温德米尔水母

艾氏温德米尔水母; 化石时期：550–543 Ma PreЄ Є O S D C P T J K Pg N 埃迪卡拉纪晚期
科学分类
界：	动物界 Animalia
门：	†前分节动物门 Proarticulata
纲：	†双侧水母纲 Dipleurozoa
科：	†狄更逊水母科 Dickinsoniidae
属：	†温德米尔水母属 Windermeria; Narbonne, 1994
种：	†艾氏温德米尔水母 W. aitkeni
二名法
	†Windermeria aitkeni; Narbonne, 1994

温德米尔水母（学名：Windermeria）又名温德米尔虫，是前分节动物门双侧水母纲底下的一个物种。在最一开始只发现了一个编号为GSC 102373的化石标本，^[2]^[3]在那之后也陆陆续续地发现了其他化石，可能是亲戚关系关系的管水母虫属（英语：Annulatubus）都是在加拿大英属哥伦比亚省塞奎布鲁克河北边的蓝花地层（英语：Blueflower Formation）。^[4]^[5]^[6]^[7]^[8]^[9]与伊沃维克虫属（英语：Ivovicia）一样都生活在大约5亿5千万年到5亿4千3百万年^[1]^[10]，也都是双侧水母纲底下的物种。^[1]温德米尔水母的是以温德米尔湖（Windermere）命名的，因为此物种的化石就是在温德米尔湖发现的。种小名的“aitkeni”是为了感谢詹姆斯·D·艾特肯（James D. Aitken）对蓝花地层的地理贡献。^[2]温德米尔水母长1.64公分，宽0.79公分，大致上是椭圆形，且两边大约平行，身体的头尾两端是圆形的。而且身体有分节，之中会有沟槽。^[2]温德米尔水母是生活在浅水里，与其他当地的双侧水母类不一样，且用匍匐的向前移动。^[3]^[4]

资料来源

^ ^1.0 ^1.1 ^1.2 Freeman, Gary. The rise of bilaterians. Historical Biology. 2009-03, 21 (1-2) [2024-03-15]. ISSN 0891-2963. doi:10.1080/08912960903295843. （原始内容存档于2023-02-19）.
^ ^2.0 ^2.1 ^2.2 Narbonne, Guy M. New Ediacaran fossils from the Mackenzie Mountains, northwestern Canada. Journal of Paleontology. 1994-05, 68 (3). ISSN 0022-3360. doi:10.1017/s0022336000025816.
^ ^3.0 ^3.1 Bowyer, F. T.; Shore, A. J.; Wood, R. A.; Alcott, L. J.; Thomas, A. L.; Butler, I. B.; Curtis, A.; Hainanan, S.; Curtis-Walcott, S.; Penny, A. M.; Poulton, S. W. Regional nutrient decrease drove redox stabilisation and metazoan diversification in the late Ediacaran Nama Group, Namibia. Scientific Reports. 2020-02-10, 10 (1). ISSN 2045-2322. doi:10.1038/s41598-020-59335-2.
^ ^4.0 ^4.1 Carbone, Calla A.; Narbonne, Guy M.; Macdonald, Francis A.; Boag, Thomas H. New Ediacaran fossils from the uppermost Blueflower Formation, northwest Canada: disentangling biostratigraphy and paleoecology (PDF). Journal of Paleontology. 2015-03, 89 (2) [2024-03-16]. ISSN 0022-3360. doi:10.1017/jpa.2014.25. （原始内容存档 (PDF)于2024-06-30）.
^ Waggoner, B. The Ediacaran Biotas in Space and Time. Integrative and Comparative Biology. 2003-02-01, 43 (1). ISSN 1540-7063. doi:10.1093/icb/43.1.104.
^ Moynihan, David P.; Strauss, Justin V.; Nelson, Lyle L.; Padget, Colin D. Upper Windermere Supergroup and the transition from rifting to continent-margin sedimentation, Nadaleen River area, northern Canadian Cordillera. GSA Bulletin. 2019-03-08, 131 (9-10). ISSN 0016-7606. doi:10.1130/b32039.1.
^ Carbone, Calla; Narbonne, Guy M. When Life Got Smart: The Evolution of Behavioral Complexity Through the Ediacaran and Early Cambrian of NW Canada. Journal of Paleontology. 2014-03, 88 (2). ISSN 0022-3360. doi:10.1666/13-066.
^ Grazhdankin, Dima. Patterns of distribution in the Ediacaran biotas: facies versus biogeography and evolution. Paleobiology. 2004-06, 30 (2) [2024-03-15]. ISSN 0094-8373. doi:10.1666/0094-8373(2004)030<0203:podite>2.0.co;2. （原始内容存档于2024-03-15）.
^ MacNaughton, Robert B; Narbonne, Guy M; Dalrymple, Robert W. Neoproterozoic slope deposits, Mackenzie Mountains, northwestern Canada: implications for passive-margin development and Ediacaran faunal ecology. Canadian Journal of Earth Sciences. 2000-07-01, 37 (7) [2024-03-15]. ISSN 0008-4077. doi:10.1139/e00-012. （原始内容存档于2024-03-15）.
^ Xiao, S.H.; Narbonne, G.M. The Ediacaran Period. Geologic Time Scale 2020 (PDF). Elsevier. 2020: 521–561 [2024-03-15]. ISBN 978-0-12-824360-2. （原始内容存档 (PDF)于2024-03-15）.

[:1-1] 1.0 ^1.1 ^1.2 Freeman, Gary. The rise of bilaterians. Historical Biology. 2009-03, 21 (1-2) [2024-03-15]. ISSN 0891-2963. doi:10.1080/08912960903295843. （原始内容存档于2023-02-19）.

[:0-2] 2.0 ^2.1 ^2.2 Narbonne, Guy M. New Ediacaran fossils from the Mackenzie Mountains, northwestern Canada. Journal of Paleontology. 1994-05, 68 (3). ISSN 0022-3360. doi:10.1017/s0022336000025816.

[:2-3] 3.0 ^3.1 Bowyer, F. T.; Shore, A. J.; Wood, R. A.; Alcott, L. J.; Thomas, A. L.; Butler, I. B.; Curtis, A.; Hainanan, S.; Curtis-Walcott, S.; Penny, A. M.; Poulton, S. W. Regional nutrient decrease drove redox stabilisation and metazoan diversification in the late Ediacaran Nama Group, Namibia. Scientific Reports. 2020-02-10, 10 (1). ISSN 2045-2322. doi:10.1038/s41598-020-59335-2.

[:3-4] 4.0 ^4.1 Carbone, Calla A.; Narbonne, Guy M.; Macdonald, Francis A.; Boag, Thomas H. New Ediacaran fossils from the uppermost Blueflower Formation, northwest Canada: disentangling biostratigraphy and paleoecology (PDF). Journal of Paleontology. 2015-03, 89 (2) [2024-03-16]. ISSN 0022-3360. doi:10.1017/jpa.2014.25. （原始内容存档 (PDF)于2024-06-30）.

[5] Waggoner, B. The Ediacaran Biotas in Space and Time. Integrative and Comparative Biology. 2003-02-01, 43 (1). ISSN 1540-7063. doi:10.1093/icb/43.1.104.

[6] Moynihan, David P.; Strauss, Justin V.; Nelson, Lyle L.; Padget, Colin D. Upper Windermere Supergroup and the transition from rifting to continent-margin sedimentation, Nadaleen River area, northern Canadian Cordillera. GSA Bulletin. 2019-03-08, 131 (9-10). ISSN 0016-7606. doi:10.1130/b32039.1.

[7] Carbone, Calla; Narbonne, Guy M. When Life Got Smart: The Evolution of Behavioral Complexity Through the Ediacaran and Early Cambrian of NW Canada. Journal of Paleontology. 2014-03, 88 (2). ISSN 0022-3360. doi:10.1666/13-066.

[8] Grazhdankin, Dima. Patterns of distribution in the Ediacaran biotas: facies versus biogeography and evolution. Paleobiology. 2004-06, 30 (2) [2024-03-15]. ISSN 0094-8373. doi:10.1666/0094-8373(2004)030<0203:podite>2.0.co;2. （原始内容存档于2024-03-15）.

[9] MacNaughton, Robert B; Narbonne, Guy M; Dalrymple, Robert W. Neoproterozoic slope deposits, Mackenzie Mountains, northwestern Canada: implications for passive-margin development and Ediacaran faunal ecology. Canadian Journal of Earth Sciences. 2000-07-01, 37 (7) [2024-03-15]. ISSN 0008-4077. doi:10.1139/e00-012. （原始内容存档于2024-03-15）.

[:4-10] Xiao, S.H.; Narbonne, G.M. The Ediacaran Period. Geologic Time Scale 2020 (PDF). Elsevier. 2020: 521–561 [2024-03-15]. ISBN 978-0-12-824360-2. （原始内容存档 (PDF)于2024-03-15）.

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