Wang Qianwei, Horne David J, Fan Jiawei, Wen Ruilin, Smith Robin J, Wang Min, Zhai Dayou
Yunnan Key Laboratory for Palaeobiology, Institute of Palaeontology, Yunnan University, Kunming 650500, China.
MEC International Joint Laboratory for Palaeobiology and Palaeoenvironment, Yunnan University, Kunming 650500, China.
Zookeys. 2022 Dec 22;1137:109-132. doi: 10.3897/zookeys.1137.94224. eCollection 2022.
Wang & Zhai, is described from late Quaternary sediments in central-eastern Inner Mongolia, northern China. The new species, which has a carapace shape and pitted surface typical of the genus, is characterised by double rows of fine, densely arranged marginal ripplets, separated by an inner list, along both anterior and posterior calcified inner lamellae in the left valve. Outline analysis and Principal Component Analysis indicate that its morpho-space overlaps with Sars, 1890, Okubo, 1990, and Martens, 1991, which have living or fossil representatives in Inner Mongolia, but it is clearly discriminated from Zhai & Xiao, 2013. Judging from the relatively coarse lithology dominated by silt and sand, and the lack of accompanying brackish-water ostracods, Wang & Zhai, may have lived in a relatively shallow freshwater lake. It perhaps can be added to the list of species that went extinct during the Quaternary, but the timing and process of extinction await further investigation.
王和翟(物种名)是在中国内蒙古中东部晚第四纪沉积物中被描述的。这个新物种具有该属典型的背甲形状和表面有凹坑的特征,其特点是在左瓣的前后钙化内薄片上,沿着内缘有两排细小、密集排列的边缘细纹,中间由一条内脊隔开。轮廓分析和主成分分析表明,它的形态空间与1890年的萨斯(Sars)、1990年的奥久保(Okubo)和1991年的马滕斯(Martens)有重叠,这些在内蒙古有现存或化石代表,但它与2013年的翟和肖(Zhai & Xiao)有明显区别。从以粉砂和沙子为主的相对粗糙的岩性以及缺乏伴生的咸水介形虫来看,王和翟(物种)可能生活在一个相对较浅的淡水湖中。它或许可以被列入第四纪灭绝的物种名单,但灭绝的时间和过程有待进一步研究。