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How do we apply this?

Despite the clear lack of taxonomic preservation during the Ediacaran (~550 million years ago, when multicellular life started to evolve and diversify), we can use this methodology to see whether early life was complex or structured similarly.
Life Modes in the Ediacaran (We're getting technical!)
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Erect, non-motile (stromatolitic vertical suspension feeder). Raised above the mat to intercept flow; passive/active suspension feeding; firmly attached to the mat or firmground. Shows early vertical tiering and exploitation of pelagic particulates (Conway Morris, 2006).
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Erect, attached sponge-type filter feeder. Sessile, rigid or semi-rigid body using porous/filter structures to remove particles from water; anchored to seafloor or mat. Exemplifies early metazoan filter-feeding architecture (Conway Morris, 2006).
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Surficial, unattached mat-surface suspension interceptor. Lies on the mat and captures particles at or just above the surface (e.g. mucus or surface structures). Highlights alternative particle-capture strategies tightly coupled to matgrounds (Narbonne, 2005).
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Surficial, slow-moving surface-deposit feeder (e.g. Yorgia). Moves across mats consuming mat biomass (external digestion or surface deposit feeding) and leaves characteristic traces; prostrate, non-attached mobility. Evidence for active exploitation of mat resources and simple motility (Buatois and M. Gabriela Mángano, 2016).
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Surficial, grazing mobile consumer (e.g. Kimberella). Directed grazing or rasping of mats/biofilms, producing scratches and feeding traces; close contact with substrate and purposeful movement. Early sign of complex consumer behaviour within mat ecosystems (Buatois and M. Gabriela Mángano, 2016).
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Surficial, facultatively mobile opportunist (e.g. Spriggina). Episodic movement with variable feeding (deposit/opportunistic); usually prostrate but able to detach and relocate. Demonstrates behavioural flexibility and steps toward sustained motility (Buatois and M. Gabriela Mángano, 2016).
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Surficial, broad prostrate mat-feeder (e.g. Dickinsonia). Mostly non-motile but capable of short moves (Buatois and M. Gabriela Mángano, 2016); feeds by mat grazing or external digestion, leaving diagnostic traces; adhesive contact with mats. Key example of large mat-feeding strategy and organized consumer morphology (RETALLACK, 2025).
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Surficial, attached holdfast form (e.g. Aspidella). Sessile anchoring structures for erect elements; associated fronds passively suspend/absorb resources. Indicates modular community architecture and anchored tiering (Conway Morris, 2006).
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Semi-infaunal, shallow deposit-feeding trace producers. Shallow under-mat movement or burrowing recorded by simple horizontal traces; exploited mat–sediment interface. Earliest evidence of under-mat sediment exploitation and incipient infaunal behaviour (Narbonne, 2005).
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Semi-infaunal, partly embedded fractal body (e.g. Rangea). Minimally motile, partly sub-mat organisms that likely absorbed pore-water nutrients or trapped particles; semi-infaunal positioning. Represents 3-D bodyplan experimentation and novel substrate interactions, though function is uncertain (Bambach et al., 2007).
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Shallow infaunal mining trace producers. Active probing miners that made vertical/horizontal probing burrows to mine organic layers beneath mats. Marks the beginning of sediment reworking and the agronomic transition toward deeper bioturbation (Narbonne, 2005).
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Shallow infaunal, small-bodied occupants (e.g. Intrites). Tiny infaunal inhabitants (casts/impressions) probably feeding on detritus or mat-associated material within very shallow sediments. Documents limited early infaunal occupation prior to widespread Phanerozoic bioturbation; details remain fragmentary (Bambach et al., 2007)
















From this, we can see early ecosystems were mat-dominated and vertically constrained (Zhang et al., 2025). Vertical tiering also seemed to appear before widespread infaunalisation (within sediment living). A gradual shift is recorded from mat-bound strategies to increased mobility, behavioural flexibility and exploiting sediments (Evans, 2017). Several modes also record morphological/body plan experimentation.
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