
http://app.pan.pl/SOM/app60-Izumi_SOM.pdf SUPPLEMENTARY ONLINE MATERIAL FOR Composite Phymatoderma from Neogene deep-marine deposits in Japan: Implications for Phanerozoic benthic interactions between burrows and the trace-makers of Chondrites and Phycosiphon Kentaro Izumi Published in Acta Palaeontologica Polonica 2015 60 (4): 1009-1020. http://dx.doi.org/10.4202/app.00060.2014 Supplementary Online Material Table. Phanerozoic records of trace fossils (or modern traces) that were reworked by Chondrites and Phycosiphon. References Table. Phanerozoic records of trace fossils (or modern traces) that were reworked by Chondrites and Phycosiphon. Reworked by Chondrites Burrow diameter Formation or Lithology/Depositional Reworked trace Age of reworked Reference Note section/Locality setting fossil materials (mm) various modern various regions such sediments/deep-sea (water Modern as outer Bengal Fan Planolites 2-15 Wetzel 1991 depth greater than 500-1000 area m) Krishna-Godavari cold-seep pellet-filled bran- Mazumdar et Quaternary 4-17 basin/Bay of Bengal carbonate/continental slope ched burrows al. 2011 British Geological muds and sandy muds with Pliocene- diameter not described, but measured using Survey Borehole rare dropstones/anomalous, Planolites 11.43 Leslie 1993 Pleistocene fig. 9 88/7 /Hebrides Slope difficult to interpret alternations of tuffaceous Shiramazu Pliocene sandstones and Phymatoderma 8.30-30.95 Izumi in press Formation/Japan siltstones/continental slope mud, sand, lignite, and shell middle Pebas Gingras et al. bed/tidally-influenced, Planolites less than 2 Miocene Formation/Peru 2002 brackish water Helicodromites 2.6-3.2 (smaller) mobilis 5.4-9.8 (larger) sandy, muddy, and Chenque Carmona et early Miocene tuffaceous/tidal bars, subtidal Gyrolithes 45-65 Formation/Argentina al. 2008 bars, shoreface Teichichnus 10-12 zigzag Thalassinoides 17-76 Planolites 3-7 middle thin-bedded siliciclastic Heard et al. Ainsa Basin/Spain Eocene turbidites/deep-sea 2008 Thalassinoides 5-20 fine-grained siliciclastic, middle Scaglia Toscana Monaco et al. carbonate, and bioclastic Palaeophycus 10-20 Eocene Formation/Italy 2012 turbidites/deep-sea alternations of limestones, marly limestones and marls, Planolites 4-5 Rodríguez- Paleocene- Itzurun with intercalations of Tovar et al. Eocene Formation/Spain turbidite/between middle and 2011b lower bathyal environments, at about 1000 m water depth Zoophycos 3-4 marginal tunnel diameter Palaeophycus 20 or larger than tubularis form A 20 Palaeophycus less than 20 tubularis form B Planolites alternating limestones, ca. 5 calcareous turbidites, and montanus Giannetti and Zumaya late Paleocene siliceous sandstones/deep- Thalassinoides McCann section/Spain 5-15 marine at water depth of ca. suevicus 2010 1000 m Zoophycos diameter of the whole structure, not diameter 50-350 brianteus of marginal tube Zoophycos isp. not described form A Thalassinoides- interbedded biomicrite and Scaglia Cinerea Phycodes late Paleocene calcareous mudstone or 3-10 Miller 2001 unit/Italy compound marl/bathyal depth system marls and marly Rodríguez- Cretaceous/ Jorquera Thalassinoides 10-20 limestones/middle bathyal Tovar and Paleogene Formation/Spain at water depth 600-1000 m turbular burrow 10 Uchman 2006 Bidart hemipelagites and Planolites 2.5-4 Rodríguez- Cretaceous/ section/France turbidites/water depth ranging Tovar et al. Paleogene Sopelana 4-9 (smaller) from 1000 to 1500 m Thalassinoides 2011a section/Spain 15-30 (larger) cyclic chalk-marl succession/below storm wave late Rørdal Lauridsen et base with water depth of Thalassinoides 15-25 Maastrichtian Member/Denmark al. 2011 probably several hundreds meters late Dania probably Bromley and diameter not described, but measured using chalk/shallow-water chalk 7.25 Maastrichtian Quarry/Denmark Thalassinoides Ekdale 1984b fig. 5 Ekdale and late Dania diameter not described, and difficult to chalk/shelf-sea Thalassinoides - Bromley Maastrichtian Quarry/Denmark measure using a published figure 1991 Planolites carbonate-siliciclastic late beverleyensis ca. 5 Monte Antola flysch/deep-sea below the Campanian- morphotype B Uchman 2007 Formation/Italy calcite compensation depth Maastrichtian (CCD) ?Radhostium isp. 3-10 thin-bedded marlstones Campanian- interbedded with muddy to Ropianka Leszczyński early clayey shales and thin-bedded Planolites 1.5-5 Formation/Poland 2004 Maastrichtian sandstones/trough-type deep- sea basin Wyandot fine-grained calcareous Santonian- Phillips and Formation/offshore mudstone/outer shelf to upper Thalassinoides 12-40 Maastrichtian McIlroy 2010 Nova Scotia bathyal setting Cenomanian- Chalk unit/northen Bromley and chalk/not described Thalassinoides - diameter not described Maastrichtian Europe Ekdale 1984a early Province de Gyrolithes Bromley and smectite/not described ca. 1 diameter of burrow walls Campanian Liége/Belgium davreuxi Frey 1974 Piesenkopf- thin-bedded turbiditic flysch late Turonian- Planolites Schichten/Austria composed of sandstone- 3-8 Uchman 1999 late Santonian beverleyensis and Germany limestone;marlstone/deep-sea marlstone dominated/outer Kędzierski Turonian- Planolites 2-6 Opole region/Poland shelf (below storm wave and Uchman Coniasian base) Thalassinoides 12-25 2001 marly limestones and marls Rogríguez- Cenomanian- Capas Blancas with chert nodules and Thalassinoides 6-11 Tovar et al. Turonian Formation/Spain beds/moderately deep pelagic 2009 plateau Cenomanian- Rybie marl dominated/submarine Uchman et al. Planolites 2.5-4.5 Turonian section/Poland high 2013a cherty limestones intercalated with black shales, gray marly Cenomanian- Bonarelli shales and non-calcareous Uchman et al. Thalassinoides 7-18 Turonian Level/Poland shales/pelagic and 2013b hemipelagic, beyond tha range of gravitational flows middle limestones, separated by The Chalk Marl/UK Thalassinoides - Gale 1989 diameter not described Cenomanian marly shalk/not described Late Resspass/ ? (= it cannot be Uchman and calcareous turbidite/deep-sea ? Cretaceous Switzerland observed today) Wetzel 1999 alternations of breccia, Kotick Point Buatois and Aptian- conglomerates, sandstones Cladichnus Formation/Antarctic 2-5 Mángano Albian and mudstones/continental fischeri a 1992 slope interbedded calcareous Bouvières Gaillard and Hauterivian mudstone and Halimedides 0.5-2.5 section/France Olivero 2009 marlstone/deep-marine Unterpurkersdorf at ? (= not described, but measured using plate 3, Cretaceous not described/not described 6.09, 6.40 Fu 1991 Wien Bandchondriten) photos A-B massive to well-bedded Monaco and Calcari Grigi limestones and Ophiomorpha Pliensbachian 20-40 Garassino Formation/Italy marls/shallow-water irregularie 2001 carbpnate platform massive to well-bedded Monaco and Sinemurian/ Calcari Grigi limestones and Ophiomorpha 30-50 Giannetti Pliensbachian Formation/Italy marls/shallow-water, oceanic nodosa 2002 carbonate platform Simpson Sinemurian Bishopsworth/UK dark shale/not described Corophioides 7-8 U-tunnel diameter 1957 age and depositional setting of the studied succession (highest part of the Blue Lias Blue Lias and interbedded mudstones and Formation to the lowest part of the Charmouth Charmouth limestones with distinctive Gallois and ?Sinemurian Planolites 15 Mudstone Formation) are not describedBlue Mudstone marker beds/?shallow shelf Paul 2009 Lias Formation: Hettangian-Sinemurian Formations/UK environment Charmouth Mudstone Formation: Sinemurian- lower Pliensbachian rhythmically bedded black Moghadam Hettangian- Blue Lias shales and marls (sometimes Thalassinoides 10-40 and Paul Simenurian Formation/UK limestones)/shallow shelf 2000 paleoenvironment Bravaisberget and dark organic-rich Mørk and Middle Botneheia Forma- shale/deltaic to restricted Thalassinoides 10-50 Bromley Triassic tions/Svalbard shelf 2008 Early Oquirrh not described/controversial Ekdale and diameter not described, but measured using Pensilvanian- Spirophycus 3-5 Formation/US (shallow vs. deep) Mason 1988 fig. 2C and F Early Permian very fine-grained silty Early Morrow Buatois et al. diameter not described, but measured using sandstone and siltstone/distal Alenicorites ca. 1.5 Pensilvannian Sandstone/US 2002 fig. 8C lower-shoreface a few mm to a few Trypanites depositional setting from Li et al. 2001 Late Yeoman carbonate-evaporite cm Pak et al. Ordovician Formation/Canada cycles/marine shelf 2010 a few mm to a few Thalassinoides cm Reworked by Phycosiphon Burrow diameter Formation or Reworked trace Age Lithology/Depositional setting of reworked Reference Note section/Locality fossil materials (mm) diameter not described, but measured using Modern off NW Africa modern deposits/bathyal Planolites 11.25, 13.75 Wetzel 2010 Text-fig. 4-2 alternations of tuffaceous Shiramazu Pliocene sandstones and Phymatoderma 9.70-40.65 Izumi in press Formation/Japan siltstones/continental slope Chenque sandy, muddy, and Carmona et early Miocene Formation/ tuffaceous/tidal bars, subtidal Thalassinoides 17-76 al. 2008 Argentina bars, shoreface diameter not described, and difficult to Thalassinoides - measure using a published figure/reworked by Anconichnus Ekdale and late Dania diameter not described, and difficult to chalk/shalf-sea Bromley Maastrichtian Quarry/Denmark ?Thalassinoides - measure using a published figure/reworked by 1991 Anconichnus diameter of vertical shaft, but Anconichnus- Zoophycos 8 animal has meticulously avoided the shaft López de mudstones and sandstones, Olivero and Bertodano glauconite-rich sandstones and Euflabella Maastrichtian 8-15 Lopez final tube diameter Formation/
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