Factors influencing underrepresented geoscientists' decisions to accept or decline faculty job offers.

Many geoscience departments are taking steps to recruit and retain faculty from underrepresented groups. Here we interview 19 geoscientists who identify as an underrepresented race or gender who recently declined a tenure-track faculty job offer. A range of key factors influenced their decisions to accept or decline a position including commitment to diversity, equity, and inclusion (DEI) including personal identities, DEI initiatives, and mentorship; (in)civility during job interviews; values revealed in negotiation; and compatibility with personal life including family and geography. Many of the participants experienced hiring processes inconsistent with existing recommendations to increase faculty diversity. Therefore, we leverage our results to provide actionable recommendations for improving the equity and effectiveness of faculty recruitment efforts. We find that departments may doubly benefit from improving their culture: in addition to benefiting current members of the department, it may also help with recruitment.

Cold seep formation from salt diapir-controlled deep biosphere oases.

Deep sea cold seeps are sites where hydrogen sulfide, methane, and other hydrocarbon-rich fluids vent from the ocean floor. They are an important component of Earth's carbon cycle in which subsurface hydrocarbons form the energy source for highly diverse benthic micro- and macro-fauna in what is otherwise vast and spartan sea scape. Passive continental margin cold seeps are typically attributed to the migration of hydrocarbons generated from deeply buried source rocks. Many of these seeps occur over salt tectonic provinces, where the movement of salt generates complex fault systems that can enable fluid migration or create seals and traps associated with reservoir formation. The elevated advective heat transport of the salt also produces a chimney effect directly over these structures. Here, we provide geophysical and geochemical evidence that the salt chimney effect in conjunction with diapiric faulting drives a subsurface groundwater circulation system that brings dissolved inorganic carbon, nutrient-rich deep basinal fluids, and potentially overlying seawater onto the crests of deeply buried salt diapirs. The mobilized fluids fuel methanogenic archaea locally enhancing the deep biosphere. The resulting elevated biogenic methane production, alongside the upward heat-driven fluid transport, represents a previously unrecognized mechanism of cold seep formation and regulation.

Carbon and nitrogen isotope variability in the seeds of two African millet species: Pennisetum glaucum and Eleusine coracana.

RATIONALE: A range of important small seeded C4 crops were domesticated in Africa, but little is known about their carbon and nitrogen isotope ratios (δ13 C and δ15 N values). Understanding natural isotopic variability within and among millets has the potential to help us to understand the conditions under which ancient cereals were grown and has significant implications for the interpretation of ancient diets based on stable isotope signatures. METHODS: We conducted carbon and nitrogen isotope analyses of modern and historical pearl millet (Pennisetum glaucum, n = 108) and finger millet (Eleusine coracana, n = 17) seed samples sourced from the United States Department of Agriculture as well as the Harlan Collection curated at the Crop Evolution Laboratory Herbarium at the University of Illinois. RESULTS: The millet species have significantly different mean carbon and nitrogen isotope ratios over broad temporal and spatial scales. We also found substantial isotopic variation within species (range of 1.9‰ and 8.5‰ in δ13 C and δ15 N values, respectively). Both water availability and growing season temperature significantly affected the P. glaucum δ13 C and δ15 N values; cumulative annual precipitation was positively correlated with both seed δ13 C and δ15 N values, while temperature was positively correlated with δ15 N values but negatively correlated with seed δ13 C values. CONCLUSIONS: The importance of both temperature and precipitation as predictors of δ13 C and δ15 N values in millets suggests that C4 plants may be more sensitive to environmental parameters than previously appreciated. Given the high degree of carbon and nitrogen isotope variability among accessions of these species, it is imperative that site-relevant plant isotope ratios are used for making isotope-based paleo-dietary predictions.