FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3200310558> ?p ?o ?g. }

• W3200310558 endingPage "20" @default.
• W3200310558 startingPage "1" @default.
• W3200310558 abstract "Abstract Arumberia is an enigmatic sedimentary surface texture that consists of parallel, sub-parallel or radiating ridges and grooves, most commonly reported from upper Neoproterozoic – lower Palaeozoic strata. It has variably been interpreted as the impression of a small metazoan, a ‘vendobiont’, a physical sedimentary structure formed on a substrate with or without a microbial mat covering, or a non-actualistic microbial community. In this paper we contribute new insights into the origin of Arumberia , resulting from the discovery of the largest contiguous bedding plane occurrence of the texture reported to date: a 300 m 2 surface in the lower Cambrian Port Lazo Formation of Brittany, NW France. We compare the characteristic features of Arumberia at this locality with 38 other global records, revealing four defining characteristics: (1) the three-dimensional (3D) morphology of exposed Arumberia lines (either positive relief ‘ridges’ or negative relief ‘grooves’) records fully preserved cords within clay laminae; (2) lines may transition laterally into reticulated patterns; (3) characteristic parallel and sub-parallel Arumberia lines can become modified by desiccation on emergent substrates prior to interment; and (4) Arumberia are streamlined with palaeoflow in successions showing evidence of unidirectional currents, but are organized parallel to ripple crests where strata were sculpted by oscillatory flows. These characteristics indicate that Arumberia records a 3D entity, distinct in material properties from its host sediment, which occurred in very shallow water settings where it was prone to passive reorganization in moving water, and desiccation when water drained. A literature survey of all known Arumberia occurrences reveals that the most reliable examples of the form are stratigraphically restricted to a 40 Ma interval straddling the Ediacaran–Cambrian boundary (560–520 Ma). Together these characteristics suggest that Arumberia records the remains of extinct, sessile filamentous organisms (microbial or algal?) that occupied very shallow water and emergent environments across the globe at the dawn of the Phanerozoic Eon." @default.
• W3200310558 created "2021-09-27" @default.
• W3200310558 creator A5001277622 @default.
• W3200310558 creator A5035754820 @default.
• W3200310558 creator A5047443910 @default.
• W3200310558 creator A5064259355 @default.
• W3200310558 date "2021-09-17" @default.
• W3200310558 modified "2023-09-30" @default.
• W3200310558 title "Enigma variations: characteristics and likely origin of the problematic surface texture <i>Arumberia</i>, as recognized from an exceptional bedding plane exposure and the global record" @default.
• W3200310558 cites W1959275669 @default.
• W3200310558 cites W1963858086 @default.
• W3200310558 cites W1972083608 @default.
• W3200310558 cites W1972992559 @default.
• W3200310558 cites W1975895954 @default.
• W3200310558 cites W1977409179 @default.
• W3200310558 cites W1986213008 @default.
• W3200310558 cites W1989686103 @default.
• W3200310558 cites W1995137647 @default.
• W3200310558 cites W2001814040 @default.
• W3200310558 cites W2011104465 @default.
• W3200310558 cites W2011200896 @default.
• W3200310558 cites W2015735647 @default.
• W3200310558 cites W2028581643 @default.
• W3200310558 cites W2039172704 @default.
• W3200310558 cites W2046501413 @default.
• W3200310558 cites W2053471224 @default.
• W3200310558 cites W2055353146 @default.
• W3200310558 cites W2058184799 @default.
• W3200310558 cites W2059043949 @default.
• W3200310558 cites W2067260360 @default.
• W3200310558 cites W2068472641 @default.
• W3200310558 cites W2070635028 @default.
• W3200310558 cites W2089735540 @default.
• W3200310558 cites W2089875464 @default.
• W3200310558 cites W2090288913 @default.
• W3200310558 cites W2092472360 @default.
• W3200310558 cites W2130982936 @default.
• W3200310558 cites W2132666243 @default.
• W3200310558 cites W2135120615 @default.
• W3200310558 cites W2146183001 @default.
• W3200310558 cites W2160214024 @default.
• W3200310558 cites W2161503203 @default.
• W3200310558 cites W2161688825 @default.
• W3200310558 cites W2174891314 @default.
• W3200310558 cites W2224212289 @default.
• W3200310558 cites W2260262913 @default.
• W3200310558 cites W2402350182 @default.
• W3200310558 cites W2477054343 @default.
• W3200310558 cites W2483013235 @default.
• W3200310558 cites W2585002790 @default.
• W3200310558 cites W2592780308 @default.
• W3200310558 cites W2617748364 @default.
• W3200310558 cites W2753888411 @default.
• W3200310558 cites W2782536658 @default.
• W3200310558 cites W2795167799 @default.
• W3200310558 cites W2809597697 @default.
• W3200310558 cites W2886049716 @default.
• W3200310558 cites W2913574362 @default.
• W3200310558 cites W2992221908 @default.
• W3200310558 cites W3020936465 @default.
• W3200310558 cites W3036901131 @default.
• W3200310558 cites W3128014556 @default.
• W3200310558 cites W3129082694 @default.
• W3200310558 cites W3134990411 @default.
• W3200310558 cites W3136489585 @default.
• W3200310558 cites W3165037622 @default.
• W3200310558 doi "https://doi.org/10.1017/s0016756821000777" @default.
• W3200310558 hasPublicationYear "2021" @default.
• W3200310558 type Work @default.
• W3200310558 sameAs 3200310558 @default.
• W3200310558 citedByCount "11" @default.
• W3200310558 countsByYear W32003105582022 @default.
• W3200310558 countsByYear W32003105582023 @default.
• W3200310558 crossrefType "journal-article" @default.
• W3200310558 hasAuthorship W3200310558A5001277622 @default.
• W3200310558 hasAuthorship W3200310558A5035754820 @default.
• W3200310558 hasAuthorship W3200310558A5047443910 @default.
• W3200310558 hasAuthorship W3200310558A5064259355 @default.
• W3200310558 hasBestOaLocation W32003105581 @default.
• W3200310558 hasConcept C109007969 @default.
• W3200310558 hasConcept C115961682 @default.
• W3200310558 hasConcept C121332964 @default.
• W3200310558 hasConcept C127313418 @default.
• W3200310558 hasConcept C134872888 @default.
• W3200310558 hasConcept C144027150 @default.
• W3200310558 hasConcept C146588470 @default.
• W3200310558 hasConcept C151730666 @default.
• W3200310558 hasConcept C154945302 @default.
• W3200310558 hasConcept C155954305 @default.
• W3200310558 hasConcept C165801399 @default.
• W3200310558 hasConcept C166528214 @default.
• W3200310558 hasConcept C18903297 @default.
• W3200310558 hasConcept C2777232088 @default.
• W3200310558 hasConcept C2779599953 @default.
• W3200310558 hasConcept C2781195486 @default.
• W3200310558 hasConcept C2816523 @default.
• W3200310558 hasConcept C41008148 @default.
• W3200310558 hasConcept C50402729 @default.

• next