Guancha, MIKLUCHO-MACLAY, 1868
publication ID |
https://doi.org/ 10.1111/j.1096-3642.2006.00221.x |
persistent identifier |
https://treatment.plazi.org/id/038E87EA-634E-1C4D-FF26-5F6E755BFADB |
treatment provided by |
Felipe |
scientific name |
Guancha |
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GUANCHA View in CoL MIKLUCHO- MACLAY, 1868
Type species: Guancha blanca Miklucho-Maclay, 1868 . Clathrinidae with a cormus composed of a peduncle and a clathroid body. The peduncle may be formed by true tubes with a normal choanoderm, or may be solid with a special skeleton. The skeleton is composed of regular (equiangular and equiradiate) spicules to which parasagittal spicules may be added, at least in the peduncle. In some species, only parasagittal spicules are present. The unpaired actine of parasagittal spicules is always basipetally orientated.
Remarks on Guancha
Prior to this work, the genus was represented by ‘about six’ species ( Borojevic et al., 2002). Species within the genus Guancha display a progressive dif- ferentiation into a clathroid body and a peduncle. In the more simple species, such as G. arnesenae sp. nov., G. blanca Miklucho-Maclay, 1868 and G. sagittaria ( Haeckel, 1872) , the peduncle is composed of normal tubes with a complete choanoderm. G. blanca is only slightly different from a typical Clathrina , and only the fact that it represents the starting point for an evolutionary line makes it possible to separate it into a distinct genus ( Borojevic & Peixinho, 1976). In more morphologically complex species such as Guancha challengeri ( Poléjaeff, 1883) , G. lacunosa ( Johnston, 1842) and G. pulcherrima (Dendy, 1891) the peduncle acquires a solid form, consequently with no choanoderm, and with a particular skeleton. Guancha is also characterized by possessing parasagittal triactines organized in a parallel manner with the unpaired actine basipetally orientated. In G. blanca the parasagittal spicules are found in the peduncle only, whereas in species such as G. arnesenae sp. nov., G. tetela Borojevic & Peixinho, 1976 and G. sagittaria all the spicules are parasagittal.
The classification of Guancha is especially difficult when the skeleton is composed of more-or-less uniform spicules with only slightly longer unpaired actine in the peduncular triactines. G. blanca has been reported from most oceans, from the littoral zone to the abyssal plains ( Barthel & Tendal, 1993; Janussen, Rapp & Tendal, 2003). Cosmopolitanism is very rare among sponges ( Klautau et al., 1999), and in the closely related Clathrina the use of statistical analyses of shape, size and distribution of spicules, combined with molecular methods, have shed new light on the classification of the genus, and have revealed that geographical distribution of the different species is more restricted ( Klautau et al., 1994; Wörheide & Hooper, 1999; Rapp et al., 2001; Klautau & Valentine, 2003). In agreement with Borojevic et al. (2002), I consider that G. ‘ blanca ’ represents a complex of species, and that the ongoing work revising the genus, including analysing specimens of G. ‘ blanca ’ from different geographical regions and from shallow to abyssal depths with a morphological and molecular approach, will reveal a number of new species.
GUANCHA ARNESENAE SP. NOV.
( FIGS 13A, B View Figure 13 , 14 View Figure 14 , TABLE 7)
Type locality: Evenskjer, 68°35′N, 16°35′E, 25 m.
Holotype: VM-398 , Evenskjer, 68°35′N, 16°35′E, 25 m, 18.08.1919, 1 specimen. GoogleMaps
Paratype: TM-183, Ramfjorden, 10–20 m, 14.07.1921, 1 specimen.
Etymology: Named in memory of the Norwegian spongiologist Emily Arnesen (1867–1928).
Previous records: None.
Additional material examined: 28 specimens.
IB. Evenskjer, 68°35′N, 16°35′E, 25 m, 18.08.1919, 2 specimens GoogleMaps . TMU. TM-150, Ramfjorden, 69°33′N, 10°10′E, 10–20 m, 14.07.1921, c. 10 specimens (small and fragmentary) GoogleMaps . VM. VM-16904 , Tromsø, 69°40′N, 19°00′E, 30–35 m, 28.10.1916, 1 specimen GoogleMaps . VM-16905 , Tromsø, 69°40′N, 19°00′E, 30 m, 21.09.1917, 1 specimen GoogleMaps . VM-16906 , Gibostad, 69°21′N, 18°05′E, 50 m, 23.05.1912, 4 specimens (dry) GoogleMaps . VM-16907 , Lødingen, 68°24′N, 15°58′E, 70–90 m, 22.08.1913, 1 specimen (dry) GoogleMaps . ZMO. B-1289, Balsnes, 69°34′N, 18°52′E, 40– 60 m, 9 specimens GoogleMaps .
Description
Clathrinidae with a cormus normally composed of a clathroid cormus of irregularly and loosely anastomosing tubes and a peduncle. Size ranging from 4 to 10 mm in height. Several true tubes with a normal choanoderm form the peduncle. The peduncular tubes run in parallel, sometimes free, or slightly anastomosed. In specimens without a proper peduncle the cormus is narrower at the base than in the apical region. Water-collecting tubes converge at the centre of the sponge, ending in one or several apical oscula. The single tubes are about 0.5 mm in diameter. Colour is light beige in alcohol and when dried. Texture soft. The skeleton of the cormus is solely composed of tripodic, parasagittal triactines. The spicules are irregularly orientated in several layers in the walls of the tubes, resulting in a wall thickness of about 30–50 µm. In the peduncle the skeleton consists of tripodic parasagittal triactines, generally similar to those in the cormus, but with shorter paired actines. In addition, there are very characteristic parasagittal triactines where the paired actines are bent, forming a concave ‘U’. Spicules in the peduncle with their unpaired actine basipetally orientated. All the actines are straight, cylindrical and with blunt tips.
Distribution
The species is found in the northern part of Norway at 10–90 m depth.
The species is also known from Greenland at 30– 54 m depth (my unpubl. data).
Remarks
The species is very similar to Guancha sagittaria Haeckel, 1872 . However, there are some differences. Haeckel (1872) made his original description based on three very small olynthus tubes, dredged from Storebaelt ( Denmark) during the Pommerania- Expedition in 1871, probably representing very young specimens. All the specimens examined here have clathroid cormi, and a more-or-less developed peduncle. Both species have the typical shape of the parasagittal triactines from the peduncle, but whereas all spicules are cylindrical in G. arenesenae they are conical in G. sagittaria ( Haeckel, 1872) . The presence of only parasagittal triactines in G. arnesenae differentiates it from all other species of Guancha except Guancha tetela Borojevic & Peixinho, 1976 from Brazil. However, G. arnesenae and G. tetela are easily distinguished by the shape of the paired actines of the parasagittal triactines from the peduncle, forming a concave ‘U’ in arnesenae and close to a ‘T’ in tetela .
GUANCHA BLANCA MIKLUCHO- MACLAY, 1868
( FIGS 15A–D View Figure 15 , 16 View Figure 16 , TABLE 8)
Original description: Guancha blanca Miklucho- Maclay, 1868: 221–232, plates 4 and 5.
Synonyms and citations
Ascetta blanca View in CoL ( Hansen, 1885: 20; Arnesen, 1901a: 9–10).
Clathrina blanca ( Ereskowsky, 1995: 730) View in CoL .
Guancha blanca View in CoL ( Borojevic & Boury-Esnault, 1987: 14–15; Borojevic et al., 1990: 252; Barthel & Tendal, 1993: 84; Rapp, 1999: 65–71; van Soest, 2001: 101; Borojevic et al., 2002: 1143–1144; Janussen et al., 2003: 17–19).
Leucosolenia blanca View in CoL ( Levinsen, 1886; Breitfuss, 1898a: 105–106, 1898b: 13–14, 1898c: 295–296, 1911: 224; Derjugin, 1915: 289; Breitfuss, 1927: 27, 1933: 240, 1936: 5; Alander in Jägerskiöld, 1971: 60).
Leucosolenia lacunosa ( Burton, 1930b: 488) .
Leucosolenia macleayi ( Burton, 1930a: 14–17, 1930b: 487; Arndt, 1935: 8–9).
Type locality: Lanzarote, Canary Islands.
Holotype: The type is probably lost (A. Plotkin, ZIL, pers. comm.).
Previous records: Bergen and Stavanger ( Burton, 1930b; as L. macleayi ); Singlefjord ( Breitfuss, 1936).
Additional material examined: 147 specimens.
IB. Skarnsundet, 63°53′N, 11°04′E, 200 m, 09.10.1968, 3 specimens GoogleMaps . Trondheimsfjord, c. 63°30′N, 10°30′E, 35 different localities, 14–500 m, 1995–96, 126 specimens. Nord-Leksa, 63°35.9′N, 09°26.3′E, 150–200 m, 21.03.1996, 2 specimens. Korsfjord, 60°09.12′N, 05°08.52′E, 300 m, 12.02.2003, 1 specimen. Balsnes, 69°34.1′N, 18°52′E, 40–60 m, 1 specimen. TMU. TM-180, Beiarn, 67°04′N, 14°35′E, 35–45 m, 02.08.1955, 2 specimens GoogleMaps . TM-181, Trondenes, Vågsfjord, 68°50′N, 16°35′E, 90–150 m, 28.08.1954, 2 specimens. VM. VM-16893 , Bjarkøy, 68°58′N, 16°42′E, 60–90 m, 07.09.1912, 2 specimens GoogleMaps . VM-16894 , Bjarkøy, 68°58′N, 16°42′E, 30–60 m, 06.09.1912, 1 specimen GoogleMaps . VM-16895 , Varanger, 70°05′N, 29°30′E, 160–170 m, 18.07.1937, 1 specimen GoogleMaps . VM-16896 , Traenfjorden, 66°25′N, 12°15′E, 40 m, 18.07.1939, 1 specimen GoogleMaps . VM-16897 , Mefjaera, Vågsfjord, 68°55′N, 16°55′E, 150–200 m, 06.07.1933, 2 specimens GoogleMaps . VM- 16898 , Gibostad, 69°21′N, 18°05′E, 40 m, 20.07.1917, 1 specimen (dry) GoogleMaps . VM-16899 , Vaerøy, 67°40′N, 12°40′E, littoral, 03.06.1929, 1 specimen GoogleMaps . ZMO. B-1287, Håka, Oslofjord, 16.09.1953, 1 specimen . B-1288, Tromsø, 69°40′N, 19°00′E, 2 specimens.
Description
Clathrinidae with a cormus normally composed of a clathroid cormus of regularly and tightly anastomosing tubes and a peduncle. Up to 2 cm in height and 2 cm in diameter. One or several true tubes with a normal choanoderm form the peduncle. Sometimes the peduncle is very short or absent. In specimens without a peduncle the cormus is often narrower at the base than in the apical region. Water-collecting tubes converge at the centre of the sponge, ending in one or sometimes several apical oscula. The single tubes are about 0.3–0.7 mm in diameter. Surface is smooth. Colour white, greyish white or beige when alive, and with almost the same colours in alcohol. Dried specimens usually light beige. The skeleton of the cormus is composed of regular (equiangular and equiradiate) triactines to which parasagittal spicules may be added. The spicules are irregularly orientated in several layers in the walls of the tubes, resulting in a wall thickness of about 80 µm. In the peduncle the skeleton consists of only parasagittal triactines, with the unpaired actine basipetally orientated. All the actines are straight, cylindrical and with blunt tips.
Distribution
The species is found along the entire Norwegian coast from littoral to 500 m depth. G. blanca is the only species among the Norwegian Calcinea that is reported to be common in abyssal depths in the North Atlantic ( Barthel & Tendal, 1993; Janussen et al., 2003). However, recent examination of material from the abyssal Norwegian Sea revealed that these deep records probably represent another new species of Guancha (H. T. Rapp & O. S. Tendal, unpubl. data).
Remarks
In the reticulate/cushion-shaped form the parasagittal spicules are not as numerous, and the unpaired actine is usually shorter than in the pedunculated form. However, parasagittal triactines are always present, also in the young olynthus. The high degree of morphological variation figured by Miklucho-Maclay has previously been questioned ( Burton, 1930a, b). However, material from Trondheimsfjord support some of Miklucho-Maclay’s observations, and the variation is assumed to be mainly due to different life stages of the sponges.
The species has previously been reported from Trondheim and Stavanger ( Burton, 1930b). In his work on the calcareous sponges from the Siboga- Expedition, Burton (1930a) decided to include all species of Guancha (Leucosolenia) with a clathroid cormus (except G. lacunosa ) in Guancha macleayi ( Von Lendenfeld, 1885) , a species originally described from Australia. He retained only Miklucho-Maclay’s olynthus-form as the true Guancha blanca , and the consequence was a cosmopolitan distribution of G. macleayi , a conclusion that has never been supported by later authors. Re-examination of Burton’s specimens from the Norwegian coast revealed that they should be identified as G. blanca .
GUANCHA CAMURA SP. NOV.
( FIGS 17A–C View Figure 17 , 18 View Figure 18 , TABLE 9)
Type locality: Østerbotn , Porsanger, north-east Norway at 70°15.1′N, 25°21.1′E GoogleMaps .
Holotype: TMU-185 , Østerbotn, Porsanger, 70°15.1′N, 25°21.1′E, 27–33 m, 14.08.1956. GoogleMaps
Paratype: TMU-184 , Bøkfjord, 69°52.2′N, 29°38.5′E, 50–90 m, 25.06.1937, 1 specimen GoogleMaps .
Etymology: From ‘camur’ (Latin), meaning tortuous or bent, referring to the horn-shaped paired actines of the parasagittal triactines from the peduncle.
Additional material examined: 5 specimens.
TMU. TM-186, Jarfjord, 69°40.7′N, 30°24.7′E, 30–45 m, 03.07.1937, 1 specimen GoogleMaps . VM. VM-16900 , Evenskjer, 68°35′N, 16°35′E, 60–85 m, 12.08.1913, 2 specimens (dry) GoogleMaps . VM-16901 , Gibostad, 69°21′N, 18°05′E, 50 m, 27.07.1917, 1 specimen (dry) GoogleMaps . VM-16902 , Lødingen, 68°24′N, 15°58′E, 35–40 m, 18.08.1913, 1 specimen (dry) GoogleMaps .
Description
Clathrinidae with a cormus normally composed of a clathroid body of irregularly and loosely anastomosing tubes and a peduncle. Up to 3 cm in height and 2 cm wide. Consistency soft because of the very thin walls of the tubes (about 20 µm). Surface smooth. Several true tubes with a normal choanoderm form the peduncle. The skeleton of the cormus is composed of regular (equiangular and equiradiate) triactines to which parasagittal spicules are frequently added. In the peduncle the skeleton consists of only parasagittal triactines. The unpaired actine of peduncular parasagittal triactines is always basipetally orientated. The paired actines are bent in a manner making them ‘horn’-shaped, whereas the unpaired actine is straight. All actines are cylindrical with slightly blunt tips.
Distribution
The species is found in the northern part of Norway at 27–90 m depth.
The species is also known from Greenland at 125– 200 m depth (my pers. observ.).
Remarks
G. camura View in CoL sp. nov. differs from other species mainly because of the horn-shaped parasagittal triactines in the peduncle. Such spicules have been found in the olynthus-form of G. ‘ blanca View in CoL ’ from Neapel ( Metschnikoff, 1879). None of his specimens has been available for examination, but from the distribution of G. camura View in CoL it is reasonable to believe that they represent two different species. These spicules also bear similarities to sagittal tripods found in G. challengeri ( Polejaeff, 1883) from Australia and New Zealand, but in G. challengeri they are found together with tripods, forming conules on the outer surface. G. challengeri also possesses a solid peduncle ( Polejaeff, 1883), whereas the peduncle is composed of true tubes in G. camura View in CoL . The species also bears similarities to G. pellucida View in CoL sp. nov. However, the spicules in G. camura View in CoL are considerably shorter and thicker than the long and slender spicules in G. pellucida View in CoL .
GUANCHA LACUNOSA ( JOHNSTON, 1842) View in CoL
( FIGS 19A–C View Figure 19 , 20 View Figure 20 , TABLE 10)
Original description: Grantia lacunosa Bean in Johnston, 1842: 176.
Synonyms and citations
Ascandra angulata Von Lendenfeld, 1891 .
Ascandra angulata ( Arnesen, 1901a: 13; 1901b: 68). Ascortis lacunosa ( Haeckel, 1872: 70–71) .
Guancha lacunosa View in CoL ( Borojevic & Boury-Esnault, 1987: 15–16; Rapp, 1999: 72).
Leucosolenia angulata ( Breitfuss, 1927: 27) . Leucosolenia lacunosa ( Breitfuss, 1933: 241) .
Type locality: Scarborough, UK.
Holotype: According to Burton (1930a) the type is lost.
Previous records: Hjeltefjorden, Bergen ( Arnesen, 1901a).
Material examined: 2 specimens.
VM. VM-16903 , Finnsnes, 69°14′N, 17°58′E, 25–40 m, 18.06.1914 GoogleMaps , 1 specimen (dry, peduncle broken off and missing). ZMUB. ZMUB-9678 , Hjeltefjorden, Bergen, 60°35 N, 04°55′E, 55–200 m, 1 specimen GoogleMaps .
Description
Sponge composed of an ovoid body of thin, tightly and regularly anastomosing tubes, and a solid peduncle without any choanoderm. Water-collecting tubes converge into one apical osculum. Colour white in ethanol and light beige when dried.
Triactines from the clathroid body range from almost regular to parasagittal with straight actines. Close to the peduncle there are parasagittal spicules with the longest unpaired actine pointing towards the peduncle. The skeleton of the peduncle is composed of large diactines with a break on the middle, and parasagittal triactines with a very long unpaired actine and short paired actines. Irregular diactines of variable sizes are present at low numbers in the peduncle. All actines are cylindrical with slightly blunt to sharp points.
Distribution
From the Norwegian coast, G. lacunosa is only known from Hjeltefjorden in the Bergen area and at Finnsnes in northern Norway, 25–200 m depth.
The species is also reported from the Mediterranean ( Von Lendenfeld, 1891), the Bay of Biscay down to 550 m depth ( Borojevic & Boury-Esnault, 1987), Great Britain ( Ackers et al., 1985) and the Arctic ( Breitfuss, 1911, 1927, 1933; Derjugin, 1915).
Remarks
In his work on the Norwegian sponges from the Norman collection, Burton (1930b) reported Guancha lacunosa from Bergen and Stavanger. Re-examination of these specimens revealed that they should be identified as Guancha blanca and Clathrina nanseni .
GUANCHA PELLUCIDA SP. NOV.
( FIGS 21A–D View Figure 21 , 22 View Figure 22 , TABLE 11)
Type locality: Porsangerfjord , northern Norway, at approximately 70°15′N, 25°21′E GoogleMaps .
Holotype: TMU-179 , Porsangerfjord, approximately 70°15′N, 25°21′E, 140–155 m, 03.08.1931. GoogleMaps
Paratype: VM-397 , Senja, 190 m, 08.07.1933, 1 specimen. No more information given on the original label .
Etymology: Named ‘pellucida’ from Latin ‘pellucidus’, meaning translucent, referring to the very thin-walled and translucent tubes of the cormus.
Additional material examined: 4 specimens. IB. Trondheimsfjord, approximately 63°30′N, 10°30′E, 3 different localities, 100–275 m, 1996, 4 small specimens GoogleMaps .
Description
Clathrinidae normally composed of a globular and highly compressible clathroid cormus of irregularly but tightly anastomosing tubes, and a very short peduncle. Up to 3 cm in height and 2.5 cm in diameter. Several anastomosing true tubes with a normal choanoderm form the peduncle. In full-grown specimens water-collecting tubes converge into one large apical osculum. Texture soft and fragile. Surface smooth. Colour greyish white and highly translucent when alive, and yellowish white in alcohol. The skeleton of the cormus is composed of 1–3 layers of very slender regular to subregular triactines, to which parasagittal spicules may be added. The walls of the tubes are only 10–15 µm thick. In the peduncle the skeleton consists of parasagittal triactines with unpaired actine of highly variable length. The unpaired actine of peduncular parasagittal triactines is always basipetally orientated. All actines are undulated, especially close to the centre of the spicule, cylindrical or slightly conical with blunt tips.
Distribution: The species is found in the northern part of Norway at 100–275 m depth.
The species is also known from Greenland at 20– 190 m depth and close to Jan Mayen at 890 m depth (my pers. observ.).
Remarks
The species bears some similarities to G. camura sp. nov., but is clearly separated by the long, slender and slightly undulated actines.
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Kingdom |
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Phylum |
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Class |
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Order |
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Family |
Guancha
Rapp, Hans Tore 2006 |
Clathrina blanca ( Ereskowsky, 1995: 730 )
Ereskowsky AV 1995: 730 |
Guancha blanca
Janussen D & Rapp HT & Tendal OS 2003: 17 |
Borojevic R & Boury-Esnault N & Manuel M & Vacelet J 2002: 1143 |
van Soest R 2001: 101 |
Rapp HT 1999: 65 |
Barthel D & Tendal OS 1993: 84 |
Borojevic R & Boury-Esnault N & Vacelet J 1990: 252 |
Borojevic R & Boury-Esnault N 1987: 14 |
Guancha lacunosa
Rapp HT 1999: 72 |
Borojevic R & Boury-Esnault N 1987: 15 |
Leucosolenia lacunosa ( Burton, 1930b: 488 )
Burton M 1930: 488 |
Leucosolenia macleayi
Arndt 1935: 8 |
Burton M 1930: 14 |
Burton M 1930: 487 |
Leucosolenia angulata ( Breitfuss, 1927: 27 )
Breitfuss LL 1933: 241 |
Breitfuss LL 1927: 27 |
Ascandra angulata
Arnesen E 1901: 13 |
Arnesen E 1901: 68 |
Haeckel E 1872: 71 |
Leucosolenia blanca
Jagerskiold LA 1971: 60 |
Breitfuss LL 1936: 5 |
Breitfuss LL 1933: 240 |
Breitfuss LL 1927: 27 |
Derjugin KM 1915: 289 |
Breitfuss LL 1911: 224 |
Breitfuss LL 1898: 105 |
Breitfuss LL 1898: 13 |
Breitfuss LL 1898: 295 |
Ascetta blanca
Arnesen E 1901: 9 |
Hansen A 1885: 20 |