Smits, L. | bioRxiv Science

bioRxiv2025

Flow transports extracellular lipid-anchored proteins across the surface of living COS-7 cells

The rapid diffusion of membrane lipids and membrane proteins in living cell plasma membranes demonstrates that the membrane is fluid. However, motion of membrane molecules is inhibited on one side by the cytoskeletal mesh, and on the other by the glycocalyx, a layer of proteoglycans with long polysaccharide chains that covers the membrane surface. A variety of biological fluid flows (including blood circulation, cilia-driven flows, and swimming motion of microorganisms) apply shear stress to cell surfaces. Cell responses to these flows govern important physiological processes such as blood pressure and immune activation. The presence of the glycocalyx is generally thought to shield cell membranes from shear stress that arises from flow. However, here we show that two different proteins, each attached by a lipid anchor to the extracellular membrane surface of living COS-7 cells, formed reversible, cell-wide concentration gradients in the direction of applied flow. Protein redistribution occurred within minutes after we applied shear stress levels commonly found in animal cardiovascular systems. The dynamic and spatial features of these gradients were consistent with passive transport by flow. Passive flow transport could be a general mechanism for spatial organization of membrane proteins. This mechanism may explain protein patterning previously observed on flow-exposed cells, and potentially forms an initial step in flow sensing.

biophysics↗

bioRxiv2025

Long-term hunter-gatherer continuity in the Rhine-Meuse region was disrupted by local formation of expansive Bell Beaker groups

The first phase of the ancient DNA revolution painted a broad-brush picture of European Holocene prehistory, whereby 6500-4000 BCE, farmers descending from western Anatolians mixed with local hunter-gatherers resulting in 70-100% ancestry turnover, then 3000-2500 BCE people associated with the Corded Ware complex spread steppe ancestry into north-central Europe. We document an exception to this pattern in the wider Rhine-Meuse area in communities in the wetlands, riverine areas, and coastal areas of the western and central Netherlands, Belgium and western Germany, where we assembled genome-wide data for 109 people 8500-1700 BCE. Here, a distinctive population with high hunter-gatherer ancestry ([~]50%) persisted up to three thousand years later than in continental European regions, reflecting limited incorporation of females of Early European Farmer ancestry into local communities. In the western Netherlands, the arrival of the Corded Ware complex was also exceptional: lowland individuals from settlements adopting Corded Ware pottery had hardly any steppe ancestry, despite a characteristic early Corded Ware Y-chromosome. The limited influx may reflect the unique ecology of the regions river-dominated landscapes, which were not amenable to wholesale adoption of the early Neolithic type of farming introduced by Linearbandkeramik, making it possible for previously established groups to thrive, and creating a persistent but permeable boundary that allowed transfer of ideas and low-level gene flow. This changed with the formation-through-mixture of Bell Beaker using populations [~]2500 BCE by fusion of local Rhine-Meuse people (9-17%) and Corded Ware associated migrants of both sexes. Their expansion from the Rhine-Meuse region then had a disruptive impact across a much wider part of northwest Europe, including Britain where its arrival was the main source of a 90-100% replacement of local Neolithic peoples.

genomics↗