WoRMS taxon details

Elasmopus gracilis Schellenberg, 1938

531489  (urn:lsid:marinespecies.org:taxname:531489)

accepted
Species
marine, brackish, fresh, terrestrial
Schellenberg, A. (1938). Litorale Amphipoden des tropischen Pazifiks. <em>Kungliga Svenska Vetenskapsakademiens Handlingar (Ser. 3).</em> 16(6): 1–105.
page(s): 59 [details]  Available for editors  PDF available [request] 
Type locality contained in Tuvaluan Exclusive Economic Zone  
type locality contained in Tuvaluan Exclusive Economic Zone [details]
Depth range Littoral (0 to 30 m)  
Depth range Littoral (0 to 30 m) [details]
Horton, T.; Lowry, J.; De Broyer, C.; Bellan-Santini, D.; Copila?-Ciocianu, D.; Corbari, L.; Costello, M.J.; Daneliya, M.; Dauvin, J.-C.; Fišer, C.; Gasca, R.; Grabowski, M.; Guerra-García, J.M.; Hendrycks, E.; Hughes, L.; Jaume, D.; Jazdzewski, K.; Kim, Y.-H.; King, R.; Krapp-Schickel, T.; LeCroy, S.; Lörz, A.-N.; Mamos, T.; Senna, A.R.; Serejo, C.; Souza-Filho, J.F.; Tandberg, A.H.; Thomas, J.D.; Thurston, M.; Vader, W.; Väinölä, R.; Valls Domedel, G.; Vonk, R.; White, K.; Zeidler, W. (2024). World Amphipoda Database. Elasmopus gracilis Schellenberg, 1938. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=531489 on 2024-03-29
Date
action
by
2010-10-12 07:32:39Z
created

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original description Schellenberg, A. (1938). Litorale Amphipoden des tropischen Pazifiks. <em>Kungliga Svenska Vetenskapsakademiens Handlingar (Ser. 3).</em> 16(6): 1–105.
page(s): 59 [details]  Available for editors  PDF available [request] 
 
 Present  Present in aphia/obis/gbif/idigbio   Inaccurate  Introduced: alien  Containing type locality 
   

From editor or global species database
Depth range Littoral (0 to 30 m) [details]

Remark The material of Myers (1986) appears to be closet to the original description of Schellenberg (1938). The specimens studied by Ledoyer (1967, 1982) have a second article on uropod 3 which indicates that they are a separate unnamed species. Ledoyer (1982) indicates that his material is different to the material studied by Ruffo (1969) from the Red Sea.  [details]