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Michael W. Binford

Researcher at University of Florida

Publications -  78
Citations -  4996

Michael W. Binford is an academic researcher from University of Florida. The author has contributed to research in topics: Sediment & Climate change. The author has an hindex of 34, co-authored 76 publications receiving 4669 citations. Previous affiliations of Michael W. Binford include Stockholm University & Environmental Change Institute.

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Calculation and uncertainty analysis of 210Pb dates for PIRLA project lake sediment cores

TL;DR: In this article, first-order error analysis and Monte Carlo simulation (of cores from Florida PIRLA lakes) are used as independent estimates of dating uncertainty, and confidence intervals for 210Pb dates are calculated.
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An Exploratory Framework for the Empirical Measurement of Resilience

TL;DR: An exploratory framework is presented as a step towards the operationalization of resilience for empirical studies, which equate resilience with the ability of a system to maintain its identity, where system identity is defined as a property of key components and relationships and their continuity through space and time.
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Reconstruction of Caribbean climate change over the past 10,500 years

TL;DR: In this article, a high-resolution reconstruction of Caribbean climate is presented based on O-18/O-16 ratios in ostracod shells from Lake Miragoane, Haiti.
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Climate Variation and the Rise and Fall of an Andean Civilization

TL;DR: Paleolimnological and archaeological records that span 3500 years from Lake Titicaca and the surrounding Bolivian-Peruvian altiplano demonstrate that the emergence of agriculture and the collapse of the Tiwanaku civilization coincided with periods of abrupt, profound climate change as mentioned in this paper.
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A 350014C yr High-Resolution Record of Water-Level Changes in Lake Titicaca, Bolivia/Peru

TL;DR: In this paper, a transect of sediment cores collected from the southern basin of Lake Titicaca (Bolivia/Peru) was used to identify a new century-scale chronology of Holocene lake-level variations.