A deep-sea necropolis of whale remains was mapped across roughly 1,200 km of the Diamantina Zone (4,616-7,001 m depth) through 32 submersible dives, yielding 485 whale-fossil sites that include five active whale falls and 476 fossil cetaceans. Isotopic dating places whale-fall occurrence in this region back at least 5.3 million years. Fossils comprise five beaked-whale species plus one baleen whale, and one of the largest modern carcasses was identified as an Antarctic minke whale by earbone morphology and a near-complete mitochondrial genome. The deepest active whale fall was recorded at 6,789 m, extending known depth limits for such ecosystems well into the abyssal-hadal transition.
Carcasses support specialized, high-density assemblages dominated by brittle stars, bone-boring Osedax worms, chemosymbiotic bivalves (including Abyssogena southwardae and other taxa hosting sulfur-oxidizing symbionts), gastropods and polychaetes, with local megafaunal densities up to 2,840 individuals m-2. Many recovered species appear new to science; molecular barcodes were obtained for 21 taxa but only one matched known records. Novel observations include sea daisies (Xyloplax) at unprecedented depths and unique brittle-star assemblages confined to bone substrates. These findings extend the biogeographic and evolutionary significance of whale-fall ecosystems and establish certain deep-sea floors as long-term fossil archives for tracing cetacean evolution.
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