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Genus Phyllospongia Ehlers, 1870

 

Distribution

States

New South Wales, Queensland, South Australia, Tasmania, Victoria, Western Australia


Extra Distribution Information

S Africa, Indian Ocean, Red Sea, Indo-Malayan region, New Zealand, Japan, W and central Pacific Ocean.


IBRA and IMCRA regions (map not available)

IMCRA

Northwest Shelf Province (27), Central Western Shelf Transition (28), Central Western Shelf Province (29), Spencer Gulf Shelf Province (33), Western Bass Strait Shelf Transition (34), Bass Strait Shelf Province (35), Southeast Shelf Transition (37), Central Eastern Shelf Province (38), Central Eastern Shelf Transition (39), Northwest Province (4), Northeast Shelf Province (40), Northeast Shelf Transition (41), Central Western Transition (5)

Distribution References

Diagnosis

Phyllospongia diagnosis
Lamellate, vasiform, digitate or foliose sponges (Fig. 7C–F), typically thin-walled, with an unarmoured, smooth, irregularly corrugated, micro-conulose surface. The fibre skeleton comprises a regular reticulation of primary ascending, secondary connecting, and vermiform tertiary fibres. Primary fibres are axially cored with foreign debris, secondary and vermiform tertiary fibres are uncored. Secondary fibres may dominate the fibre skeleton in some species, particularly those with a thicker habit. Vermiform tertiary fibres are sometimes dispersed throughout the mesohyl, but are more typically arranged as an axial skeleton, particularly in the base and stalk. In digitate forms they can form fascicles, arranged in a similar orientation to secondary fibres. A sand cortex is usually present on one or both surfaces, but it never becomes a distinct sand armour, as seen in Carteriospongia and Strepsichordaia. The consistency is tough and flexible.

Carteriospongia diagnosis
Lamellate, foliose, caliculate and spreading forms are typical (Fig. 7G–I), though variable. The surface is heavily armoured with foreign debris and displays a characteristic pattern of mounds or ridges (Fig. 7J), that tend to be more pronounced on the oscular face. The relatively dense, irregular fibre skeleton comprises primary, secondary and tertiary fibres. Primary fibres are heavily cored, and may form strong fascicles in the subsurface region; primary fibres do not necessarily comprise the ascending component of the skeleton, at times tending to be more disorganised. The secondary fibres may be difficult to distinguish, being without orientation to primary fibres, and are either cored or uncored. More prominent are long, thin vermiform tertiary fibres which branch and rejoin, creating a tangled network of fine fibres. These vermiform fibres meander throughout the sponge without any apparent orientation. The consistency is coarse and flexible.

 

ID Keys

See Subfamily Phyllospongiinae Diagnosis

 

History of changes

Note that this list may be incomplete for dates prior to September 2013.
Published As part of group Action Date Action Type Compiler(s)
03-Mar-2022 DEMOSPONGIAE Sollas, 1885 10-Aug-2021 MODIFIED
29-Mar-2018 15-Dec-2011 MOVED
29-Mar-2018 13-Apr-2011 MODIFIED
12-Feb-2010 (import)