Turrispirillina Karasikensis (n. sp.) and Turrispirillina Pervesleri (n. sp.) Associated with Large Sponges on the Gakkel Ridge (Arctic Ocean)

2020 ◽  
Vol 50 (2) ◽  
pp. 174-181
Author(s):  
Patrick Bukenberger ◽  
Petra Heinz ◽  
Jutta E. Wollenburg

ABSTRACT Here we describe two new species of the genus Turrispirillina associated with large siliceous sponge reefs on the Karasik Seamount (Gakkel Ridge, Arctic Ocean). Careful analysis of Rose Bengal-stained samples and observations on untreated frozen sponge material revealed both species live exclusively inside siliceous sponges of the genus Geodia. More detailed information on the intra-sponge habitat was obtained from untreated frozen sponge material that showed both Turrispirillina species attach themselves to the large megascelere spicules that stabilize the choanoflagellates-harbouring subcortical crypts situated under the thick sponge cortex. Unstained specimens of both species were very abundant in the sediments surrounding the sponge. The number of Rose Bengal-stained specimens in each sample obviously depended on the penetration of a Geodia sponge, likely also the exact position of penetration with respect to the sponge. As sexual and asexual generations are observed in both taxa and sampling took place in autumn, opportunistic behavior with rapid reproduction following the spring bloom may determine the standing stock of both species. These are the first Arctic Turrispirillina species described with pseudospines.

2002 ◽  
Vol 182 (2-4) ◽  
pp. 227-235 ◽  
Author(s):  
Eric Hellebrand ◽  
Jonathan E Snow ◽  
Richard Mühe

1991 ◽  
Vol 190 (1) ◽  
pp. 95-108 ◽  
Author(s):  
R.K. Mühe ◽  
H. Bohrmann ◽  
P.K. Hörmann ◽  
J. Thiede ◽  
P. Stoffers
Keyword(s):  

2002 ◽  
Vol 76 (3) ◽  
pp. 565-569 ◽  
Author(s):  
Brian R. Pratt

The fossil record of siliceous sponges—Hexactinellida and demosponge “Lithistida”—hinges upon both body fossils plus isolated spicules mostly recovered from limestones by acid digestion. The earliest record of siliceous sponge spicules extends back to the late Neoproterozoic of Hubei, southern China (Steiner et al., 1993) and Mongolia (Brasier et al., 1997), and body fossils attributed to the hexactinellids have been described from the Ediacaran of South Australia (Gehling and Rigby, 1996); thus they are the oldest-known definite representatives of extant animal phyla. The Early Cambrian saw a remarkable diversification in spicule morphology, with the appearance of an essentially “modern” array of forms (Zhang and Pratt, 1994). While a diversity decline may have occurred with the late Early Cambrian extinction(s), the subsequent Paleozoic and Mesozoic fossil record of spicules shows a relatively consistent range of morphologies (e.g., Mostler, 1986; Bengtson et al., 1990; Webby and Trotter, 1993; Kozur et al., 1996; Zhang and Pratt, 2000). However, because spicule form is not restricted to individual taxa and many sponge species secrete a variety of spicule shapes, it is difficult to gauge true siliceous sponge diversity and to explore their biostratigraphic utility using only isolated spicules.


2009 ◽  
Vol 283 (1-4) ◽  
pp. 122-132 ◽  
Author(s):  
Chuan-Zhou Liu ◽  
Jonathan E. Snow ◽  
Gerhard Brügmann ◽  
Eric Hellebrand ◽  
Albrecht W. Hofmann

2021 ◽  
pp. 229186
Author(s):  
Yumiko Harigane ◽  
Katsuyoshi Michibayashi ◽  
Tomoaki Morishita ◽  
Akihiro Tamura ◽  
Satoshi Hashimoto ◽  
...  

2021 ◽  
Author(s):  
Bianca Lintner ◽  
Michael Lintner ◽  
Jutta Wollenburg ◽  
Erik Wurz ◽  
Petra Heinz

<p><span>This is the first study on the interactions between foraminifera and sponges. Although </span><span><em>Cibicides</em></span><span> and </span><span><em>Hyrrokin</em></span><span> are regarded as parasites on siliceous sponges, it is not yet clarified whether foraminifera specifically colonize sponges or are accidentally sucked in during the pelagic stage. To better elucidate these relationships, 12 sponges of different genera were examined and their foraminiferal communities analyzed. In 2018, the sponges for this study were collected with a ROV in water depths of 223 to 625 m in the Norwegian-Greenland Sea. Sponge parts were preserved in ethanol (96 %) and stained with Rose Bengal (2g l</span><sup><span>-1</span></sup><span>) to allow a differentiation between the living and dead foraminiferal fauna. </span></p><p><span>Each sponge sample contained several hundred live and dead foraminiferal individuals of up to 60 different species. Even on </span><span><em>Geodia baretti,</em></span><span> which is able to release barettin to avoid colonalisation of other organisms, few foraminiferal individuals were observed. On all sponges, the most abundant genus was </span><span><em>Cibicides, </em></span><span>with</span><span><em> Cibicides lobatulus</em></span><span> and</span><span><em> Cibicides refulgens </em></span><span>as the most common taxa. Other very common species were </span><span><em>Discorbinella bertheloti</em></span><span> or </span><span><em>Epistominella nipponica</em></span><span>. Also, </span><span><em>Hyrrokkin</em></span> <span><em>sarcophaga</em></span><span> was found on different sponges and following its lifestyle, penetrating the sponge surfaces. The fact that besides adult foraminifera splendid juvenile stages were found indicate that foraminifera reproduced while inside the sponges. This reproduction might be stimulated/triggered by enhanced food availability by the pumping sponge.</span></p><p><span>In summary, sponges are a special habitat for a high number of foraminiferal taxa. Their interaction ranges from parasitic lifestyle up to reproduction purposes. All these aspects highlight the importance of foraminifera-sponge interactions.</span></p>


Sign in / Sign up

Export Citation Format

Share Document