scholarly journals Palaeoenvironmental changes in Eocene Tibetan lake systems traced by geochemistry, sedimentology and palynofacies

2021 ◽  
Vol 214 ◽  
pp. 104778
Author(s):  
Qin Yuan ◽  
Natasha Barbolini ◽  
Luisa Ashworth ◽  
Catarina Rydin ◽  
Dong-Lin Gao ◽  
...  
Author(s):  
Małgorzata Leśniewska ◽  
Małgorzata Witak

Holocene diatom biostratigraphy of the SW Gulf of Gdańsk, Southern Baltic Sea (part III)The palaeoenvironmental changes of the south-western part of the Gulf of Gdańsk during the last 8,000 years, with reference to the stages of the Baltic Sea, were reconstructed. Diatom analyses of two cores taken from the shallower and deeper parts of the basin enabled the conclusion to be drawn that the microflora studied developed in the three Baltic phases: Mastogloia, Littorina and Post-Littorina. Moreover, the so-called anthropogenic assemblage was observed in subbottom sediments of the study area.


BMC Biology ◽  
2021 ◽  
Vol 19 (1) ◽  
Author(s):  
Daniel DeMiguel ◽  
Laura Domingo ◽  
Israel M. Sánchez ◽  
Isaac Casanovas-Vilar ◽  
Josep M. Robles ◽  
...  

Abstract Background The two main primate groups recorded throughout the European Miocene, hominoids and pliopithecoids, seldom co-occur. Due to both their rarity and insufficiently understood palaeoecology, it is currently unclear whether the infrequent co-occurrence of these groups is due to sampling bias or reflects different ecological preferences. Here we rely on the densely sampled primate-bearing sequence of Abocador de Can Mata (ACM) in Spain to test whether turnovers in primate assemblages are correlated with palaeoenvironmental changes. We reconstruct dietary evolution through time (ca. 12.6–11.4 Ma), and hence climate and habitat, using tooth-wear patterns and carbon and oxygen isotope compositions of enamel of the ubiquitous musk-deer Micromeryx. Results Our results reveal that primate species composition is strongly correlated with distinct environmental phases. Large-bodied hominoids (dryopithecines) are recorded in humid, densely-forested environments on the lowermost portion of the ACM sequence. In contrast, pliopithecoids inhabited less humid, patchy ecosystems, being replaced by dryopithecines and the small-bodied Pliobates toward the top of the series in gallery forests embedded in mosaic environments. Conclusions These results support the view that pliopithecoid primates preferred less humid habitats than hominoids, and reveal that differences in behavioural ecology were the main factor underpinning their rare co-occurrence during the European Miocene. Our findings further support that ACM hominoids, like Miocene apes as a whole, inhabited more seasonal environments than extant apes. Finally, this study highlights the importance of high-resolution, local investigations to complement larger-scale analyses and illustrates that continuous and densely sampled fossiliferous sequences are essential for deciphering the complex interplay between biotic and abiotic factors that shaped past diversity.


2021 ◽  
Vol 153 ◽  
pp. 104791
Author(s):  
Gregor Pfalz ◽  
Bernhard Diekmann ◽  
Johann-Christoph Freytag ◽  
Boris K. Biskaborn
Keyword(s):  

Boreas ◽  
2020 ◽  
Author(s):  
Matěj Roman ◽  
Barbora Chattová ◽  
Jiří Lehejček ◽  
Václav Tejnecký ◽  
Daniel Vondrák ◽  
...  

Hydrobiologia ◽  
1993 ◽  
Vol 251 (1-3) ◽  
pp. 257-268 ◽  
Author(s):  
Anna Hillbricht-Ilkowska
Keyword(s):  

2009 ◽  
Vol 44 (1) ◽  
pp. 203-215 ◽  
Author(s):  
G. Vilaclara ◽  
G. Martinez-Mekler ◽  
E. Cuna ◽  
E. Ugalde

2021 ◽  
Vol 49 (1) ◽  
pp. 133-146
Author(s):  
T. A. Chikisheva ◽  
D. V. Pozdnyakov

On the basis of statistical analysis of craniometric data relating to Mesolithic and Neolithic samples from northern Eurasia, we discuss the peopling of the Baraba forest-steppe in the Early Holocene. This region is represented by samples from Sopka-2/1 (early sixth millennium BC), Protoka (late fifth to early fourth millennia BC), Korchugan (early-mid sixth millennium BC), and Vengerovo-2A (late sixth millennium BC). The results of the principal component analysis are interpreted in the context of debates over the role of autochthonous traditions in the Neolithic. During the Preboreal period (10 ka BP), large parts of the Baraba forest-steppe were flooded by the transgression of lake systems during climatic warming. This may have caused depopulation, lasting for at least a millennium. The Early Holocene people of Baraba were an offshoot of Meso-Neolithic populations of the northwestern Russian Plain. On that basis, the Early Neolithic populations of Baraba were formed. Direct population continuity is traceable only through the Chalcolithic. Since the late sixth millennium BC, however, the local population had incorporated migrants from the Pit-Comb Ware area in the central Russian Plain and, indirectly (via the Neolithic Altai), from the Cis-Baikal area.


1991 ◽  
pp. 325-329 ◽  
Author(s):  
Robert G. Wetzel ◽  
Gene E. Likens
Keyword(s):  

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