Detrital zircon–apatite fingerprinting challenges glacial transport of Stonehenge’s megaliths

Salisbury Plain detrital zircon ages align with southern British rocks from the London Basin, indicating local sedimentary recycling without glaciogenic evidence, negating glacial transport of the Stonehenge blocks, according to detrital zircon and apatite U-Pb isotopic fingerprinting of stream sediments across the Salisbury Plain.