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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.
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.
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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.
Sub-fossil assemblages indicate that between 38-25 BC (i.e. before the LGM), the distribution of the red fox is likely to have covered central Europe, and at least as far north as Southern England [ 49].
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.
Further ecomorphological analysis of wing shape trends in interglacial, Holocene, and historic-aged assemblages indicate that interglacial faunas are dominated by fast-flying, open-space taxa (T. brasiliensis) while late Holocene and Historic assemblages contain more taxa that utilized closed forest or forest gaps.
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.
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 mineral assemblages therefore indicate that the volcanic ash was derived from a subvolcanic hydrothermal system developed beneath the edifice of Ontake volcano.
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