Cassiopea cf. maremetens, Gershwin, Zeidler & Davie, 2010

Keable, Stephen J. & Ahyong, Shane T., 2016, First Records of the Invasive “ Upside-down Jellyfish ”, Cassiopea (Cnidaria: Scyphozoa: Rhizostomeae: Cassiopeidae), from Coastal Lakes of New South Wales, Australia, Records of the Australian Museum 68 (1), pp. 23-30: 26-28

publication ID

http://doi.org/ 10.3853/j.2201-4349.68.2016.1656

persistent identifier

http://treatment.plazi.org/id/03F7880E-A51B-FFD9-E0F2-19A9FA62FB0D

treatment provided by

Carolina

scientific name

Cassiopea cf. maremetens
status

 

Cassiopea cf. maremetens  

Gershwin, Zeidler & Davie, 2010

Figs 2 View Figure 2 E–H, 3C, 4E,F

Material examined. AM G.18137, 1 specimen, in channel splitting Godwin Island approximately one third distance from southern shore, Breckenridge Channel, Wallis Lake, New South Wales, Australia, 32°11'45"S 152°29'56"E GoogleMaps   , R. Pearce , 15 August 2014   . AM G.18138, 1 specimen, collection data as for G.18137   . AM G.18139, 11 specimens, collection data as for G.18137   . AM G.18143–18155, single specimens; AM G.18156, 13 specimens, Pipers Creek , behind Smugglers Cove Caravan Park, Wallis Lake, New South Wales, Australia, 32°12'00"S 152°30'39"E GoogleMaps   , R. Pearce , 18 September 2014   . AM G.18181–18183, 4 specimens, inlet on south east side of Mather Island , Wallis Lake, New South Wales, Australia, 32°11'26"S 152°29'36"E, S. J. Keable & A. D. Hegedus, 28 April 2015 GoogleMaps   . AM G.18184, 1 specimen, Pipers Creek within Smugglers Cove Caravan Park, Wallis Lake, New South Wales, Australia, 32°11'58"S 152°30'39"E, S. J. Keable & A. Murray, 30 April 2015 GoogleMaps   . Bell diameter 35 mm ( AM G.18182) to 210 mm ( AM G.18139)   .

Comparative material of C. maremetens   . QM G6645, 3 paratypes (110–130 mm), Mud Island, Moreton Bay , Queensland, C. Wallace, 8 April 1972   .

Remarks. The Wallis Lake specimens appear to be closest to C. maremetens Gershwin, Zeidler & Davie, 2010   , from Queensland ( Figs 2 View Figure 2 I–L, 3D) (type locality, Lake Magellan, southwest of Caloundra, 26°49'42"S 153°06'48.6"E), with which they agree in most respects including exumbrella conformation, branching pattern of the oral tentacles and the numbers of rhopalia (19–21) ( Gershwin et al., 2010). The material from Wallis Lake ( Fig. 2G View Figure 2 ) agrees with type material of C. maremetens   (QM G6645; Fig. 2K View Figure 2 ), and most noticeably differs from the Lake Illawarra specimens ( Fig. 2C View Figure 2 ), in having alternating (i.e., non-opposing) rather than pinnate lateral branches along the length of the oral arms and lacking a distinct subequal bifurcation just distal to the midpoint of the primary arm. They differ, however, from both C. maremetens   sensu stricto and C. ndrosia   in the presence of numerous, large, conspicuous vesicles along the length of these arms (compare Fig. 2H View Figure 2 and Fig. 2D View Figure 2 [ C. ndrosia, Lake Illawarra   ] and Fig. 2L View Figure 2 [ C. maremetens   ]). The vesicles are variably leaf shaped (generally slightly broader in the distal half, maximum width approximately one-third length), and generally as wide as the lateral arm branches. The presence of the numerous large vesicles on the oral arms is the most significant distinction between the Wallis Lake specimens and C. maremetens   sensu stricto, which has few or no vesicles. Gershwin et al. (2010), however, noted they could not adequately assess the significance of the presence or absence of vesicles in their material, whether a polymorphism or indicative of an additional unrecognized species. Just as Gershwin et al. (2010) observed no correlation between body size and presence of vesicles on the oral arms in C. maremetens   , the vesicles in the Wallis Lake specimens are similarly numerous across the size range.

Significantly, our Wallis Lake specimens also differ from the description of C. maremetens   in the lappet shape and arrangement ( Fig. 3 View Figure 3 C–D). Ocelli are present in the Wallis Lake specimens, absent in C. maremetens   . The margin of the parameres in the Wallis Lake specimens are sinuous, resulting in 4–5 low, rounded lobes ( Fig. 3C View Figure 3 ). In contrast, the lappets of C. maremetens   are reported as square and deeply incised, with four per paramere ( Gershwin et al., 2010). Close examination of paratypes of C. maremetens   , however, revealed the squared, apparently deep incisions are bridged by transparent exumbrella membrane ( Fig. 3D View Figure 3 ). Thus, instead of being deeply incised, the outline of the lappets of C. maremetens   (at least in the paratypes examined) is actually essentially sinuous and indistinctly lobate, much like that of C. ndrosia   . The lappets in the Wallis Lake material differ from C. maremetens   in having a more strongly sinuous margin with more numerous lobes per paramere. The differences in lappet shape and vesicle complement in comparison to C. maremetens   suggest that the Wallis Lake specimens may represent a separate, possibly undescribed species. Pending further study, however, we tentatively identify our material as C. cf. maremetens   to highlight its similarity to C. maremetens   . Cassiopea maremetens   sensu stricto is presently known from Bentinck Island, Gulf of Carpentaria, Queensland (c. 17°03'34"S 139°29'09"E) to Moreton Bay on the Queensland east coast (27°48'S 153°24'E). Reports of C. andromeda   from Southport, Queensland (27°58'S 153°25'E), just south of Moreton Bay, may also represent C. maremetens ( Gershwin et al., 2010)   .

The original collector of Cassiopea cf. maremetens   from Wallis Lake first observed these jellyfish “in their hundreds” in Pipers Creek in 2009. The 2014 outbreak in the vicinity of Godwin Island (reported as “in large numbers within a small area”), documented here with specimens, was noticed on or near 2 August 2014 although specimens were not collected until 15 August 2014. Specimens of C. cf. maremetens   were obtained again from the same location in Pipers Creek in September 2014.

Subsequent fieldwork in Wallis Lake in April 2015 confirmed the continued presence of C. cf. maremetens   in Pipers Creek ( Fig. 4B View Figure 4 ) and at a third locality within the lake adjacent to the shore at Mather Island ( Fig. 4C View Figure 4 ). A 75 m transect line was placed randomly along the shoreline in both these locations and Cassiopea   within 1 m of the shore along this distance were counted. Five randomly selected individuals from each transect were also measured for bell diameter.At Pipers Creek, 30 individuals were present along the transect, the bell diameter of the individuals measured ranged from 120 to 210 mm ( Fig. 4D View Figure 4 ) with a mean of 170 mm. At Mather Island 24 individuals were present along the transect, those measured ranged in size from 40–70 mm with a mean of 53 mm. Distribution of Cassiopea   appeared patchy. Outside the transects, dense aggregations were observed ( Fig. 4E,F View Figure 4 ) with up to 35 per square metre at Mather Island. A water temperature of 21.5°C and a salinity of 28.7 parts per thousand was recorded during the Mather Island transect and a salinity of 12.1 parts per thousand at Pipers Creek. Cassiopea   were observed lying with the aboral surface resting on very soft sediment in depths of 10–100 cm.

AM

Australian Museum

R

Departamento de Geologia, Universidad de Chile

QM

Queensland Museum