"
Thalassinoides mazes occur in lower Cambrian nearshore carbonate sediments, leading to intense disruption of the primary fabric. "
"The top of the channel and crevasse-splay sandstone represents colonization surfaces that allow direct measurements of maximum burrowing depth. Taenidium barretti extends up to 2.2 m into the crevasse sand sheets. Depth and intensity of bioturbation of the main-channel and crevasse sands seem to be a function of time between depositional events. Main-channel and crevasse sandstones underlying thick packages of bioturbated overbank mudstones are intensely bioturbated, recording prolonged periods of low-energy sediment fallout between crevassing events. Conversely, the lowest degree of bioturbation is found in amalgamated channel sandstone units underlying thin intervals of overbank mudstones, reflecting high-frequency depositional episodes.
Deep and intense bioturbation in... (PDF Download Available). Available from:
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https://www.researchgate.net/public...ence_from_Miocene_fluvial_deposits_of_Bolivia
"Episode I occurred in Beds 25–27b when the ecologically complicate forms such as Chondrites, Skolithos, Rhizocorallium, and Thalassinoides disappeared hereafter, the bioturbation index reduced from 1–5 to 1–3, and the disturbed depth declined from 5–66 to 2–5 cm. "
"Sand without primary sedimentary structures due to pervasive bioturbation."
" Commonly the primary sedimentary structures are completely destroyed by bioturbation."
" The sandstones may locally display wave ripple lamination and apparently bio-lamination, but commonly the primary stratification is destroyed by very intense bioturbation. "
"(A)
Bioturbation in sandstone with glauconite-rich, finer-grained
Ophiomorpha or
Palaeophycus burrow linings; well 16/3–6. (B) Coarse grained sandstone with intense bioturbation (
Palaeophycus?) forming a mottled appearance due to finer-grained, stained linings of the roofs of burrows. The bioturbated sandstone is gradational downwards to structureless sandstone; well 16/2-7A (C) Large bifurcating burrow filled with gravel and lined with darker coloured finer grained sand (
Thalassinoides or
Ophiomorpha). Notice that the background sand matrix is composed of bioturbated coarse grained sand with darker medium grained sand burrow linings (?
Palaeophycus); well 16/2-13A. (D) Bioturbated sand with granule infill of boxwork
Thalassinoidesor O
phiomorpha burrows; well 16/2–8."
"(B) Very fine to fine grained sandstone bed, showing parallel
lamination passing up to intense
bioturbation. Notice large burrow filled with coarse sand from a bed above; well 16/2–15. (C) Totally bioturbated fine grained sandstone bed with
Macaronichus (?); well 16/2-14T2."
" Fining-upward heterolith with numerous belemnites. The heterolith is intensely bioturbated, destroying the original layering; well 16/2–16. (D) Transition from facies 8 through facies 9 and to facies 10. Notice numerous belemnites in heterolithic and apparently bioturbated facies "
"In the Johan Sverdrup area the shoreface deposits seem to fall into two associations – upper shoreface with abundant stratification, and lower shoreface with virtually no stratification due to
bioturbation. "
"[4] The organisms responsible for bioturbation on the shallower flanks of Santa Barbara Basin (500– 550 m) have been well studied. They include tubificid oligochaetes, tubicolous ampeliscid amphipods, dorvilleid polychaetes and the bivalve Lucinoma aequizonata [Levin et al., 2001, 2002; Cary et al., 1989; L.A. Levin, unpublished data]. In general, bioturbation results from foraging activities of deposit feeding animals, although other activities such as tube building also affect sediment structure."
The bottom left image is displaying several feet in which lamination has been obstructed by burrowing.
"
Wave-dominated environment sandstones were
previously interpreted as shoreface sands, which were
extensively bioturbated, associated with beach, offshore
transition and shelf deposits in wave-dominated
environment sandstones accumulated on the marine
coastal quite far from the deltaic river mouth."
Depositional Environment of... (PDF Download Available). Available from:
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