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Dallas Abbott

From Wikipedia, the free encyclopedia

Dallas Abbott (born 1963)[1] 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.[2] Her research focuses on submarine impacts, megatsunamis, cosmic dust, and their effects on climate and Earth's geological history.[3] She also has presented research regarding a large impact crater in the Gulf of Maine.[4]

Education and career

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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.[5] During her graduate studies, she received the Boris Bakmeteff Fellowship in Fluid Mechanics and the Bruce Heezen Prize.[5]

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.[6] 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.[7]

She previously served on the editorial board of Precambrian Research and was named a Graduate Fellow of Columbia University.[8]

Research

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In 1994, Abbott and colleagues published the first empirical thermal history of Earth's mantle.[9] 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.[10]

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.[11] 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.[6] 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.[2] This finding was later confirmed in diatoms by her student, Jiahua Wu (2024).[12]

In the field of Precambrian geology, Abbott documented 2.0 billion-year-old native iron in the Chaibasa Formation of India,[13] later interpreted by other researchers as resulting from a meteorite impact.[14] Her work also explored correlations between mantle plume activity and the timing of large impact events during the Precambrian.[15]

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.[10]

In climate research, Abbott has examined the 536 AD climate anomaly, attributing its severity to a combination of volcanic activity and cosmic dust deposition.[16]

Selected publications

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See also

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References

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  1. ↑ "Marine & Polar Geophysics Division | Lamont-Doherty Earth Observatory". lamont.columbia.edu. Retrieved 2026-02-18.
  2. 1 2 Blakeslee, Sandra (November 14, 2006), "Ancient Crash, Epic Wave", The New York Times
  3. ↑ Easterbrook, Gregg. "The Sky Is Falling". The Atlantic. Retrieved 2017-11-06.
  4. ↑ Geological Society of America – Joint Meeting of Atlantic Geoscience Society and GSA NE Section – Press Release Archived 2007-07-11 at the Wayback Machine
  5. 1 2 "VITA". www.ldeo.columbia.edu. Retrieved 2017-11-06.
  6. 1 2 Chang, Kenneth (2008-12-30). "Meteorite Strikes, Setting Off a Tsunami: Did It Happen Here?". The New York Times. ISSN 0362-4331. Retrieved 2025-05-27.
  7. ↑ ""New Revelations about Impact Craters" with Dallas Abbott (May 2005)". earth2class.org. Retrieved 2025-05-28.
  8. ↑ "Friday seminars of Institute of Earth Sciences and Nordic Volcanological Center 31 March - Dallas Abbott | Institute of Earth Sciences". earthice.hi.is. Retrieved 2025-05-28.
  9. ↑ Abbott, Dallas; Burgess, Lee; Longhi, John; Smith, Walter H. F. (1994). "An empirical thermal history of the Earth's upper mantle". Journal of Geophysical Research: Solid Earth. 99 (B7): 13835–13850. doi:10.1029/94JB00112. hdl:11380/458250. ISSN 2156-2202.
  10. 1 2 Smithies, R. H.; Champion, D. C.; Cassidy, K. F. (2003-11-10). "Formation of Earth's early Archaean continental crust". Precambrian Research. Archaean Tectonics, Volume 1. 127 (1): 89–101. doi:10.1016/S0301-9268(03)00182-7. ISSN 0301-9268.
  11. ↑ Abbott, Dallas; Rubenstone, James L. (2024-07-22). "The abundance of submarine volcanism in arcs". Volcanica. 7 (2): 447–459. doi:10.30909/vol.07.02.447459. ISSN 2610-3540.
  12. ↑ Martinez, Vanessa; Cruz, Natasha M.; Wu, Jiahua (2024). "Increased Biological Productivity and Appearance of Black Foraminifera Due to Large Eruptions in the Past 150,000 Years in Low-Latitude". American Geophysical Union, Ocean Sciences Meeting (882): OB34C–0882.
  13. ↑ Abbott, Dallas H.; Mazumder, Rajat; Breger, Dee (2012). "Native iron in the Palaeoproterozoic Chaibasa Formation: primary or secondary?". Geological Society, London, Special Publications. 365 (1): 77–90. doi:10.1144/SP365.5. ISSN 0305-8719.
  14. ↑ Ravillous, Kate. "Earth's volcanism linked to meteorite impacts". New Scientist. Retrieved 2025-05-28.
  15. ↑ Abbott, Dallas H; Isley, Ann E (2002). "Extraterrestrial influences on mantle plume activity". Earth and Planetary Science Letters. 205 (1–2): 53–62. doi:10.1016/S0012-821X(02)01013-0.
  16. ↑ Fecht, Sarah. "Undersea Volcanism May Help Explain Medieval Year of Darkness | Lamont-Doherty Earth Observatory". lamont.columbia.edu. Retrieved 2025-05-28.