Evidence that involucrin, a marker for differentiation, is oxygen regulated in human squamous cell carcinomas

Hypoxia is associated with poor prognosis in squamous cell carcinomas affecting both local control and distant spread (Hockel et al., 1996a, 1996b, 1999; Nordsmark et al, 1996; Fyles et al, 2002; Kaanders et al, 2002). Local control is believed to depend on local radiation response while distant spread is thought to depend, at least in part, on the induction of oxygen-regulated proteins. In order to test this, pimonidazole, an extrinsic marker for tissue hypoxia (Arteel et al, 1995; Kennedy et al, 1997; Varia et al, 1998; Raleigh et al, 1999), with prognostic value (Kaanders et al, 2002) was used to examine whether ORPs such as VEGF (Raleigh et al, 1998a), metallothionein (Raleigh et al, 2000), HIF-1α (Janssen et al, 2002), Glut-1 (Airley et al, 2003) and CAIX (Olive et al, 2001) were, in fact, associated with cellular hypoxia in human tumours. Unexpectedly, VEGF and metallothionein (MT) were not expressed in the majority of hypoxic cells in squamous cell carcinomas (Raleigh et al, 1998a, 2000) even though these ORPs were induced by hypoxia in experimental systems (Shweiki et al, 1992; Raleigh et al, 1998b; Murphy et al, 1999)

Trends and connections across the Antarctic cryosphere

Satellite observations have transformed our understanding of the Antarctic cryosphere. The continent holds the vast majority of Earth’s fresh water, and blankets swathes of the Southern Hemisphere in ice. Reductions in the thickness and extent of floating ice shelves have disturbed inland ice, triggering retreat, acceleration and drawdown of marine-terminating glaciers. The waxing and waning of Antarctic sea ice is one of Earth’s greatest seasonal habitat changes, and although the maximum extent of the sea ice has increased modestly since the 1970s, inter-annual variability is high, and there is evidence of longer-term decline in its extent