Titlebook: Limnogeology: Progress, Challenges and Opportunities; A Tribute to Elizabe Michael R. Rosen,David B. Finkelstein,Sila Pla-Pue Book 2021 The

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Middle Holocene Hydrologic Changes Catalyzed by River Avulsion in Big Soda Lake, Nevada, USAnd the stable- isotope and diatom assemblages indicate a consistently hypersaline lake until near the top of the core, when fresh water entered the lake due to irrigation and canal building in the twentieth century. The stable isotopes of the calcite abruptly change from inversely varying isotopic c

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A 12,000 Year Diatom-Based Paleoenvironmental Record from Lago De Zirahuén, Mexiconating the diatom assemblages. The lake deepening is associated with the last two La Magueyera lava flows that caused the final damming of the lake. These volcanic events increased hydrothermal activity and eutrophic conditions in the lake and favored increased silica availability for the . blooms,

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Sedimentary Record of the Zacapu Basin, Michoacán, México, and Implications for P’urhépecha Culture o known as Late Uricho phase). In this time span, the population may have witnessed the volcanic activity of the Capáxtiro volcano (between 193 BC (2143 y BP) and 84 BC (2034 y BP) and the Malpaís Prieto volcano (AD 826 - 962 or 1124 - 988 y BP), but also the tectonic activity of nearby faults (i.e.

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Stratigraphy and Sedimentology of the Upper Pleistocene to Holocene Lake Chalco Drill Cores (Mexico c, with (i) organic-rich silty clay, (ii) sapropelic silty clay, and (iii) peat; (2) Diatomaceous, with laminated, banded, and mottled diatomaceous silty clay; (3) Calcareous, with banded or massive carbonate silty clay and ostracod-rich layers; (4) Clastic, with silty clay, sand, and gravel, both c

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2211-2731 ogic processes and basin descriptions in North and South America, Europe, Africa, and China..*Free supplementary material available online for chapters 3,11,12 and 13..Access by searching for the book on link.springer.com.978-3-030-66578-4978-3-030-66576-0Series ISSN 2211-2731 Series E-ISSN 2211-274X

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