Automated Author ProfileChistyakova, Natalia O
Chistyakova, Natalia O
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 16.1 (sum of 7 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
No description available
Authors
- Risebrobakken, Bjørg ;
- Moros, Matthias ;
- Ivanova, Elena V ;
- Chistyakova, Natalia O ;
- Rosenberg, Reinhild
No description available
Authors
- Risebrobakken, Bjørg ;
- Moros, Matthias ;
- Ivanova, Elena V ;
- Chistyakova, Natalia O ;
- Rosenberg, Reinhild
No description available
Authors
- Risebrobakken, Bjørg ;
- Moros, Matthias ;
- Ivanova, Elena V ;
- Chistyakova, Natalia O ;
- Rosenberg, Reinhild
No description available
Authors
- Risebrobakken, Bjørg ;
- Moros, Matthias ;
- Ivanova, Elena V ;
- Chistyakova, Natalia O ;
- Rosenberg, Reinhild
No description available
Authors
- Risebrobakken, Bjørg ;
- Moros, Matthias ;
- Ivanova, Elena V ;
- Chistyakova, Natalia O ;
- Rosenberg, Reinhild
No description available
Authors
- Risebrobakken, Bjørg ;
- Moros, Matthias ;
- Ivanova, Elena V ;
- Chistyakova, Natalia O ;
- Rosenberg, Reinhild
Environmental changes in the surface and bottom water layers of the Ingøydjupet Basin and history of Atlantic water inflow to the southwestern Barents Sea during the last 16 ka are reconstructed on the base of planktic and benthic foraminiferal assemblages. A multiproxy study of sediment cores PSh-5159R and PSh-5159N, including AMS 14C dating, provides time resolution of about 200 years for the deglaciation period, 100 years for Holocene, and 25-50 years for the last 400 years. Stable polar conditions with sea ice on the surface were typical for the early deglaciation period. Unstable bottom settings and onset of ice rafting marked Oldest Dryas. Cold Atlantic water inflow increased notably during the Boiling-Allerod interstadial nearby the site location and then decreased during the Younger Dryas. Early Holocene was characterized by abrupt warming in the bottom and surface water layers, especially ~9.7-7.6 ka BP. Stable conditions prevailed during Middle Holocene. Remarkable changes in the sea-surface temperature and bottom environments occurred during last 2.5 cal. ka BP.
Authors
- Chistyakova, Natalia O ;
- Ivanova, Elena V ;
- Risebrobakken, Bjørg ;
- Ovsepyan, E A ;
- Ovsepyan, Ya S