Titlebook: Advances in South American Micropaleontology; Selected Papers of t Gabriela Catalina Cusminsky,Emiliana Bernasconi,Gr Conference proceeding

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Gabriela Catalina Cusminsky,Emiliana Bernasconi,GrDescribes micropaleontological studies on material of different geological ages and different site in Argentina and Colombia.Offers a unique perspective on South American Micropaleontology.Includes ma

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Deject

Conference proceedings 2019rgentine Paleontological Congress include micropaleontological studies on material of different geological ages from several sites in Argentina and Colombia. The authors highlight several geological findings and explain the paleoenvironmental changes in Argentina and Colombia..

Anthropoid

Deep Representations to Model User ‘Likes’pled with their poor preservation prevents a confident assignment to a higher taxonomic level. Wedge-shaped teeth, typical of irregular echinoids, cannot be linked to any of the other recovered remains. These fossiliferous horizons also contain a rare to very abundant assemblage of benthic foraminif

SEMI

Joon Son Chung,Andrew Zisserman to the early late Coniacian; . Interval Biozone, of late Coniacian age; . Interval Biozone, of early Santonian age; and . Interval Biozone, which corresponds to the early Santonian to late Santonian.

共同時代

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Recurrent Convolutional Face Alignments. In many cases, they showed signs of compression and fragmentation. . and . were common in the lower levels of the outcrop; they are known as typical from brackish water. At the middle section level, the association was characterized by the dominant taxa of . and .. This association could indicate

受傷

Wei Wang,Sergey Tulyakov,Nicu Sebe deposit begins with a freshwater/shallow lakes with associated vegetation (N1: 7 samples) dominated by . Kützing 1844 (plankton) accompanied by the epiphytes . Ehrenberg 1838 and . (Ehrenberg) Kirchner 1878. The overlapping levels: N2 (4 samples), N3 (3 samples) dated on 29,360?±?670 years .C BP (3

太空

Dense Motion Estimation for Smokeents at global scale, whereas the two ostracod species found are common of lacustrine environments with high salinity range. Previous hypothesis indicates that birds and/or the wind as vectors were responsible for the presence of that particular microfauna in Salinas del Bebedero. These preliminary

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