Campanian-Maastrichtian时代的介形虫非海洋生物地理学：南美洲、非洲和印度的联系

IF 0.7 Q4 PALEONTOLOGY

REVUE DE MICROPALEONTOLOGIE Pub Date : 2023-07-01 DOI:10.1016/j.revmic.2023.100716

Silvia Regina Gobbo, Reinaldo J. Bertini

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引用次数: 1

摘要

对南半球（南美洲、非洲和印度）上白垩纪的非海洋介形虫进行了研究和讨论，以建立生物地层学方案及其古地理分布。在这里进行的古地理分析揭示了十个不同的物种群：（1）Neuquén和Paraná盆地（巴西）的特征是里奥格兰德Ilyocypis riograndensis、小Neuquenocypis minor、细NeuquenoCypis tenuipunctata、Wolburgiopsis vicinalis和Vecticypris aff。点状；（2）新雷塔Wolburgiopsis是Los Llanos组（阿根廷亚安第斯盆地）、Neuquén（阿根廷）和巴拉那盆地（巴西）的特征；（3） Ilyocypis triebeli是亚安第斯盆地（玻利维亚El Molino组；阿根廷Los Llanos、Ciénaga del Rio Huaco组）和亚珊瑚岩组（Salta盆地）的特征；Neuquén（阿根廷）、Paraná和Campos盆地（巴西）：Ilyocyris triebeli；（4） Neuquén（阿根廷）、Paraná和Santos盆地（巴西）：小叶Fossocytheridea foliata；（5） Paraná，Santos（巴西），刚果（刚果民主共和国）盆地和Lameta组（印度）：圆柱状Stenocypris；（6）巴拉那（巴西）和刚果（刚果民主共和国）盆地：马卡威Paracypia makawensis和物种“K 530 b”Grekoff，1960年；（7） Yacoraite组（Salta盆地）和Neuquén盆地（阿根廷）、Paraná（巴西）和刚果（刚果民主共和国）盆地：阿根廷Ilyocypis argetiniensis；（8） Neuquén（阿根廷）、Paraná（巴西）和刚果（刚果民主共和国）盆地：Alicenula kwangoensis；（9） Paraná盆地（巴西）和Lameta组（印度）：Candona chuiensis、Cypridopsis huenei、Paracandona jabalpurensis和Paralimnocythere hasuii；（10） Paraná（巴西）、刚果（刚果民主共和国）盆地和Lameta组（印度）：Periosocyris megistus。其他属相关性，特别是Wolburgiopsis属、Neuquenocypris属、Virgatocypis属、Altanicypris和Talycypridea属，加强了这种古生物地理学的相似性，以及与Bauru群（巴拉那盆地）和Kwango系列（刚果盆地）的Campanian Maastrichtian时代，后者的时代仍需完善。

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Ostracoda non-marine biogeography in Campanian-Maastrichtian ages: South America, Africa and India connections

Non-marine ostracods from the Upper Cretaceous of Southern Hemisphere (South America, Africa and India) are studied and discussed for the purpose of establishing a biostratigraphy scheme and their paleogeographic distribution. The paleogeographic analysis performed here reveals ten distinct groupings of species: (1) Neuquén and Paraná basins (Brazil) are characterized by Ilyocypris riograndensis, Neuquenocypris minor, Neuquenocypris tenuipunctata, Wolburgiopsis vicinalis and Vecticypris aff. punctata; (2) Wolburgiopsis neocretacea is characteristic of Los Llanos Formation (Sub-Andean Basin, Argentina) and Neuquén (Argentina) and Parana basins (Brazil); (3) Ilyocypris triebeli is characteristic of Sub-Andean Basins (El Molino Formation, Bolivia; Los Llanos, Ciénaga del Rio Huaco formations, Argentina), and Yacoraite formations (Salta Basin); Neuquén (Argentina), Paraná and Campos basins (Brazil): Ilyocypris triebeli; (4) Neuquén (Argentina), Paraná and Santos basins (Brazil): Fossocytheridea lobulata; (5) Paraná, Santos (Brazil), Congo (R. D. Congo) basins and Lameta Formation (India): Stenocypris cylindrica; (6) Paraná (Brazil) and Congo (R. D. Congo) basins: Paracypria makawensis and Species “K 530 b” Grekoff, 1960; (7) Yacoraite Formation (Salta Basin) and Neuquén Basin (Argentina), Paraná (Brazil) and Congo (R. D. Congo) basins: Ilyocypris argentiniensis; (8) Neuquén (Argentina), Paraná (Brazil) and Congo (R. D. Congo) basins: Alicenula kwangoensis; (9) Paraná Basin (Brazil) and Lameta Formation (India): Candona chuiensis, Cypridopsis huenei, Paracandona jabalpurensis and Paralimnocythere hasuii; (10) Paraná (Brazil), Congo (R. D. Congo) basins and Lameta Formation (India): Periosocypris megistus. Other generic correlations, especially the genera Wolburgiopsis, Neuquenocypris, Virgatocypris, Altanicypris and Talycypridea, reinforce this paleobiogeographical similarities and a Campanian-Maastrichtian age to the Bauru Group (Paraná Basin) and the Kwango Series (Congo Basin), whose age was still in need of refinement.

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来源期刊

REVUE DE MICROPALEONTOLOGIE PALEONTOLOGY-

CiteScore

2.50

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0.00%

发文量

期刊介绍： La Revue de micropaléontologie publie 4 fois par an des articles de intérêt international, consacrés à tous les aspects de la micropaléontologie. Les textes, en anglais ou en français, sont des articles originaux, des résultats de recherche, des synthèses et mises au point, des comptes rendus de réunions scientifiques et des analyses de ouvrages. La revue se veut résolument ouverte à tous les aspects de la micropaléontologie en accueillant des travaux traitant de la systématique des microfossiles (et de leurs équivalents actuels), des bactéries aux microrestes de vertébrés, et de toutes leurs applications en sciences biologiques et géologiques.