Sentence examples for assemblages indicate that from inspiring English sources
However, the post-glacial landscape was not devoid of vegetation because pollen assemblages indicate that terrestrial vegetation, likely a spruce tundra, survived near the site.
Available reconstructions of the palaeoecology of faunal and floral assemblages indicate that the earliest Kenyan hominids, including Orrorin tugenensis, are associated with forest landscapes.
Faunal and boring assemblages indicate that the buildup settled and developed in very shallow conditions (most likely less than 10 m water depth).
The physical and geochemical properties of the paleosols and associated ichnofossil assemblages indicate that the paleolandscapes were composed of shrublands and open environments that experienced changes in moisture regimes due to seasonal precipitation and flooding events and had varying degrees of temporal stability.
Grain-size distribution and fossil ostracod assemblages indicate that deglaciation of the Herschel Island ice-thrust moraine was accompanied by alluvial, proluvial, and eolian sedimentation on the adjacent unglaciated Yukon Coastal Plain until ~ 11 cal ka BP during a period of low glacio-eustatic sea level.
The first two age clusters with the petrographical and geochemical results obtained on the different assemblages indicate that the development of the pisolitic crust first induced Mn-leaching and Fe-Al accumulations due to warmer and wetter climatic conditions in the age interval 56 47 Ma that characterizes the Tertiary greenhouse effect period propitious to bauxite formation in West Africa.
Quadrat analysis of 93 mostly (par)autochthonous megafloral assemblages indicates that pteridosperms and ferns dominated communities, with three taxa (Pecopteris spp., Callipteridium pteridium, and Neuropteris ovata) accounting for ≈ 58% of all plant remains.
The assemblage indicates that cold conditions obtained, with an open, barren landscape and a mean annual air temperature of −3°C.
A numerical study of the sub-assemblages indicated that the proposed macro-based model could provide a reliable foundation for the analysis of progressive collapse in RC frames.
Our discovery of granulitic clasts with the diopside-albite assemblage indicates that there is an andesitic material (partial melt) in some parts of the LL parent body.
Analysis of the weathering patterns of the Dinaledi assemblage indicates that most of the bones show weathering stages 1 or 2 (after Behrensmeyer, 1978); while 18% have an etched appearance and 11% exhibit dissolution (Supplementary file 2).
