taxonID	type	format	identifier	references	title	description	created	creator	contributor	publisher	audience	source	license	rightsHolder	datasetID
03DB87D8FFEEFF90ACF5FB19027DC333.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/14530602/files/figure.png	https://doi.org/10.5281/zenodo.14530602	FIG. 1. — Sequestered and downward-transferred material in Zoophycos Massalongo,1855: A, black mud and white nannofossil ooze displaced for> 26 (black arrows) and> 23 cm (white arrows) downward, respectively, as indicated by colour and composition of sediment (Institute of Geological Sciences Kiel, Germany, core 16867-3; 2.2°S, 5.1°E, 3894 m water depth, mid Atlantic; 16.56-16.99 m core depth); B, sequestered organic-rich grey sediment filling Zoophycos spreite (white arrows) produced in red pelagic mud (Maastrichtian, Zumaia, Spain); C, homogeneous and pelleted sequestered sediment alternating with host sediment in Zoophycos spreite; inset (C’) showing pellets occurring in both sequestered sediment (green arrows) and host sediment (yellow arrows) (DSDP Leg 93, Site 605, Core 16-4, 59.5-66.5 cm core depth; for details see Wetzel 1987); D, truncation of lamellae (marked with red stippled lines) in Zoophycos spreite in horizontal section, indicating reworking of previously emplaced material (Paleogene, Zumaia, Spain). Scale bars: 1 cm.	FIG. 1. — Sequestered and downward-transferred material in Zoophycos Massalongo,1855: A, black mud and white nannofossil ooze displaced for> 26 (black arrows) and> 23 cm (white arrows) downward, respectively, as indicated by colour and composition of sediment (Institute of Geological Sciences Kiel, Germany, core 16867-3; 2.2°S, 5.1°E, 3894 m water depth, mid Atlantic; 16.56-16.99 m core depth); B, sequestered organic-rich grey sediment filling Zoophycos spreite (white arrows) produced in red pelagic mud (Maastrichtian, Zumaia, Spain); C, homogeneous and pelleted sequestered sediment alternating with host sediment in Zoophycos spreite; inset (C’) showing pellets occurring in both sequestered sediment (green arrows) and host sediment (yellow arrows) (DSDP Leg 93, Site 605, Core 16-4, 59.5-66.5 cm core depth; for details see Wetzel 1987); D, truncation of lamellae (marked with red stippled lines) in Zoophycos spreite in horizontal section, indicating reworking of previously emplaced material (Paleogene, Zumaia, Spain). Scale bars: 1 cm.	2024-08-30	Uchman, Alfred;Wetzel, Andreas		Zenodo	biologists	Uchman, Alfred;Wetzel, Andreas			
03DB87D8FFEEFF92AF6BF8BF07A1C492.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/14530606/files/figure.png	https://doi.org/10.5281/zenodo.14530606	FIG. 2. — Tubulichnium Książkiewicz, 1977 in turbiditic sand (Inoceramian Beds, Campanian-Paleocene, Magura Nappe, Słopnice, Poland): A, Tubulichnium penetrating down into turbidite sandstone; typical lining with mud pellets. Depression (surrounded by a white stippled line) resulting from sediment collapse after abandonment of the tube inhabited by the producer; B, C, traverse (B) and transverse oblique (C) sections of Tubulichnium. Pelletal laminae occurring at the base of the burrow (white arrows) and also in intermediate position (yellow arrows); local truncation of pellet-rich layers indicating subsequent, perhaps multiple reworking by the producer. Scale bars: 1 cm.	FIG. 2. — Tubulichnium Książkiewicz, 1977 in turbiditic sand (Inoceramian Beds, Campanian-Paleocene, Magura Nappe, Słopnice, Poland): A, Tubulichnium penetrating down into turbidite sandstone; typical lining with mud pellets. Depression (surrounded by a white stippled line) resulting from sediment collapse after abandonment of the tube inhabited by the producer; B, C, traverse (B) and transverse oblique (C) sections of Tubulichnium. Pelletal laminae occurring at the base of the burrow (white arrows) and also in intermediate position (yellow arrows); local truncation of pellet-rich layers indicating subsequent, perhaps multiple reworking by the producer. Scale bars: 1 cm.	2024-08-30	Uchman, Alfred;Wetzel, Andreas		Zenodo	biologists	Uchman, Alfred;Wetzel, Andreas			
03DB87D8FFECFF92AF98FBD8027CC1D1.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/14530609/files/figure.png	https://doi.org/10.5281/zenodo.14530609	FIG. 3. — Thalassinoides Ehrenberg, 1944 filled with planktonic foraminifera tests (downward displacement marked by a yellow arrow) in a sub-CCD setting indicating rapid sequestration after deposition on the sea floor; inset showing local truncation (red lines) of laminae (yellow lines), indicating subsequent,probably multiple reworking by the producer.(RV Sonne cruise 114, core 27-1, 0-21 cm sediment depth;15°45.00’N,115°45.00’E, central South China Sea, 4220 m water depth; for details see Wetzel & Unverricht 2013). Scale bar: 1 cm.	FIG. 3. — Thalassinoides Ehrenberg, 1944 filled with planktonic foraminifera tests (downward displacement marked by a yellow arrow) in a sub-CCD setting indicating rapid sequestration after deposition on the sea floor; inset showing local truncation (red lines) of laminae (yellow lines), indicating subsequent,probably multiple reworking by the producer.(RV Sonne cruise 114, core 27-1, 0-21 cm sediment depth;15°45.00’N,115°45.00’E, central South China Sea, 4220 m water depth; for details see Wetzel & Unverricht 2013). Scale bar: 1 cm.	2024-08-30	Uchman, Alfred;Wetzel, Andreas		Zenodo	biologists	Uchman, Alfred;Wetzel, Andreas			
03DB87D8FFECFF9CAF47F97F07DBC3D2.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/14530612/files/figure.png	https://doi.org/10.5281/zenodo.14530612	FIG. 4. — A-C, Field photographs of Avetoichnus luisae Uchman & Rattazzi, 2011 in the upper part of a turbiditic marl bed (Middle Eocene) at Zbludza, Magura Nappe, Polish Carpathians. Note that in A, Avetoichnus co-occurs with other sequestrichnia,i.e., Zoophycos. Abbreviations:Av, Avetoichnus luisae; Cha, Chondrites affinis (Sternberg, 1833); Chi, Chondrites intricatus (Brongniart, 1828); Zo, Zoophycos Massalongo, 1855. Scale bars: 1 cm.	FIG. 4. — A-C, Field photographs of Avetoichnus luisae Uchman & Rattazzi, 2011 in the upper part of a turbiditic marl bed (Middle Eocene) at Zbludza, Magura Nappe, Polish Carpathians. Note that in A, Avetoichnus co-occurs with other sequestrichnia,i.e., Zoophycos. Abbreviations:Av, Avetoichnus luisae; Cha, Chondrites affinis (Sternberg, 1833); Chi, Chondrites intricatus (Brongniart, 1828); Zo, Zoophycos Massalongo, 1855. Scale bars: 1 cm.	2024-08-30	Uchman, Alfred;Wetzel, Andreas		Zenodo	biologists	Uchman, Alfred;Wetzel, Andreas			
