Soft-bodied animals dominate the deepest parts of the deep sea

Publicly released:
Pacific; International
Credit:  Smartex Project/NERC
Credit: Smartex Project/NERC

International researchers have found that the number of animal species living near the bottom of the deep sea does not decrease with depth, upending expectations of Earth's most extensive and under-explored ecosystem. However, researchers observed a distinct shift in the types of animals observed around depths of 4.5km. Animals with shells were abundant above this transition boundary, while soft-bodied animals such as anemones, glass sponges and sea cucumbers dominated deeper zones. Authors of the study suggest that conditions below this transition boundary are unfavourable for the formation of animal shells. 

Media release

From: Springer Nature

Depth zones divide shelled and soft-bodied deep-sea creatures

A distinct transition zone, more than 4 km below the water’s surface, that divides deep sea organisms by body type is reported in a study in Nature Ecology & Evolution. Animals with shells were found to be abundant above the transition boundary, whereas soft-bodied animals dominated in the deep abyss.

The abyssal zone of the deep sea is the most extensive habitat on Earth, covering over 60% of the Earth’s surface, but also the least explored. It occurs between 3 and 6 km below the surface, where sunlight cannot penetrate, temperatures range between 0.5 and 3 °C, and organisms must be adapted to cope with extreme pressures. Although it is thought that there are fewer species in the deep ocean than in shallower ecosystems, it is unclear how biodiversity changes within the abyssal zone.

Erik Simon-Lledó and colleagues analyse data on the occurrence of more than 50,000 megafauna (animals larger than 10 mm) living near the seabed, collated from images taken from 12 deep-sea expeditions within the Clarion–Clipperton Zone — an area in the Pacific Ocean. The authors identify two distinct zones of deep-sea fauna: shallow abyssal communities at depths between 3.8 and 4.3km that are dominated by soft corals, brittle stars (a close relative of starfish) and shelled molluscs; and deep abyssal communities at depths between 4.8 and 5.3 km depth that are dominated by anemones, glass sponges and sea cucumbers. The intermediate transition zone between these zones consisted of a mixture of the two communities. Biodiversity was maintained across these boundaries, instead of decreasing with depth as is typically expected in the deep ocean. The authors suggest that this strong zonation in the abyss is likely to be driven by the carbonate compensation depth: the point at which calcium carbonate in seawater becomes undersaturated, and conditions for the formation of animal shells become unfavourable.

The authors argue that climate change and ocean acidification may alter this zonation, which, together with the effects of deep-sea mining, makes this a vulnerable ecosystem.

Multimedia

Examples of seabed species that inhabit the abyssal Pacific seafloor
Examples of seabed species that inhabit the abyssal Pacific seafloor
A 'mount-building' shrimp
A 'mount-building' shrimp
A likely undescribed species of crinoid
A likely undescribed species of crinoid
A glass sponge and an anemone
A glass sponge and an anemone
Plesiodiadema globulosum
Plesiodiadema globulosum
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Journal/
conference:
Nature Ecology & Evolution
Research:Paper
Organisation/s: National Oceanography Centre, Southampton, UK
Funder: This work was part of the UK Natural Environment Research Council funded Seabed Mining and resilience to Experimental impact (SMARTEX) project (grant reference NE/T003537/1). D.O.B.J., E.S.L., N.B., A.M.S., G.B.C. and A.G.G. also received support from TMC (The Metals Company) through its subsidiary Nauru Ocean Resources (NORI); this is contribution TMC/NORI/D/007. S.P.R. was supported by funds from FCT/MCTES in the scope of the CEEC contract (CEECIND/00758/2017) and funds attributed to CESAM (UIDP/50017/2020, UIDB/50017/2020 and LA/P/0094/2020). Samples from the BGR license area were made available by C. Rühlemann and A. Vink from the Federal Institute for Geosciences and Raw Materials (BGR) in Hannover. P.M.A. and K.U. acknowledge EU JPIO-Oceans project Ecological Aspects of Deep-Sea Mining and MinigImpact-2 (German Ministry for Science and Education BMBF contract 03F0707E and 03F0812E.). The KODOS and APEI-9 datasets had been collected through environmental baseline studies for the polymetallic manganese nodules exploration contract of Republic of Korea (Ministry of Ocean and Fisheries’ R&D no. 20160099). D.C. acknowledges funding from Mining2/0002/2017, Mining2/0005/2017, granted by FCT/MCTES and DGPM and OP AZORES 2020 (01-0145-FEDER-000140 ‘MarAZ Researchers: Consolidate a body of researchers in Marine Sciences in the Azores’ and funds attributed to Okeanos-UAç (UIDB/05634/2020, UIDP/05634/2020 and M1.1.A/ REEQ.CIENTIFICOU I&D/2021/010). The funders had no role in the conceptualization, design, data collection, analysis, decision to publish or preparation of the manuscript.
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