Conservation paleobiology has coalesced over the last two decades since its formal coining,
united by the goal of applying geohistorical records to inform the conservation …

Over the last 50 years, access to new data and analytical tools has expanded the study of
analytical paleobiology, contributing to innovative analyses of biodiversity dynamics over …

Climate change is expected to result in smaller fish size, but the influence of fishing has
made it difficult to substantiate the theorized link between size and ocean warming and …

The latitudinal diversity gradient (LDG) is a prevalent feature of modern ecosystems across
diverse clades,,–. Recognized for well over a century, the causal mechanisms for LDGs …

The geographic ranges of marine organisms, including planktonic foraminifera, diatoms,
dinoflagellates, copepods and fish, are shifting polewards owing to anthropogenic climate …

Hotspots of tropical marine biodiversity are areas that harbour disproportionately large
numbers of species compared to surrounding regions. The richness and location of these …

Planktonic foraminifera are a major constituent of ocean floor sediments, and thus have one
of the most complete fossil records of any organism. Expeditions to sample these sediments …

Aim Palaeoecological data are crucial for comprehending large‐scale biodiversity patterns
and the natural and anthropogenic drivers that influence them over time. Over the last …

Paleontologists generally use a low-cost electro-optical system to classify microfossils. This
manual identification is a time-consuming process and it may take about a long time …

Anthropogenic climate change is altering global biogeographical patterns. However, it
remains difficult to quantify how bioregions are changing because pre‐industrial records of …