Erratum to: Palaeobio Palaeoenv

Doi 10.1007/s12549-016-0263-y

The scale bars of the figures 7, 8, 9, and 10 had to be modified. Please see corrected figures below.

Fig. 7
figure 1

Incertae sedis algae Dreesenulella. a Silty algal wackestone/packstone affected by pressure solution (“peastone”). Dark stylocummulate separates Dreesenulella-rich facies (above) from Serrisinella-rich facies (below). Sample Goé-N-10-01. b Algal packstone with Dreesenulella showing a transition with Serrisinella (left, centre). Sample Goé-N-10a-04. c–d Micrographs of an algal packstone with Dreesenulella, showing specimens with 3 succeeding chambers. Samples Goé-Rive droite Falaise-SVP-01-02 (c), Goé-N-10a-13 (d)

Fig. 8
figure 2

Foraminifers (Septabrunsiina baeleni) with crinoids, Serrisinella and Kamaena,and solitary rugose corals. a Bioclastic wackestone with crinoids, ostracods and rare foraminifers (see top left). Sample Les Forges LF-7-2. b, c Recrystallized (slightly dolomitized) crinoidal grainstone (displaying limpid syntaxial rim cement around the crinoids) with relatively common plurilocular foraminifera, some Serrisinella, and kamaenaceans (Kamaena or Subkamaena sp.). c Samples Les Forges-2-02 (b). Les Forges LF-2-1 (c). d Recrystallized silty bioclastic packstone affected by pressure solution, with an oblique section of Neaxon? sp. Sample Goé-2

Fig. 9
figure 3

Crinoidal grainstones and silty packstones, affected by pressure solution (a–c) and mineralized hardgrounds (d). a Crinoidal grainstone (tempestite) strongly affected by pressure solution. Upper part shows unaffected bioclastic grainstone. Lower part shows corroded crinoid ossicles and dark stylocumulates. Sample Limbourg-Mali-encrinite-02. b–c Micrographs of a silty crinoid-rich packstone/grainstone and even rudstone affected by pressure solution, generating a so-called stylonodular fabric (not affected relicts resemble intraclasts). Samples Les Forges-8-01 (b) and Les Forges-8-02 (c). d Thin brown phosphoritized microstromatolitic hardground and intraclasts (top left) separating a bioclastic packstone/grainstone (below) from a very silty bioclastic packstone (above) affected by pressure solution. This sample yielded a relatively rich conodont fauna indicating a Late marginifera age as well as a diversified (silicified) ostracod assemblage (see Dreesen et al. 1985). Sample COM-1-hardground-01

Fig. 10
figure 4

Mud mound core (including microbial-spiculitic mudstones and bioclastic wackestones) with reworked Baculella, crinoids, sponge spicules and stromatactis-type fenestrae. a Bioclastic wackestone with crinoids (bottom, left) and Dreesenulella (top, right). Sample Hors-les-Portes-3-1. b–c Bioclastic (spiculitic) mudstone/wackestone with abundant sponge spicules and relatively common crinoid ossicles (especially in micrograph). Samples Hors-les-Portes-1-01 (b) and Hors-les-Portes-1-02 (c). d Red, microbial/bioclastic wackestone with stromatactis structures and bioclasts (including ostracods, crinoids, sponge spicules, reworked algae, etc.). Sample Les Forges (rouge) 01

Please note, that one reference was not correctly published, below the correct reference:

Dreesen, R. (1989). The “Cheiloceras Limestone” a Famennian (Upper Devonian) event-stratigraphical marker in Hercynian Europe and Northwestern Africa? Bulletin de la Société belge de Géologie, 98, 127–133.