identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
A536878FFFD1FFD0FF7E6B82B656FAC4.text	A536878FFFD1FFD0FF7E6B82B656FAC4.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Nannastacidae Bate 1866	<div><p>Family NANNASTACIDAE Bate, 1866</p><p>Marmacuma Artüz &amp; Sakınç, gen nov.</p><p>LSID. urn:lsid:zoobank.org:act: D96F213B-61E0-493E-B4CA-213230F8604E</p><p>(Figure 2)</p><p>Type species: Marmacuma samimei sp. nov., by monotypy.</p><p>Diagnosis: Based on a fossil carapace with characteristics of the family Nannastacidae Bate, 1866, which differs by tubercles, spines and continuously strong serration on anterolateral, lateral, and posterolateral margins of carapace from the other genera of the family.</p><p>Description. The material studied consists of twenty-one specimens collected in a period of two years from five localities (Figure 1) in the Upper Pleistocene sediments in the Sea of Marmara. Most of the specimens represent parts of the carapace, except for one nearly complete carapace. In all specimens no ventral structures are present nor are there any indications of the pleon and pleopods. This is not surprising when one considers that generally modern cumaceans have abdomens that are less calcified than the cephalothorax.</p><p>Carapace with pronounced anterolateral processes, with numerous blunt or acute tubercles and spines. Anterolateral, lateral, and posterolateral margins of carapace are strongly serrated.</p><p>Etymology. The generic name refers to the location of the sediments from which the specimens were collected, coupled with the generic name Cumacea .</p><p>Species. Type species only.</p><p>Geographic and geologic distribution.</p><p>Specimens referred to this taxon were recorded as been collected from five localities.</p><p>The holotype, LA60-001.00, and paratypes, LA60-001.01and LA60-001.02, were collected at locality 40°45.167’N / 027°32.850’E (Station A-2), off Uçmakdere, in the sediment core sample from western deep basin (Tekirdağ Basin), at the depth of 1100 m, on August 2009, in the Sea of Marmara.</p><p>Paratypes, AK14-009.00 and DG20-005.00, were collected at locality 40°43.300’N / 029°21.233’E (Station 1), in the sediment core sample from the entrance of the İzmit Bay, at the depth of 90 m, on August 2008 in the <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=29.353884&amp;materialsCitation.latitude=40.72167" title="Search Plazi for locations around (long 29.353884/lat 40.72167)">Sea of Marmara</a>.</p><p>Paratypes, AK21-006.00; AK26-006.00 and AK26-006.01, were collected at locality 40°44.000’ N / 028°00.000’E (Station 2), in the sediment core sample from north off the Kapıdağ Peninsula, at the south part of the Tekirdağ Basin, at the depth of 1042 m, on August 2008, in the <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=28.0&amp;materialsCitation.latitude=40.733334" title="Search Plazi for locations around (long 28.0/lat 40.733334)">Sea of Marmara</a>.</p><p>Paratypes, LA14-002.00; LA14-002.01; LA14-002.02; LA16-003.00; LA18-004.00; LA18-004.01; LA18- 004.02; LA20-004.00; LA20-004.01and LA20-004.02, were collected at locality 40°46.767’N / 027°26.983’E (Station 6), in the sediment core sample from off Tekirdağ, (western deep basin), at the depth of 1100 m, on August 2008, in the <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=27.449717&amp;materialsCitation.latitude=40.77945" title="Search Plazi for locations around (long 27.449717/lat 40.77945)">Sea of Marmara</a>.</p><p>Paratype, LA44-001.00, was collected at locality 40°33.017’N / 027°15.367’E (<a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=27.256117&amp;materialsCitation.latitude=40.55028" title="Search Plazi for locations around (long 27.256117/lat 40.55028)">Station</a> 7), in the sediment core sample from the connection of <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=27.256117&amp;materialsCitation.latitude=40.55028" title="Search Plazi for locations around (long 27.256117/lat 40.55028)">Dardanelles</a> with the Sea of Marmara, (on the shelf between Karabiga and Şarköy), at the depth of 92 m, on August 2008, in the Sea of Marmara .</p><p>Geologic range. Based on the new fossils (present study), the Geologic Range of Nannastacidae is Upper Pleistocene to present.</p></div>	https://treatment.plazi.org/id/A536878FFFD1FFD0FF7E6B82B656FAC4	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Artüz, M. Levent;Sakinç, Mehmet	Artüz, M. Levent, Sakinç, Mehmet (2020): Marmacuma samimei gen. et sp. nov., (Peracarida; Cumacea; Nannastacidae) from Tarantian (Upper Pleistocene) sediments from the Sea of Marmara, Turkey. Zootaxa 4718 (1): 134-144, DOI: 10.11646/zootaxa.4718.1.11
A536878FFFD7FFD3FF7E69EEB5F1FEF5.text	A536878FFFD7FFD3FF7E69EEB5F1FEF5.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Marmacuma samimei Artuz & Sakinc 2020	<div><p>Marmacuma samimei Artüz &amp; Sakınç, sp. nov.</p><p>LSID. urn:lsid:zoobank.org:pub: D6A3604A-89BC-4277-8EB8-43407CF98CA6</p><p>(Figures 2–3)</p><p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>Gender. Unknown.</p><p>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.</p><p>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.</p></div>	https://treatment.plazi.org/id/A536878FFFD7FFD3FF7E69EEB5F1FEF5	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Artüz, M. Levent;Sakinç, Mehmet	Artüz, M. Levent, Sakinç, Mehmet (2020): Marmacuma samimei gen. et sp. nov., (Peracarida; Cumacea; Nannastacidae) from Tarantian (Upper Pleistocene) sediments from the Sea of Marmara, Turkey. Zootaxa 4718 (1): 134-144, DOI: 10.11646/zootaxa.4718.1.11
