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Biology subjects

Drucker, D. G.

Publications and source records attributed to Drucker, D. G..

3 recordsLinked to original sources

Ancient biomolecules suggest learned foraging strategy in extinct cave bears

Studying the behavioural ecology of long-extinct species is challenging due to the difficulty in measuring the behavioural phenotype and correlating this with genetic and environmental factors. However, a multidisciplinary approach integrating isotope analysis of diet and ancient DNA analysis of genetic relationships offers a potential framework to test the proximate causes of dietary preferences. Our study focuses on Late Pleistocene cave bears from the Romanian Carpathians. Stable isotope analysis of bone collagen reveals substantial lifetime variation in food plant preferences among individuals. We find that bears with similar diets do not cluster according to their population structure, sex, time period, climatic conditions, or location. This disconnect suggests that diet preference in cave bears is not genetically inherited, and instead that individuals adapted their diets based on foraging experience. This integrative approach opens new avenues for understanding Pleistocene animal behaviour, leveraging ancient biomolecules synergistically to reveal insights otherwise inaccessible.

evolutionary biology↗

Trophic adaptation of large terrestrial omnivores to global change

Large omnivores at the top of food webs play a key role in ecosystems, as their ability to feed on multiple trophic levels stabilizes food-web dynamics and impacts ecosystem functioning. However, it is largely unexplored how large omnivores adapt their trophic interactions to altered resource availability under global change, particularly in terrestrial ecosystems. Here, we combine macroecological and paleoecological approaches and reveal that extant bears, the largest terrestrial omnivores, adapt their trophic position in food webs dynamically to net primary productivity and growing season length. Throughout their geographic ranges, extant bears occupy higher trophic positions in unproductive ecosystems with short growing seasons than in productive ecosystems with long growing seasons. Consistent with this geographic pattern, the trophic position of the brown bear sharply decreased at the transition from the Late Pleistocene to the Holocene, coinciding with an increase in net primary productivity and growing season length. These findings demonstrate that trophic interactions of omnivores are not static but change dynamically in response to environmental change. Our findings suggest that global change impacts on primary production and vegetation seasonality may trigger shifts in the functional role of omnivores, with consequences for food webs and ecosystem functions. Significance statementLarge omnivores play a key role in ecosystems, as they stabilize food-web dynamics and impact ecosystem functioning. However, how omnivores adapt their trophic interactions to changes in resource availability under global change remains unexplored. Combining macroecological and paleoecological approaches, we show that extant bears, the largest terrestrial omnivores, occupy lower trophic positions in food webs as net primary productivity and growing season length increase. This trophic adaptation is evident across the geographic ranges of all extant terrestrial bear species and for brown bears at the transition from the Late Pleistocene to the Holocene. Therefore, impacts of global change on primary production and vegetation seasonality may trigger shifts in the functional role of omnivores, with consequences for food webs and ecosystems. One sentence summaryGlobal changes in primary productivity and vegetation seasonality alter the functional role of large omnivores in terrestrial ecosystems.

ecology↗

Out of Africa by spontaneous migration waves

Hominin evolution is characterized by progressive regional differentiation, as well as migration waves, leading to anatomically modern humans that are assumed to have emerged in Africa and spread over the whole world. Why or whether Africa was the source region of modern humans and what caused their spread remains subject of ongoing debate. We present a spatially explicit, stochastic numerical model that includes ongoing mutations, demic diffusion, assortative mating and migration waves. Diffusion and assortative mating alone result in a structured population with relatively homogeneous regions bound by sharp clines. The addition of migration waves results in a power-law distribution of wave areas: for every large wave, many more small waves are expected to occur. This suggests that one or more out-of-Africa migrations would probably have been accompanied by numerous smaller migration waves across the world. The migration waves are considered \"spontaneous\", as the current model excludes environmental or other factors. Large waves preferentially emanate from the central areas of large, compact inhabited areas. During the Pleistocene, Africa was the largest such area most of the time, making Africa the statistically most likely origin of anatomically modern humans, without a need to invoke additional environmental or ecological drivers.

evolutionary biology↗