Reconstruction of Phanerozoic climate using carbonate clumped isotopes and implications for the oxygen isotopic composition of seawater. [PDF]
Thiagarajan N +6 more
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Lower Triassic beds from Tehovec (Polhov Gradec Hills, Slovenian)
Bogdan Jurkovšek +2 more
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Morphogenesis of pteraspid heterostracan oral plates and the evolutionary origin of teeth. [PDF]
Grohganz M +3 more
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Finite element and microstructural analyses indicate that pteraspid heterostracan oral plate microstructure was adapted to a mechanical function. [PDF]
Grohganz M +5 more
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Uncertainty in the timing of diversification of flowering plants rests with equivocal interpretation of their fossil record. [PDF]
Clark JW, Donoghue PCJ.
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Reconstruction of feeding behaviour and diet in Devonian ctenacanth chondrichthyans using dental microwear texture and finite element analyses. [PDF]
Greif M +5 more
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Conodonts are zoologically enigmatic, toothlike phosphatic microfossils occurring in marine sedimentary rocks ranging in age from Cambrian to Triassic. Dimpled spheres of less than 1 millimeter in diameter are sporadic associates of conodonts and have identical chemical composition and microstructure.
B F, Glenister, G, Klapper, K M, Chauff
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ʻConodont pearlsʼ do not belong to conodonts
Lethaia, 2021We investigated the mineralogical and chemical signatures of enigmatic microspherules commonly recovered in conodont residues and referred to in literature as 'conodont pearls.' Comparison between these 'pearls,' associated conodonts and other phosphatic skeletal elements present in the same stratigraphical level was run in an effort to reveal any ...
Ferretti A. +4 more
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