The redox cycling of oxygen between O2, water, and intermediate redox states including hydrogen peroxide and superoxide, has profound impact on the availability and distribution of dissolved O2, the habitability of the marine biosphere, and cellular metabolic and physiological reactions that utilize O2. The sum total of processes that produce, consume, and exchange atoms with O2 in the atmosphere, oceans, and subsurface leave their isotopic fingerprints on the abundance of the three stable isotopes of O2 in the environment. In this thesis, I explore two aspects of the oxygen cycle in the past and present. First, I investigate the ability of manganese (Mn) oxide minerals to capture and retain the oxygen isotopic signature of dissolved O2 during the oxidation of aqueous Mn(II) to Mn-oxide minerals. I determine that approximately half of the oxygen atoms in Mn(III,IV) oxides I would like thank my committee, Colleen Hansel, Scott Wankel, and Kristin Bergmann for your academic guidance, feedback, and support in planning and executing my research. Thank you to Collin Ward for chairing my defense.Thanks to WHOI academic programs office for the many ways you've supported my work at WHOI and facilitated classes, research, and living between MIT and WHOI. Thank you to the wonderful team of admins in MC&G who have provided incredible help and assistance the last five years.Scott and Colleen, thank you for your mentorship, encouragement, and guidance in matters academic and otherwise over my time at WHOI. You have served as role models in and out of the lab, you gave me the freedom to pursue my own ideas, you have provided me with so many incredible research opportunities on land and at sea, and you have always been fierce advocates. Thank you for not giving up on me in year one when I almost destroyed both of your labs. Thank you for taking meetings at your dining room table and for blurring the lines between your lab children and your real children.