Watershed Cerebral Infarction
Watershed cerebral infarction is infarction in the border zones between major arterial territories, usually from reduced perfusion pressure or from microembolism. Cortical (external) border zones lie between the anterior, middle and posterior cerebral arteries, and internal border zones lie in the deep white matter, between deep and superficial middle cerebral branches.
It accounts for about 10% of ischaemic strokes. Common settings are severe carotid stenosis or occlusion, cardiac surgery, cardiac arrest, hypovolaemia and profound hypotension, and it also occurs with embolism.
Patterns. Anterior cortical (anterior to middle cerebral artery), posterior cortical (middle to posterior cerebral artery), internal (corona radiata and centrum semiovale) and, less often, cerebellar and spinal cord territories.
Mechanism. Haemodynamic and embolic mechanisms often coexist: reduced flow slows clearance of emboli from distal branches.
Pathophysiology.
Border zone regions sit at the end of arterial supply and have limited collateral flow, so a fall in perfusion pressure causes ischaemia first at these sites.
Impaired autoregulation in chronic carotid disease reduces tolerance to even brief hypotension.













