In his 1706 treatise on the physical state of the sea, Italian polymath Luigi Ferdinando Marsigli investigated the persistent hydrodynamical puzzle of the Strait of Gibraltar: despite a continuous surface inflow of Atlantic water into the Mediterranean, the water level of the Mediterranean basin did not rise indefinitely. Prevailing hypotheses attributed this equilibrium almost exclusively to atmospheric evaporation. Marsigli, however, postulated an opposing deep countercurrent returning water to the Atlantic. To test this, he constructed a dual-compartment tank divided by a partition, filling one side with dense, highly saline water to simulate the Mediterranean and the other with less dense water to simulate the Atlantic. Opening apertures at both top and bottom revealed a two-way circulation: lighter water moved surface-wise toward the denser side, while denser water flowed along the bottom in the opposite direction. Although Marsigli argued that density differentials caused by salinity and temperature drove submarine currents, his contemporaries broadly rejected his countercurrent hypothesis. This resistance arose largely because seventeenth- and early eighteenth-century natural philosophers viewed the abyssal ocean as a quiescent, homogenous realm, isolated from the thermal and saline variations that affected surface waters.
It can be inferred from the passage that many natural philosophers in the early eighteenth century rejected Marsigli's countercurrent hypothesis because they
- Aassumed that laboratory scale models were fundamentally incapable of replicating the hydrodynamic behaviors of natural maritime bodies
- held a conception of deep ocean environments that was incompatible with the mechanism of density-driven submarine circulationAnswer
- Cbelieved that atmospheric evaporation was entirely insufficient to maintain the water level equilibrium of the Mediterranean Sea
- Dmaintained that surface winds were the sole mechanism regulating fluid dynamics across all major maritime straits
- Evehemently denied that salinity and temperature could influence fluid density under any circumstances