Are biologists getting the mathematical training they need in college?

Several major organizations have recommended revisions to mathematics requirements for biology majors. To determine whether these changes would benefit future biologists, we investigated mathematics use in research biology. We surveyed prominent journals in high and low math-use areas for articles referencing the use of quantitative methods. In addition, we conducted a large-scale survey of research biologists within these fields about their use of, and training in, mathematics and statistics. We then performed follow-up interviews with a purposeful sample of respondents. Our results indicate that biologists need a base in descriptive and inferential statistics and mathematical modeling, including some concepts from calculus, focused on conceptual understanding rather than computational accuracy, followed by differentiated programs of study in mathematics and statistics, depending on intended discipline within biology. Comparison of our findings with the recommended requirements from major stakeholder groups indicates some alignment but also some discrepancies. © 2018 International Union of Biochemistry and Molecular Biology, 46(6):612-618, 2018.

Frost for the trees: Did climate increase erosion in unglaciated landscapes during the late Pleistocene?

Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved problem in Earth science that is important for quantifying soil formation rates, sediment and solute fluxes to oceans, and atmospheric CO2 regulation by silicate weathering. Glaciated landscapes record the erosional legacy of glacial intervals through moraine deposits and U-shaped valleys, whereas more widespread unglaciated hillslopes and rivers lack obvious climate signatures, hampering mechanistic theory for how climate sets fluxes and form. Today, periglacial processes in high-elevation settings promote vigorous bedrock-to-regolith conversion and regolith transport, but the extent to which frost processes shaped vast swaths of low- to moderate-elevation terrain during past climate regimes is not well established. By combining a mechanistic frost weathering model with a regional Last Glacial Maximum (LGM) climate reconstruction derived from a paleo-Earth System Model, paleovegetation data, and a paleoerosion archive, we propose that frost-driven sediment production was pervasive during the LGM in our unglaciated Pacific Northwest study site, coincident with a 2.5 times increase in erosion relative to modern rates. Our findings provide a novel framework to quantify how climate modulates sediment production over glacial-interglacial cycles in mid-latitude unglaciated terrain.