When OpenStreetMap put a slippy map on its front page on its front page in 2005 it used a Mercator map. This made excellent sense at the time: true north was at the top everywhere, angles were good (spherical Mercator less so than geoidal Mercator) and the raster tiles at then in use could be scrolled without spending computational power on changing their shape. Other maps at the time made the same decision for the same reasons.
Twenty years on desktop and even mobile processors can render vector tiles with consummate ease, keeping the labels in the right shape while they do so. The need to keep tiles the same shape has evaporated and many maps can be spun to put whichever direction the user wants at the top. But the disadvantages of Mercator remain: at small scales Canada and Greenland are exaggerated in size compared to Africa. At large scales this is more subtle, each zoom level maps Helsinki at a linear scale twice as large as Bogota with four times the area and shifting a zoom level doesn’t mix well with map styles that use the level to show differing amounts of detail. There is more than a further zoom level of difference between Helsinki and Longyearbyen. The widest used scheme for tile URLs leaves a hole 1000km across around each pole; this was tolerated because the is no land in the Arctic hole and, as any Australian will tell you, the southern hemisphere doesn’t count.