Minze Stuiver (October 25, 1929 – December 26, 2020) was a geochemist who was at the forefront of geoscience research from the 1960s until his retirement in 1998. He helped transform radiocarbon dating from a simple tool for archaeology and geology to a precise technique with applications in solar physics, oceanography, geochemistry, and carbon dynamics. Minze Stuiver's research encompassed the use of radiocarbon (14C) to understand solar cycles and radiocarbon production, ocean circulation, lake carbon dynamics and archaeology as well as the use of stable isotopes to document past climate changes.
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| - Minze Stuiver (de)
- Minze Stuiver (en)
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| - Minze Stuiver (* 25. Oktober 1929 in Vlagtwedde) ist ein niederländisch-US-amerikanischer Geochemiker. Er ist bekannt für Verbesserungen der Radiokarbonmethode. (de)
- Minze Stuiver (October 25, 1929 – December 26, 2020) was a geochemist who was at the forefront of geoscience research from the 1960s until his retirement in 1998. He helped transform radiocarbon dating from a simple tool for archaeology and geology to a precise technique with applications in solar physics, oceanography, geochemistry, and carbon dynamics. Minze Stuiver's research encompassed the use of radiocarbon (14C) to understand solar cycles and radiocarbon production, ocean circulation, lake carbon dynamics and archaeology as well as the use of stable isotopes to document past climate changes. (en)
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| - Minze Stuiver (* 25. Oktober 1929 in Vlagtwedde) ist ein niederländisch-US-amerikanischer Geochemiker. Er ist bekannt für Verbesserungen der Radiokarbonmethode. (de)
- Minze Stuiver (October 25, 1929 – December 26, 2020) was a geochemist who was at the forefront of geoscience research from the 1960s until his retirement in 1998. He helped transform radiocarbon dating from a simple tool for archaeology and geology to a precise technique with applications in solar physics, oceanography, geochemistry, and carbon dynamics. Minze Stuiver's research encompassed the use of radiocarbon (14C) to understand solar cycles and radiocarbon production, ocean circulation, lake carbon dynamics and archaeology as well as the use of stable isotopes to document past climate changes. (en)
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