In 1868, biologist Thomas Henry Huxley examined seafloor mud retrieved from the North Atlantic telegraph cable surveys and identified a gelatinous, structureless substance embedded with microscopic calcareous disks (coccoliths). Huxley posited that this matrix was an expansive layer of continuous, primordial living protoplasm carpeting the abyssal ocean floor, naming it Bathybius haeckelii in homage to Ernst Haeckel’s evolutionary theories of abiogenesis. Because Bathybius appeared to bridge the divide between non-living inorganic matter and organized cellular life, it was rapidly assimilated into contemporary evolutionary paradigms as empirical vindication of a universal organic substrate. However, during the 1872–1876 Challenger expedition, naturalists sought to observe Bathybius in freshly hauled abyssal dredgings but consistently failed to detect the gelatinous matrix in fresh seawater. Only after chemist John Young Buchanan added alcohol to store and preserve the specimens did a dense, precipitate-like slime materialize. Subsequent chemical assays demonstrated that the purported organism was merely an inorganic precipitate of hydrated calcium sulfate, formed when the preserving alcohol reacted with seawater sulfates in the presence of sediment. Huxley openly retracted his biological characterization in 1879, acknowledging that the initial observations were artifacts of preservation chemistry rather than evidence of abyssal protoplasm.
Based on the passage, which of the following assertions regarding the scientific investigation of Bathybius haeckelii are logically supported by the text? (Select all that apply.)
- Initial scientific acceptance of Bathybius was facilitated in part by its alignment with prevailing theoretical frameworks concerning the origins of living organisms.Cevap
- BThe naturalists aboard the Challenger expedition concluded that deep-sea hydrostatic pressure was essential to maintain the structural integrity of Bathybius protoplasm in its native habitat.
- The physical presence of the gelatinous substance in the 1868 seafloor specimens depended upon the addition of a chemical preserving agent to the seawater-sediment mixture.Cevap
- DHuxley’s 1879 retraction was motivated primarily by contemporary discoveries demonstrating that coccoliths originated exclusively from photosynthetic surface algae rather than abyssal organisms.
- EThe Challenger researchers successfully isolated living cellular organisms from the sediment once the inorganic calcium sulfate precipitate was dissolved.