MAG LAB Slotznick Research Group Department of Earth Sciences
Home
People Research Publications Facilities Teaching Contact

Iron is the most abundant transition metal in the Earth's crust; as such, it is a key player in the planetary redox budget and is utilized by nearly all life.  Iron is present in a diverse suite of minerals and is the crucial component in magnetic minerals such as natural "permanent" magnets.  Our group uses iron minerals to understand the (co)evolution of Earth’s surface environments and life as well as the fidelity of the rock record in preserving ancient bio- and environmental signatures.

 © 2024 by Sarah Slotznick
MAG LAB Slotznick Research Group Department of Earth Sciences
Home
MAG LAB Slotznick Research Group Department of Earth Sciences
Home
MAG LAB Slotznick Research Group Department of Earth Sciences
Home
MAG LAB Slotznick Research Group Department of Earth Sciences
Home
 © 2024 by Sarah Slotznick
MAG LAB Slotznick Research Group Department of Earth Sciences
  • Menu
    HomePeopleResearchPublicationsFacilitiesTeachingContact
 © 2024 by Sarah Slotznick
MAG LAB Slotznick Research Group Department of Earth Sciences
  • Menu
    Home
 Slotznick Research Group Department of Earth Sciences MAG LAB
  • Menu
    HomePeopleResearchPublicationsFacilitiesTeachingContact
Iron is the most abundant transition metal in the Earth's crust; as such, it is a key player in the planetary redox budget and is utilized by nearly all life. Iron is present in a diverse suite of minerals and is the crucial component in magnetic minerals such as natural "permanent" magnets. Our group uses iron minerals to understand the (co)evolution of Earth’s surface environments and life as well as the fidelity of the rock record in preserving ancient bio- and environmental signatures.
 Slotznick Research Group Department of Earth Sciences MAG LAB
  • Menu
    Home
Iron is the most abundant transition metal in the Earth's crust; as such, it is a key player in the planetary redox budget and is utilized by nearly all life. Iron is present in a diverse suite of minerals and is the crucial component in magnetic minerals such as natural "permanent" magnets. Our group uses iron minerals to understand the (co)evolution of Earth’s surface environments and life as well as the fidelity of the rock record in preserving ancient bio- and environmental signatures.