Bivalve Filter Feeding: Hydrodynamics, Bioenergetics, Physiology and Ecology.C. Barker Jorgensen

Tom Fenchel

doi:10.1086/417296

Feeding behavior of 5 species filter-feeding bivalves on Paralichthys olivaceus feed,fecal and sediment particulates in cage farming area

JOURNAL OF FISHERIES OF CHINA ◽

10.3724/sp.j.1231.2013.38401 ◽

2013 ◽

Vol 37 (5) ◽

pp. 727 ◽

Cited By ~ 5

Author(s):

Jihong ZHANG ◽

Tao WU ◽

Yaping GAO ◽

Wang TANG

Keyword(s):

Feeding Behavior ◽

Paralichthys Olivaceus ◽

Filter Feeding ◽

Farming Area

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CFD-DEM simulation of the hydrodynamic filtration performance in balaenid whale filter feeding

The Science of The Total Environment ◽

10.1016/j.scitotenv.2021.147696 ◽

2021 ◽

pp. 147696

Author(s):

Ya-Wei Zhu ◽

De-An Hu ◽

Chang-Ran Li ◽

Chen Zhuang ◽

Gang Yang

Keyword(s):

Filter Feeding ◽

Dem Simulation ◽

Filtration Performance ◽

Hydrodynamic Filtration

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Glossifungites gingrasi n. isp., a probable subaqueous insect domicile from the Cretaceous Ferron Sandstone, Utah

Journal of Paleontology ◽

10.1017/jpa.2020.115 ◽

2021 ◽

pp. 1-13

Author(s):

M. Ryan King ◽

Andrew D. La Croix ◽

Terry A. Gates ◽

Paul B. Anderson ◽

Lindsay E. Zanno

Keyword(s):

Coastal Plain ◽

Upper Cretaceous ◽

Filter Feeding ◽

Chironomid Larvae ◽

Large Size ◽

Rock Record ◽

Axis Parallel ◽

Freshwater Fauna

Abstract A new ichnospecies, Glossifungites gingrasi n. isp., is described from multiple locations in basal sand-filled coastal plain distributary channels of the Turonian (Upper Cretaceous) Ferron Sandstone (central Utah). Glossifungites gingrasi n. isp. is attributed to the ichnogenus Glossifungites based on the presence of scratch imprints, passive fill, and a tongue-shaped structure, yet the new ichnospecies is distinct because it displays transverse bioglyphs that run perpendicular to the planiform structure, which contrasts to the axis parallel bioglyphs present in the ichnospecies G. saxicava. The transverse arrangement of ornamentation exhibited by G. gingrasi n. isp. is observed in modern subaqueous insect burrows produced by mayfly and chironomid larvae, and constitutes a way to differentiate insect-generated burrows from structures produced by crustaceans that are known to create other Glossifungites ichnospecies. Differentiating insect- from crustacean-generated burrows is significant because it provides a way to distinguish bioturbation by marine-recruited fauna from that produced by freshwater fauna in the rock record, making G. gingrasi n. isp. a valuable ichnological tool for paleoenvironmental and stratigraphic interpretation. While G. gingrasi n. isp. may represent a burrow created by a variety of filter-feeding subaqueous insects, the large size of G. gingrasi n. isp. in the Ferron Sandstone suggests that the largest specimens are probable mayfly burrows and supports the assertion that burrowing mayflies (e.g., Polymitarcyidae and Ephemeridae) adapted to domicile filter-feeding during or prior to the Turonian. UUID: http://zoobank.org/a033b22f-bf09-481a-975e-3a1b096154cc

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