Results 91 to 100 of about 182,437 (357)

Impact of late glacial climate variations on stratification and trophic state of the meromictic lake Längsee (Austria): validation of a conceptual model by multi proxy studies

open access: yesJournal of Limnology, 2002
Selected pigments, diatoms and diatom-inferred phosphorus (Di-TP) concentrations of a late glacial sediment core section of the meromictic Längsee, Austria, were compared with tephra- and varve-dated pollen stratigraphic and geochemical results.
Jens MÜLLER   +4 more
doaj   +1 more source

RELATIVE SEA-LEVEL CHANGE OF THE WHITE SEA IN THE LATE GLACIAL AND HOLOCENE: CASE STUDY OF THE SREDNYAYA TRET’ LAKE, EASTERN COAST OF THE GORLO STRAIT<a href="#FN4"><sup>4</sup></a>

open access: bronze, 2023
T. Yu. Repkina   +7 more
openalex   +2 more sources

Overexpression of CDT1 inhibits cell cycle progression at S phase by interacting with the mini‐chromosome maintenance complex and causes DNA damage

open access: yesFEBS Open Bio, EarlyView.
CDT1 is an essential protein for DNA replication licensing that loads the MCM complex, the eukaryotic replicative DNA helicase, onto replication origins. Overexpression of CDT1 induces cell cycle arrest at the S phase. Here we showed CDT1 inhibits the progression of replication forks by interacting with the MCM complex, leading to the stalling and ...
Takashi Tsuyama   +7 more
wiley   +1 more source

Organic carbon isotope record since the Late Glacial period from peat in the North Bank of the Yangtze River, China

open access: yesEuropean Journal of Remote Sensing, 2020
Detailed organic carbon isotope (δ13Corg) measurements were conducted on two peat sequences recovered from the north bank of the Yangtze River, East China. Seven radiocarbon dates provided firm age control of this δ13Corg record and reveal palaeoclimatic
Hui Zhou   +6 more
doaj   +1 more source

Late-Glacial Cwm Glaciers In Wales [PDF]

open access: yesJournal of Glaciology, 1957
AbstractThe evidence for the existence of small glaciers in the cwms of the Caernarvonshire mountains during the Late-glacial Period is presented, and by an analysis of their distribution some of the factors responsible for their formation are deduced.
openaire   +1 more source

DIATOMS FROM NEASHAM LATE‐GLACIAL DEPOSITS [PDF]

open access: yesNew Phytologist, 1952
In the remainder of this note the samples will be referred to by the arabic numerals given to them above. An appreciable number of diatoms was found in sample no. i, and they were present in large numbers in sample no. 2. There were none in samples nos. 3 and 4 and very few in samples nos. 5 and 6.
openaire   +1 more source

HSP70 governs permeability and mechanotransduction in primary human endothelial cells

open access: yesFEBS Open Bio, EarlyView.
HSP70 chemical inhibition reduces endothelial cell proliferation and increases permeability, the latter supported by normal interendothelial junctional protein distribution. HSP70 also plays a role in shear stress response, a hemodynamic force naturally present in blood vessels and correlated with vessel protection.
Andrea Pinto‐Martinez   +5 more
wiley   +1 more source

Last Glacial Maximum cooling induced positive moisture balance and maintained stable human populations in Australia

open access: yesCommunications Earth & Environment
Long-standing interpretations of the Last Glacial Maximum (21,000 ± 2000 years ago) in Australia suggest that the period was extremely cold and arid, during which the Indo-Australian summer monsoon system collapsed, and human populations declined and ...
Haidee Cadd   +7 more
doaj   +1 more source

Significance of Hippophae rhamnoides L. in evolution of the Eemian Interglacial' flora in Warsaw area

open access: yesActa Societatis Botanicorum Poloniae, 2014
Palynologic studies of sediments from Warsaw-Wawrzyszew and other sites in the Warsaw Basin enabled to analyze main occurrence phases of Hippophae rhamnoides during the widely understood Lake Pleistocene interglacial warming.
Krzysztof M. Krupiński
doaj   +1 more source

A Cenozoic-style scenario for the end-Ordovician glaciation [PDF]

open access: yes, 2014
The end-Ordovician was an enigmatic interval in the Phanerozoic, known for massive glaciation potentially at elevated CO2 levels, biogeochemical cycle disruptions recorded as large isotope anomalies and a devastating extinction event.
Achab, A   +10 more
core   +7 more sources

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