Marmacuma samimei gen. et sp. nov., (Peracarida; Cumacea; Nannastacidae) from Tarantian (Upper Pleistocene) sediments from the Sea of Marmara, Turkey Author Artüz, M. Levent Author Sakinç, Mehmet text Zootaxa 2020 2020-01-03 4718 1 134 144 journal article 24444 10.11646/zootaxa.4718.1.11 91e73266-88bc-459f-a807-77033bed6596 1175-5326 3602189 0F32B144-CABB-4FED-B528-5F2F7954AAC6 Marmacuma samimei Artüz & Sakınç , sp. nov. LSID. urn:lsid:zoobank.org:pub: D6A3604A-89BC-4277-8EB8-43407CF98CA6 ( Figures 2–3 ) Material examined. Holotype : LA60-001.00 ( Figure 2 A, B ); 20 Paratypes : AK14-009.00; DG20-005.00; AK21- 006.00; AK26-006.00; AK26-006.01( Figure 2 D ); AK26-006.02; AK29-003.00 ( Figure 2 E, F ); LA60-001.01; LA60-001.02; LA14-002.00; LA14-002.01; LA14-002.02; LA16-003.00 ( Figure 2 C ); LA18-004.00; LA18-004.01; LA18-004.02; LA20-004.00; LA20-004.01; LA20-004.02; LA44-001.00. All same data as holotype. Diagnosis . Carapace 1.3 times as long as high, 1.3 times as long as wide; ocular lobe present; mid-dorsal carina absent; dorsally 5–7 pairs of spines directed anteriorly; posterior single pair of posteriorly directed spines; both anterolateral, lateral and posterolateral margins serrated; pseudorostrum prominent. Description. Holotype LA60-001.00: Carapace (TL 949.2 μm; CL716.4; CW 552.1 μm and CH 554 μm) ( Figure 2 ) 1.3 times as long as high, 1.3 times as long as wide; ocular lobe present; mid-dorsal carina absent, domelike dorsally, more elevated in the middle, posterior part slightly excavated, anterior flattened; regular and sparsely scattered, densely covered with small acute tubercles and small pits, and numerous spines with a large anteriorly directed postocular spine on pseudorostral lobe; dorsally 5–7 pairs of spines directed anteriorly; posterior single pair of posteriorly directed spines; both anterolateral, lateral and posterolateral margins serrated, anterolateral margin with 28–32 notches on each side; serration on anterolateral margin directed forward; pseudorostrum one-third the carapace length, base width 1.4 times and tip width 5.4 times in length, prominent, obliquely directed, carinate, tip with couple of spines; single pair of forward directed medium sized spins laterally located, one-third of the base of pseudorostrum. Thorax, pleon, and appendages are unknown. Measurements of the carapace are given in Table 2 and the ornamentation of the carapace is shown in Figure 3 . FIGURE 3A. The cephalothorax of Marmacuma samimei gen. et sp. nov. , showing the position and orientation of measurements given in Table 2. dorsal view FIGURE 3B. The cephalothorax of Marmacuma samimei gen. et sp. nov. , showing the position and orientation of measurements given in Table 2. lateral view. TABLE 2 Measurements (μm) taken on holotype and selected paratypes of Marmacuma samimei gen. et sp. nov. (L 1 ) total length including pseudorostrum: (L 2 ) length of pseudorostrum; (L 3 ) Carapace length excluding pseudorostrum; (W 1 ) Carapace width; (W 2 ) Width of carapace on fronto-orbital; (W 3 ) Pseudorostral base width; (W 4 ) Pseudorostral apex width; (W 5 ) Carapace height. Positions and orientation of measurements are illustrated in Figure 3. * Holotype of Marmacuma samimei gen. et sp. nov.
Specimen Measurements
LA60-001.00* L1 949.2 L2 232.8 L3 716.4 W1 552.1 W2 412.2 W3 166.2 W4 43.2 W5 554.0
LA16-003.00 938.1 230.1 708.0 545.6 407.3 164.2 42.7 547.5
AK29-003.00 951.3 233.3 718.0 553.3 413.1 166.5 43.3 555.2
AK21-006.00 - 231.4 712.1 - - - - 552.4
LA14-002.01 948.3 232.6 715.7 551.6 411.9 166.0 43.2 553.5
LA44-001.00 948.1 232.5 715.6 551.5 411.7 166.1 43.1 553.3
Remarks. No other body fragments and/or other species belonging to this order were found in any of the sediment core samples studied within the MAREM project (N= 51) throughout the Sea of Marmara. In addition, no extant specimen was found during the numerous biodiversity samples from the same localities performed between 2008 and 2018 . Gender. Unknown. Etymology. The trivial name honours Prof. Dr. F. Samime Artüz, geologist and preeminent sediment specialist and primary author of studies on petrography and palynology around Turkey . The specific name is a noun in the genitive singular. Localities. Sea of Marmara, ( 34° 00.000’ N– 029° 55.050’ E / 41° 20.000’ N– 025° 00.000’ E ) with an approximately depth of 800–1200 m at the Upper Pleistocene.