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Dallas Abbott

American research scientist From Wikipedia, the free encyclopedia

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Dallas Abbott is a geophysicist and adjunct research scientist at the Lamont–Doherty Earth Observatory of Columbia University and is part of the Holocene Impact Working Group. [1] Her research focuses on submarine impacts, megatsunamis, cosmic dust, and their effects on climate and Earth's geological history.[2] She also has presented research regarding a large impact crater in the Gulf of Maine.[3]

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Education and career

Abbott received her B.S. from the Massachusetts Institute of Technology (Earth and Planetary Sciences) in 1974; her M.S. from the Lamont–Doherty Earth Observatory of Columbia University (Marine Geology) in 1978; and her Ph.D. from the Lamont–Doherty Earth Observatory (Marine Geology with a Geophysics minor) in 1982.[4] During her graduate studies, she received the Boris Bakmeteff Fellowship in Fluid Mechanics and the Bruce Heezen Prize.[4]

She held academic positions at Oregon State University and Barnard College. Also, she has been an adjunct research scientist at LDEO of Columbia University since 1996.[5] Since 1990, Abbott has directed or co-directed LDEO's summer undergraduate internship program, which trains students in scientific research methods, technical writing, and data analysis. [6]

She previously served on the editorial board of Precambrian Research and was named a Graduate Fellow of Columbia University.[7]

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Research

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In 1994, Abbott and colleagues published the first empirical thermal history of Earth's mantle.[8] Prior to their work, most discussions of mantle evolution relied on theoretical models or assumed that Archean komatiites represented the average Archean mantle rather than isolated hotspot regions.[9]

Her research in submarine geology has shown that volcanic arcs contain significantly more active underwater volcanoes than previously recorded in standard databases, as documented in a 2024 study.[10] Abbott has also investigated potential links between submarine impacts and megatsunamis, including dating deposits in southern Madagascar that may have originated from submarine landslides or extraterrestrial impacts.[5] Abbott has studied cosmic dust deposition in Earth’s geological record, identifying tin-rich particles in ice cores and discovering tin-coated pelagic foraminifera in Hudson River sediments—the first documented case of such marine microfossils. [1]This finding was later confirmed in diatoms by her student, Jiahua Wu (2024).[11]

In the field of Precambrian geology, Abbott documented 2.0 billion-year-old native iron in the Chaibasa Formation of India,[12] later interpreted by other researchers as resulting from a meteorite impact.[13] Her work also explored correlations between mantle plume activity and the timing of large impact events during the Precambrian.[14]

Her tectonic research proposed the concept of buoyant subduction around 2.4 billion years ago, which may account for differences in the formation of Archean continental crust.[9]

In climate research, Abbott has examined the 536 AD climate anomaly, attributing its severity to a combination of volcanic activity and cosmic dust deposition.[15]

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Selected publications

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See also

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