Diversification of Iron-Biomineralizing Organisms During the Paleocene-Eocene Thermal Maximum: Evidence From Quantitative Unmixing of Magnetic Signatures of Conventional and Giant Magnetofossils

Diversification of Iron-Biomineralizing Organisms During the Paleocene-Eocene Thermal Maximum: Evidence From Quantitative Unmixing of Magnetic Signatures of Conventional and Giant MagnetofossilsDOI: info:10.1029/2021PA004225v. 36No. 5American Geophysical Union
Wagner, Courtney L., Lascu, Ioan, Lippert, Peter C., Egli, Ramon, Livi, Kenneth J. T., and Sears, Helen B. 2021. "Diversification of Iron-Biomineralizing Organisms During the Paleocene-Eocene Thermal Maximum: Evidence From Quantitative Unmixing of Magnetic Signatures of Conventional and Giant Magnetofossils." Paleoceanography and Paleoclimatology, 36, (5). https://doi.org/10.1029/2021PA004225.
ID: 160946
Type: article
Keywords: NMNH; NH-Mineral Sciences