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Lambe, in 1920, split Saurolophinae and found only two genera remaining in it, Prosaurolophus, and the type genus.
The second level of discrepancies included 15 genera remaining unclassified within a particular family in the NCBI-VGR.
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Despite previous phylogenetic studies of on morphological characters, the relationships among the five euglossine genera remain under debate.
Of the planktonic marine flora and fauna, only about 13 percent of the coccolithophore and planktonic foraminiferal genera remained alive.
Holosteans diverged from their chondrostean ancestors in the order Palaeonisciformes during the Permian Period and were particularly abundant in the Mesozoic Era (251 65.5 million years ago); however, only three living genera remain.
However, the genes involved in trichothecene biosynthesis in the other genera remain unknown.
The exact relationships with other basal sauropod genera remain unclear.
The two genera remain, nevertheless, distinct.
The Meandrinidae and the Agariciidae are otherwise unaffected by these analyses (although two other Pacific genera remain unstudied in the Meandrinidae, which is otherwise Atlantic in distribution).
Some zooxanthellate genera remain to be analyzed (Online Supporting Information Table S2, plus many azooxanthellates), and firm conclusions about biogeographic distributions and the prevalence of families containing single genera are thus premature.
Phylogenetically, P. ovale clusters with Plasmodium species affecting simian primates (as do P. malariae and P. vivax, but not P. falciparum), but its phylogenetic relationships to other Plasmodium species or haemosporidian parasite genera remain unclear [4].
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