homologs Bax mit schlechter Prognose, d.h. kürzerem Überleben korrelierte. Überexpression von Cyclin E, p53 oder Bcl-2, sowie Mutation von p53 bzw. K-ras zeigten hingegen keinen Einfluss auf die Prognose. Das längste Überleben wurde in einer Subgruppe von Patienten beobachtet deren Tumore eine Kombination günstiger Genotypen zeigte, und zwar niedrige Cyclin D1 Expression, sowie hohe Expression von Rb, p21CIP/WAF-1, p16INK4a und Bax. Diese Ergebnisse zeigen, dass eine Multigen- oder "Multimarker"-Analyse von Genen, die konsekutiv oder synergistisch in Zellzyklus- und Apoptose-Signalwegen agieren, zur Prognoseabschätzung der Analyse individueller Gene deutlich überlegen ist. Die Identifikation solcher genetischer Markerprofile sollte sich auch zukünftig als nützlich für die klinische Entscheidungsfindung in der Therapie maligner Tumore erweisen und wird konventionelle klinische und pathologische Faktoren komplementieren, die bisher keine ausreichende Prognoseabschätzung erlauben.
Malignant tumors frequently show inactivation of the Rb pathway and, as a result, deregulation of the G1 restriction point of the cell cycle and loss of growth control. Together with the inhibition of apoptosis signaling pathways, such events are key pathogenetic factors in tumor development. Moreover, these aberrations are decisive in determining tumor biology and characteristics such as intrinisic or acquired resistance to therapy and, consequently, the clinical prognosis of the malignant disease. In the present work, aberrations in the Rb and the p53 pathway were analysed. This retrospective study was undertaken in a cohort of 53 patients with esophageal squamous cell carcinoma who underwent R0 resection with a curative intent. Protein expression in tumor samples was analysed by means of immunohistochemistry and mutations were investigated by the use of genomic SSCP-PCR. Activating point mutations of the K-ras oncogene were detected by the use of mutation-selective genomic PCR and a sequence specific solid phase hybridization assay. The analysis of individual genes showed a correlation between poor prognosis, i.e. short overall survival, and loss of the Rb pathway components p16INK4a, p21CIP/WAF-1, p27KIP1, and Rb itself, or overexpression of cyclin D1 or loss of the pro-apoptotic Bcl-2 homolog Bax. In contrast, overexpression of cyclin E, p53 or Bcl-2 and mutation of p53 or K-ras had no influence on disease prognosis. The longest survival was found in a subgroup of patients whose tumors exhibited a combination of favorable genotypes, i.e. low expression of cyclin D1, and high expression of Rb, p21CIP/WAF-1, p16INK4a and Bax. These results demonstrate that a multigene or "multimarker"-analysis of genes that act consecutively or synergistically in cell cycle and apoptosis signaling pathways is far superior to determine disease prognosis when compared to the analysis of individual genes. The identification of such genetic marker profiles should proove beneficial in clinical decision making in the therapy of malignant tumors. In the future, such diagnostic tools may be useful to complement conventional clinical and pathologic factors which in most instances do not allow prediction of disease prognosis.

Zielsetzung In den Industrieländern stellt der Schlaganfall nach kardiovaskulären und Krebs – erkrankungen die dritthäufigste Krankheitsgruppe dar. Im Hinblick auf die Therapie des akuten Schlaganfalls muss die bildgebende Diagnostik schnell und einfach das Ausmaß der zerebralen Ischämie beschreiben können. Ziel dieser Studie war die Einführung und die Validierung eines CT – Protokolls, welches die Diagnostik des akuten Schlaganfalls verbessern soll. Zu diesem CT – Protokoll gehören ein Nativ – CT des Schädels, eine CT – Perfusionsuntersuchung und eine CT – Angiographie. Zusätzlich wollte diese Arbeit herausfinden, ob es physiologische Unterschiede zwischen der grauen Substanz und der weißen Substanz gibt, deren Kenntnis entscheidend für die Auswertung von computertomographischen Perfusionsuntersuchungen sind. Material und Methoden Insgesamt wurden 101 Patienten (Alter von 14 – 94 Jahre, mittleres Alter 69 Jahre) mit einem 8 – bzw. 16 – Zeilen – MSCT (Light Speed Ultra oder Light Speed pro 16, GE Healthcare), die zur Abklärung einer zerebralen Ischämie zum CT vorgestellt wurden, untersucht. Zuerst wurde eine native CT – Serie akquiriert. In der Untersuchung der zerebralen Perfusion wurde eine 2 cm breite Schicht über 60 sec mit 20 intermittierenden Aufnahmen während einer Injektion von 40 ml Kontrastmittel (Iopromid, Jodgehalt von 370 mg) aufgezeichnet. Daran an schloss sich eine CT – Angiographie Untersuchung. Zur Bestimmung des regionalen zerebralen Blutflusses, des regionalen zerebralen Blutvolumens und der mittleren Verweildauer wurden definierte Messfelder (Regions of Interests, ROIs) bestimmt und mit der kontralateralen Hemisphäre verglichen. Ergebnisse Es konnte gezeigt werden, dass der regionale zerebrale Blutfluss und das Blutvolumen im Bereich der Hirnrinde höher sind als im Hirnmark. Insgesamt wurden 66 Patienten mit einer zerebralen Ischämie wurden gefunden. Bei 22 dieser Patienten konnte ein Infarktgeschehen in der Nativ – CT diagnostiziert werden. Diese Ischämien ließen sich auch in der CT – Perfusion mit reduziertem regionalem zerebralem Blutfluss und verlängerter mittlerer Verweildauer nachweisen. Zusätzlich fanden sich 44 Patienten von 101 Untersuchten, die in der CT – Perfusion ein Perfusionsdefizit aufwiesen. Bei diesen Patienten ließ sich kein entsprechendes Korrelat in der Nativ – CT nachweisen. Für 38 dieser 44 Patienten konnte eine CTA durchgeführt werden, wovon für 35 Patienten ein Korrelat zwischen der CT – Perfusion und der CTA gefunden werden konnte. Schlussfolgerung Die Ergebnisse dieser Arbeit zeigen, dass es physiologische Unterschiede zwischen der Hirnrinde und dem Hirnmark gibt, deren Kenntnis für die Bewertung computertomographischer Perfusionsuntersuchungen eine wesentliche Interpretationshilfe darstellt. In Bezug auf die Diagnostik des akuten Schlaganfalls mit der Nativ – CT konnte diese Arbeit zeigen, dass der Nachweis von Infarktfrühzeichen eingeschränkt ist. Mit Hilfe der CT – Perfusion ist es möglich, anhand von zerebralen Perfusionswerten den Schweregrad und die Ausdehnung der zerebralen Ischämie zu bestimmen. Die CT – Angiographie zeigt eine gute Korrelation zur CT – Perfusion, es lassen sich zuverlässig Gefäßverschlüsse darstellen. Im Hinblick auf das weitere Therapievorgehen geben diese Methoden eine wichtige Hilfestellung, etwa zur Überlegung, ob man eine Lysetherapie durchführen sollte oder nicht.
Purpose Stroke is the third – leading cause of death in developed countries, following cardiovascular disease and cancer. There is a need for an easily and rapidly performed technique to detect cerebral ischemia in the first hours after its occurrence. The purpose of this study was the introduction and validation of a Stroke protocol which includes an unenhanced CT scan, a CT Perfusion and a CT Angiography. Furthermore, the purpose of this study was to determine if there is a difference between Perfusion parameters in gray and white matter, which are necessary to know while performing perfusion maps. Data and Methodology A total of 101 patients (age range 14 – 94, average age 69 years) were examined using multiple row CT (8 / 16 row multiple detector, light ultra speed or light speed 16, GE medical systems) for diagnosing cerebral ischemia. First a series of native images was acquired. During the examination of cerebral perfusion a 2 cm wide slab was recorded for 60 sec with 20 intermittent scans following injection of 40 ml of contrast medium with an iodine content of 370 mg / ml. By defining Regions of Interests (ROIs) regional cerebral blood flow (CBF), regional cerebral blood volume (CBV) and mean transit time (MTT) were calculated. Results Physiological regional cerebral blood flow and cerebral blood volume in gray matter were higher than in white matter. In total 66 patients with a cerebral ischemia were found. The unenhanced CT detected 22 patients with cerebral ischemia, which were confirmed by CT Perfusion in all cases. These ischemic areas revealed reduced regional CBF and extended MTT. Furthermore an ischemia correlative was discovered by perfusion analysis for 44 patients (out of 101 investigated) where the extent of the cerebral ischemia had not been visible by unenhanced CT. For 38 out of 44 patients with cerebral ischemia we were able to perform a CTA. For 35 out of these 38 patients, we found a sizable correlation between perfusion maps and CTA. Conclusion There are physiological differences for CT Perfusion parameters between gray and white matter, which are necessary to know for the interpretation of perfusion maps. However, this examination was able to show that unenhanced CT is not always capable of showing early CT signs. With the help of CT perfusion it is possible to detect the extent of acute cerebral ischemia. Furthermore, CT Angiography shows a sizable correlation compared to CT Perfusion. In conjunction, these methods give important Information for the early diagnosis and the therapeutic strategy of ischemic brain injury.

We analyze a 2400-year rainfall reconstruction from an ultra-high-resolution absolutely-dated stalagmite (JX-6) from southwestern Mexico (Lachniet et al., 2012). Oxygen isotope variations correlate strongly to rainfall amount in the Mexico City area since 1870 CE, and for the wider southwestern Mexico region since 1948, allowing us to quantitatively reconstruct rainfall variability for the Basin of Mexico and Sierra Madre del Sur for the past 2400 years. Because oxygen isotopes integrate rainfall variations over broad geographic regions, our data suggest substantial variations in Mesoamerican monsoon strength over the past two millennia. As a result of low age uncertainties (≤ 11 yr), our stalagmite paleoclimate reconstruction allows us to place robust ages on past rainfall variations with a resolution an order of magnitude more precise than archeological dates associated with societal change. We relate our new rainfall reconstruction to the sequence of events at Teotihuacan (Millon, 1967; Cowgill, 2015a) and to other pre-Colombian civilizations in Mesoamerica. We observe a centuries long drying trend that culminated in peak drought conditions in ca. 750 CE related to a weakening monsoon, which may have been a stressor on Mesoamerican societies. Teotihuacan is an ideal location to test for links between climate change and society, because it was located in a semi-arid highland valley with limited permanent water sources, which relied upon spring fed irrigation to ensure a reliable maize harvest (Sanders, 1977). The city of Teotihuacan was one of the largest Mesoamerican cities, which apparently reached population sizes of 80,000 to 100,000 inhabitants by AD 300 (Cowgill, 1997; 2015a). Following the “Great Fire”, which dates approximately to AD 550, population decreased to lower levels and many buildings were abandoned (Cowgill, 2015). Because of the apparent reliance on rainwater capture (Linn é, 2003) and spring-fed agriculture in the Teotihuacan valley to ensure food security and drinking water, food production and domestic water supplies should have been sensitive to rainfall variations that recharge the surficial aquifer that sustained spring discharge prior recent groundwater extraction.

Periodic attempts to plot global distribution of erosion and sedimentation usually attribute most of Southeast Asia with a very high sediment yield (Milliman and Meade 1983). The erosion rates and sediment yield figures are especially high for maritime Southeast Asia. Milliman and Syvitski (1992), for example, listed 3000 t km−2 yr−1 for the archipelagos and peninsulas of Southeast Asia. They provided a number of natural explanations for the high erosion rate: location near active plate margins, pyroclastic eruptions, steep slopes, and mass movements. This is also a region with considerable annual rainfall, a very substantial percentage of which tends to be concentrated in a few months and falls with high intensity. Part of Southeast Asia (the Philippines, Viet Nam, Timor) is visited by tropical cyclones with heavy, intense rainfall and possible associated wind damage to existing vegetation. The fans at the foot of slopes, the large volume of sediment stored in the channel and floodplain of the rivers, and the size of deltas all indicate a high rate of erosion and episodic sediment transfer. This episodic erosion and sediment transfer used to be controlled for most of the region by the thick cover of vegetation that once masked the slopes. When vegetation is removed soil and regolith de-structured, and natural slopes altered, the erosion rates and sediment yield reach high figures. Parts of Southeast Asia display striking anthropogenic alteration of the landscape, although the resulting accelerated erosion may be only temporary, operating on a scale of several years. Over time the affected zones shift, and slugs of sediment continue to arrive in a river but from different parts of its drainage basin. The combination of anthropogenic alteration and fragile landforms may give rise to very high local yields. Sediment yields of more than 15 000 t km−2 yr−1 have been estimated from such areas (Ruslan and Menam, cited in Lal 1987). This is undoubtedly towards the upper extreme, but current destruction of the vegetation cover due to deforestation, expansion of agriculture, mining, urbanization, and implementation of large-scale resettlement schemes has increased the sediment yield from < 102 to > 103 t km−2 yr−1.

The ocean and the atmosphere exchange massive amounts of carbon dioxide (CO2). The pre-industrial influx from the ocean to the atmosphere was 70.6 Gt C yr –1 , while the flux in the opposite direction was 70 Gt C yr –1 ( IPCC 2007 ). Since the Industrial Revolution an anthropogenic flux has been superimposed on the natural flux. The concentration of CO2 in the atmosphere, which remained in the range of 172–300 parts per million by volume (ppmv) over the past 800 000 years ( Lüthi et al. 2008 ), has increased during the industrial era to reach 387 ppmv in 2009. The rate of increase was about 1.0% yr –1 in the 1990s and reached 3.4% yr –1 between 2000 and 2008 ( Le Quéré et al. 2009 ). Future levels of atmospheric CO2 mostly depend on socio-economic parameters, and may reach 1071 ppmv in the year 2100 ( Plattner et al. 2001 ), corresponding to a fourfold increase since 1750. As pointed out over 50 years ago, ‘human beings are now carrying out a large scale geophysical experiment of a kind that could not have happened in the past nor be reproduced in the future’ ( Revelle and Suess 1957 ). Anthropogenic CO2 has three fates. In the years 2000 to 2008, about 29% was absorbed by the terrestrial biosphere and 26% by the ocean, while the remaining 45% remained in the atmosphere ( Le Quéré et al. 2009 ). The accumulation of CO2 in the atmosphere increases the natural greenhouse effect and generates climate changes ( IPCC 2007 ). It is estimated that the surface waters of the oceans have taken up 118 Pg C, or about 25% of the carbon generated by human activities since 1800 ( Sabine et al. 2004 ). By taking CO2 away from the atmosphere, the oceanic and terrestrial sinks mitigate climatic changes. Should their efficiency decrease, more CO2 would remain in the atmosphere, generating larger climate perturbations. This book has four main groups of chapters.

ABSTRACT Mono Lake occupies an internally drained basin on the eastern flank of the Sierra Nevada, and it is sensitive to climatic changes affecting precipitation in the mountains (largely delivered in the form of snowpack). Efforts to recover cores from the lake have been impeded by coarse tephra erupted from the Mono Craters, and by disruption of the lake floor due to the uplift of Paoha Island ~300 yr ago. In this study, we describe the stratigraphy of cores from three recent campaigns, in 2007, 2009, and 2010, and the extents and depths of the tephras and disturbed sediments. In the most successful of these cores, BINGO-MONO10-4A-1N (BINGO/10-4A, 2.8 m water depth), we used core stratigraphy, geochemistry, radiocarbon dates, and tephrostratigraphy to show that the core records nearly all of the Holocene in varying proportions of detrital, volcanic, and authigenic sediment. Both the South Mono tephra of ca. 1350 cal yr B.P. (calibrated years before A.D. 1950) and the 600-yr-old North Mono–Inyo tephra are present in the BINGO/10-4A core, as are several older, as-yet-unidentified tephras. Laminated muds are inferred to indicate a relatively deep lake (³10 m over the core site) during the Early Holocene, similar to many records across the region during that period. The Middle and Late Holocene units are more coarsely bedded, and coarser grain size and greater and more variable amounts of authigenic carbonate detritus in this interval are taken to suggest lower lake levels, possibly due to lower effective wetness. A very low lake level, likely related to extreme drought, is inferred to have occurred sometime between 3500 and 2100 cal yr B.P. This interval likely corresponds to the previously documented Marina Low Stand and the regional Late Holocene Dry Period. The BINGO/10-4A core does not preserve a complete record of the period encompassing the Medieval Climate Anomaly, the Little Ice Age, and the historical period, probably due to erosion because of its nearshore position.

The use of fossil fuels—petroleum, natural gas, and coal—is ubiquitous today and has made possible the advances of modern civilization. These fuels are capable of providing energy for a variety of applications—from very small to very large—and touch our lives in many ways. A small gas-fired heater uses about 50,000 Btu/hr (1 standard cubic foot [scf] of gas/min) and keeps our homes warm. A 200-horsepower gasoline engine in a family car consumes around 2 gal/hr of oil and can carry a load of five passengers a distance of 60 miles on a level highway. An 1,800-ton/hr cement plant consumes 900 MBtu/hr (about 0.9 million scf gas/hr) when in full operation and produces the building material widely used for constructing homes, offices, industries, roads, and bridges. A large, coal-fired electric power station (1,000 MW rating) requires between 300 and 500 tons of coal per hour and produces enough electricity to power half a million homes. The range of power that fossil fuels, particularly oil, can deliver is truly amazing: the same basic fuel that powers jet aircraft also powers children’s model aircraft engines. It is unlikely that aircraft will ever be powered by solar panels mounted on the wings or by on-board nuclear reactors. The importance of fossil fuels in our lives cannot be overemphasized. It took millions of years to accumulate them, and their potential exhaustion in just a few centuries should seriously concern all of us. In this chapter, we briefly review the circumstances that led to formation of our fossil fuels and then discuss how much of each of them is available. This discussion requires clarifying the special meanings ascribed to such terms as reserves and resources. For all three fuels, we look at the global distribution of our resources. We also present estimates of possible resource lifetimes under varying conditions of use and indicate the nominal equipment and infrastructure requirements for producing these inherited resources at a rate of 1 CMO/yr. As we shall see, our conventional reserves are somewhat limited, but our resource base is large, and unconventional oil and gas resources offer a substantially greater potential. Nonetheless, exploiting unconventional resources is certain to be more expensive and, in most cases, potentially more damaging to the environment.