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![Loloichnus ichnofabric (Lo) and Loloichnus-Taenidium ichnofabric (Lo/Tae). A, B) Lo ichnofabric is constituted by a monospecific suite of multiple-tier Loloichnus isp. preserved in both lateral accretion units of the middle part of point bars (A) and conglomeratic facies of the lower part of point bars (B). C) General view of Lo ichnofabric in overbank facies truncated by channel deposits recording Lo/Tae ichnofabric. D) Close up of the Lo ichnofabric in overbank deposits. E, F) Lo/Tae ichnofabric formed by dwelling and feeding trace fossils occurring in moderately to highly bioturbated overbank facies (E) and above inclined surfaces of the lateral accretion units of the middle part of point bars (F). G) Close up of the top of a lateral accretion unit. The Lo/Tae ichnofabric shows abundant shallow-tier Taenidium barreti. Abbreviations: BI = bioturbation index; Ta = Taenidium barreti; Lo = Loloichnus isp.; Pa = Palaeophycus isp.]()
![Sedimentology of the tide-influenced meander-loop deposits of the Lower Red Unit (Tremp Formation). A) Panoramic field view and stratigraphic log. Note the sigmoidal shape of the lateral accretion units, separated by reactivation surfaces (rs). B) Summary of sedimentological characteristics, including the results of this study. Modified from Díez-Canseco et al. (2014, 2016). Abbreviations: Ar/Tae = Arenicolites/Taenidium ichnofabric; Tae1 = Taenidium ichnofabric 1; Tae2 = Taenidium ichnofabric 2; Lo = Loloichnus ichnofabric; Lo/Tae = Loloichnus-Taenidium ichnofabric.]()
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![Loloichnus isp. preserved as full relief: (1) general view of the cylindrical and gently sinuous burrow with knobby surface, field photo, scale bar represents 1 cm; (2) detail of the knobby surface texture on the burrow fill, DEUC-IC 16, scale bar represents 1 cm; (3) burrow wall and fill in thin-section; note the micritic wall (white arrow) and the semicircular sections in the inner wall of the transversal grooves (white dashed lines), microscope photo, scale bar represents 500 μm.]()
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![Descriptive statistics for the measures of burrow width: (1) distribution of burrow widths grouped by ichnotaxa; note the burrow width ranging from 3 to 28 mm; (2) Interquartile Range (IQR) plotted for each ichnogenus and showing three populations of burrow widths based in the position and size of the IQR; note that “variable” is here synonymous of relative high dispersion of values. Mean is indicated with the black transversal line. Ichnogenera displayed are from the bottom to the top, Palaeophycus, Planolites, Taenidium, Arenicolites, and Loloichnus.]()
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Loloichnus
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Image
Loloichnus ichnofabric (Lo) and Loloichnus-Taenidium ichnofabric (Lo/Tae...
in UNLOCKING THE ARCHITECTURE OF THE COLONIZATION WINDOW: ICHNOFABRICS FROM UPPER CRETACEOUS TIDE-INFLUENCED MEANDER-LOOP DEPOSITS
> PALAIOS
Published: 03 May 2023
Fig. 5 Loloichnus ichnofabric (Lo) and Loloichnus-Taenidium ichnofabric (Lo/Tae). A , B ) Lo ichnofabric is constituted by a monospecific suite of multiple-tier Loloichnus isp. preserved in both lateral accretion units of the middle part of point bars (A) and conglomeratic facies
Image
Sedimentology of the tide-influenced meander-loop deposits of the Lower Red...
in UNLOCKING THE ARCHITECTURE OF THE COLONIZATION WINDOW: ICHNOFABRICS FROM UPPER CRETACEOUS TIDE-INFLUENCED MEANDER-LOOP DEPOSITS
> PALAIOS
Published: 03 May 2023
characteristics, including the results of this study. Modified from Díez-Canseco et al. (2014 , 2016 ). Abbreviations: Ar/Tae = Arenicolites / Taenidium ichnofabric; Tae1 = Taenidium ichnofabric 1; Tae2 = Taenidium ichnofabric 2; Lo = Loloichnus ichnofabric; Lo/Tae = Loloichnus-Taenidium ichnofabric.
Journal Article
UNLOCKING THE ARCHITECTURE OF THE COLONIZATION WINDOW: ICHNOFABRICS FROM UPPER CRETACEOUS TIDE-INFLUENCED MEANDER-LOOP DEPOSITS
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 03 May 2023
PALAIOS (2023) 38 (4): 173–187.
...Fig. 5 Loloichnus ichnofabric (Lo) and Loloichnus-Taenidium ichnofabric (Lo/Tae). A , B ) Lo ichnofabric is constituted by a monospecific suite of multiple-tier Loloichnus isp. preserved in both lateral accretion units of the middle part of point bars (A) and conglomeratic facies...
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Journal Article
Ichnofauna from coastal meandering channel systems (Upper Cretaceous Tremp Formation, South-Central Pyrenees, Spain): delineating the fluvial-tidal transition
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 March 2016
Journal of Paleontology (2016) 90 (2): 250–268.
...Davinia Díez-Canseco; Luis A. Buatois; M. Gabriela Mángano; Margarita Díaz-Molina; M. Isabel Benito Abstract The Upper Cretaceous “redbeds” of the lower Tremp Formation (South-Central Pyrenees, Spain) contains an ichnofauna consisting of Taenidium barretti , Taenidium bowni , Loloichnus isp...
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Image
Loloichnus isp. preserved as full relief: ( 1 ) general view of the cylind...
in Ichnofauna from coastal meandering channel systems (Upper Cretaceous Tremp Formation, South-Central Pyrenees, Spain): delineating the fluvial-tidal transition
> Journal of Paleontology
Published: 01 March 2016
Figure 3 Loloichnus isp. preserved as full relief: ( 1 ) general view of the cylindrical and gently sinuous burrow with knobby surface, field photo, scale bar represents 1 cm; ( 2 ) detail of the knobby surface texture on the burrow fill, DEUC-IC 16, scale bar represents 1 cm; ( 3 ) burrow wall
Image
Sedimentologic and paleontologic features in the “redbed” facies (Maastrich...
in Ichnofauna from coastal meandering channel systems (Upper Cretaceous Tremp Formation, South-Central Pyrenees, Spain): delineating the fluvial-tidal transition
> Journal of Paleontology
Published: 01 March 2016
authigenic glauconite Paleosols Root traces Invertebrate traces. Taenidium and Loloichnus Paleochannel deposits Hybrid arenite and sandy-marly mudstone and subordinate conglomerate at the base Inclined heterolithic stratification with erosional and no erosional reactivation
Image
Descriptive statistics for the measures of burrow width: ( 1 ) distribution...
in Ichnofauna from coastal meandering channel systems (Upper Cretaceous Tremp Formation, South-Central Pyrenees, Spain): delineating the fluvial-tidal transition
> Journal of Paleontology
Published: 01 March 2016
in the position and size of the IQR; note that “variable” is here synonymous of relative high dispersion of values. Mean is indicated with the black transversal line. Ichnogenera displayed are from the bottom to the top, Palaeophycus , Planolites , Taenidium , Arenicolites , and Loloichnus .
Image
Statistical data for the measures of burrow width. Statis...
in Ichnofauna from coastal meandering channel systems (Upper Cretaceous Tremp Formation, South-Central Pyrenees, Spain): delineating the fluvial-tidal transition
> Journal of Paleontology
Published: 01 March 2016
5,7 9,31 6,92 50 12,88 15,33 5,16 7,8 9,98 9,82 11,88 10 75 16,07 18,85 6,52 10,2 13,16 12,57 12,84 12,82 (a) Several modes. Minimum mode displayed Ar, Arenicolites isp.; Lo, Loloichnus isp.; Pa= Palaeophycus isp.; Pa= Planolites isp.; T. ba (1
Journal Article
A MIDDLE PERMIAN (ROADIAN) LUNGFISH AESTIVATION BURROW FROM THE RIO DO RASTO FORMATION (PARANÁ BASIN, BRAZIL) AND ASSOCIATED U-Pb DATING
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 27 February 2018
PALAIOS (2018) 33 (2): 69–84.
... 1993 ; Capayanichnus Melchor et al. 2010 ; Daimonelix Barbour 1895 ; Gyrolithes Saporta 1884 ; Ichnogyrus Bown and Kraus 1983 ; Katarrhedrites Hembree and Hasiotis 2008 ; Kladosystemites Hembree and Hasiotis 2008 ; Loloichnus Bedatou et al. 2008 ; Lunulichnus Zonneveld et al. 2006...
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