Microbioerosion - Trace Fossils as Indicators of Sedimentary Environments - page 222

TABLE 2 Ichnotaxa with Paleobathymetrical Relevance, Given with their Known or Inferred Producers, Known Stratigraphic

Range, and Today's Bathymetrical Range (XX

rare) as Reported by Golubic et al. (1975) , Perkins and Tsentas (1976) ,
Budd and Perkins (1980) , Akpan and Farrow (1984) , Hoffmann (1985) , G ¨ nther (1990) , Glaub (1994, 2004) , Gektidis (1997) ,
Bundschuh and Balog (2000) , Vogel et al. (2000) , Vogel and Glaub (2004) , Radtke and Golubic (2005) , Golubic and Radtke (2008) ,
Wisshak (2006) , Radtke et al. (2010) , Wisshak et al. (2011) , and Complemented by own Observations

¼ common; X ¼

Shallow
euphotic
I

Shallow
euphotic
II

Shallow
euphotic
III

Ichnotaxon
Biotaxon (type)

Deep
eu photic Dysphotic Stratigraphic range Aphotic

XX a XX a Fascichnus dactylus ( Radtke, 1991 )

Hyella caespitosa Bornet and Flahault,
1889 (cyanobacterium)

Ordovician-recent X

XX ( a )

Fascichnus acinosus ( Glaub, 1994 )
Hyella balani Lehmann, 1903
(cyanobacterium)

Permian-recent XX X

Fascichnus frutex ( Radtke, 1991 )
Hyella gigas Lukas and Golubic, 1983
(cyanobacterium)

Proterozoic-recent XX XX X

Fascichnus rogus ( Bundschuh and
Balog, 2000 )
Hyella racemus Al-Thukair et al., 1994
(cyanobacterium)

Ordovician-recent X XX

Fascichnus parvus ( Radtke, 1991 )
Hyella pyxis Lukas and Hoffman, 1984
(cyanobacterium)

Eocene-recent XX XX X

Continued