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Whale Fall Ecosystem: 15 Years of Sulphophilic Community Persistence Observed

High-resolution seafloor photogrammetry reveals the long-term persistence of a sulphophilic community on a whale fall in the NE Pacific, highlighting its significance as a biodiversity hotspot.

3 min readFrontiers in Marine Science | New and Recent Articles
Whale Fall Ecosystem: 15 Years of Sulphophilic Community Persistence Observed

The recent observation of a whale fall ecosystem on the Clayoquot Slope, spanning a remarkable 15-year period, provides critical empirical data on the persistence of deep-sea communities. Our validated, time-series analysis, leveraging ROV surveys and high-resolution 3D photogrammetry, offers a precise measurement of ecosystem dynamics in a challenging environment. The skeletal remains, comprising skull bones and caudal vertebrae, exhibited minimal structural degradation over the study duration, with quantifiable metrics showing only slight decreases in length. This stability is fundamental to understanding the long-term viability of these unique habitats.

Crucially, our findings demonstrate a significant and measurable increase in bacterial mat coverage on the skeletal structure, a direct indicator of an expanding sulphophilic stage. This expansion, coupled with the sustained presence of characteristic chemosynthetic fauna such as vestimentiferan tube worms and vesicomyid clams, solidifies the observation of a prolonged sulphophilic phase. The absence of previously documented bone-eating Osedax worms in the later survey, while bone-eating worms were present in 2009, suggests a transition beyond the initial enrichment opportunist phase and further supports the extended duration of the sulphophilic community. This integrated data ecosystem approach allows us to track complex ecological shifts with scientific integrity.

The implications of this sustained sulphophilic stage are far-reaching, particularly in the context of expanding Oxygen Minimum Zones (OMZs) driven by climate change. The Clayoquot Slope whale fall, situated at the edge of an OMZ, highlights the resilience of these ecosystems under lower oxygen conditions. The persistent presence of lipid-rich bone structures and the growth of chemosynthetic communities suggest that whale falls can serve as vital stepping stones for deep-sea biodiversity for decades, even in increasingly challenging oceanic environments. Understanding these long-term processes is essential for effective ocean stewardship and for predicting the impact of environmental changes on these biodiverse hotspots.

From Frontiers in Marine Science | New and Recent Articles

Deep-sea whale falls serve as biodiversity hotspots and pass through distinct successional stages, with the duration of the sulphophilic stage remaining controversial. We conducted a 15-year time-series study of a blue or fin whale skeleton on the edge of the Oxygen Minimum Zone at 1288 m depth on the Clayoquot Slope, Cascadia Continental Margin, using ROV surveys and high-resolution 3D photogrammetry to assess long-term ecosystem changes. The skeleton, consisting of skull bones and 23 caudal vertebrae, showed minimal structural degradation, based on 3D models from 2012 and 2023, with vertebrae decreasing in length by only 1.4% and mandibles showing the…

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