David John Beerling FLSW (born 21 June 1965) is the Director of the Leverhulme Centre for Climate change mitigation and Sorby Professor of Natural Sciences in the Department of Animal and Plant Sciences (APS) at the University of Sheffield, UK. He is also Editor-in-Chief of the Royal Society journal Biology Letters.

Education

Beerling was educated at University of Wales, College of Cardiff where he was awarded a Bachelor of Science degree in Botany in 1987 followed by a PhD in 1990 for research into the biogeography, ecology and control of two important and highly invasive alien plant species Japanese knotweeed Reynoutria japonica and Himalayan balsam Impatiens glandulifera. His PhD was supervised by Ron Walter Edwards CBE and he authored two ecological monographs on the species and scientific papers reporting simulated projections of their potential future distributions in Europe with global climate change.

David Beerling

Research and career

Beerling's research group investigate fundamental questions concerning the conquest of the land by plants and the role of terrestrial ecosystems in shaping Earth's global ecology, climate and atmospheric composition. This is achieved by approaches that integrate evidence from fossils, experiments and theoretical models applied across spatial and temporal scales. Increasingly, his group's research discoveries are informing our understanding of current global climate change issues.

David Beerling

Earth's atmospheric CO₂ history

An important early success of his biophysical approach to palaeobotany was the discovery of evidence for a substantial increase in the atmospheric CO₂ concentration and 'super-greenhouse' conditions across the Triassic-Jurassic (Tr-J) boundary, 200 million years ago, based on analyses of fossil stomata and leaf morphology from Greenland. This causally linked a catastrophic extinction event with the break-up of Pangaea. Before his group's work, the Tr-J extinction represented one of the most poorly understood of the so-called 'big-five' mass extinctions in the Phanerozoic (past 540 million years). His paper resulted in major new international research programmes that subsequently identified evidence confirming the carbon cycle perturbation in marine and terrestrial sediments world-wide. He extended this discovery by evaluating hypothesized causal mechanisms with numerical geochemical carbon cycle modelling in collaboration with the Yale University geochemist Robert Berner.

David Beerling

Beerling was the only UK participant in an international consortium led by James Hansen (former Director of the Goddard Institute for Space Studies) analysing Cenozoic CO₂ and palaeoclimate evidence to investigate the broader societal question of the target CO₂ level required to avoid 'dangerous' anthropogenic interference of the climate system. Stabilization of human-made greenhouse gases in the atmosphere at a level avoiding this concern is a core objective of the United Nations Framework Convention on Climate Change. The resulting 2008 'Target CO₂' paper made the front page of the UK newspaper The Guardian which commented:

Fossils and experimental palaeobiology

Beerling is a leading architect in the field of experimental palaeobiology, adopting advanced experimental research programmes to address fundamental questions raised by the fossil record of plant life. Characterized by the formulation and evaluation of rigorous hypotheses, these programmes demonstrate how experimental evidence serves to deepen our causal understanding of past events. By productively collaborating with Jonathan Leake, his group established essential missing functional evidence supporting the long-standing conjecture, based largely on 400-million-year-old-fossils from the Devonian Rhynie chert, that the establishment of rootless early land plants in skeletal soils was promoted by their mutualistic symbiotic partnership with soil fungi. They went on to reveal how the simulated high CO₂ Palaeozoic atmosphere and arbuscular mycorrhizal fungi synergistically enhanced plant fitness to create uniquely strong selection pressures favouring the establishment of mycorrhiza-like partnerships in 'lower' land plants. These findings now place fungi as key players in the earliest symbiotic events during the greening of the Earth's land-masses.