Site 1121 is located southeast of New Zealand on the Campbell Drift (50°53.876'S 176°59.862'E) at a water depth of 4487.90 meters below sea level (mbsl). The site was drilled to recover an expanded se
Our recent research revealed noticeable degenerative change in calcified concrements and soft tissue of human pineal gland (PG) with neuropathology. However, the genesis and dynamics of PG concremen
Association between individual and household-level characteristics and evidence of brain calcifications on non-contrast computerized tomography of the head.
