Passage:
During the 1872–1876 oceanographic expedition of HMS Challenger, directed by Scottish naturalist Charles Wyville Thomson, researchers conducted the first systematic global survey of deep-sea abyssal environments. Prior to the voyage, prevailing oceanic theory—most notably Edward Forbes's "azoic hypothesis" formulated in 1843—asserted that marine life could not exist below a depth of 300 fathoms (1,800 feet) due to extreme hydrostatic pressure and total darkness. However, Thomson's team collected biological specimens from depths exceeding 3,000 fathoms using reinforced dredges. Despite these groundbreaking findings, Thomson maintained that deep-sea organisms were not primitive relicts of ancient geological eras, as some evolutionary biologists speculated, but were instead specialized descendants of shallow-water species that had migrated downward over time. Crucially, the expedition also documented that deep-water temperatures remained uniformly cold across disparate oceanic basins regardless of surface latitude, disproving the earlier assumption that tropical seabed waters were warmed by equatorial solar radiation.
According to the passage, Charles Wyville Thomson held which of the following views regarding the origin of deep-sea organisms?
- AThey were primitive biological relicts preserved from ancient geological epochs.
- BThey originated in tropical seabed waters before gradually spreading to polar basins.
- They were specialized descendants of shallow-water species that had migrated into deeper oceanic environments over time.Cevap
- DThey evolved exclusively at depths above the 300-fathom threshold postulated by Edward Forbes.
- EThey developed thermal adaptation mechanisms to withstand elevated temperatures near equatorial ocean floors.