Automated Author ProfileChambers, Steven R
Chambers, Steven R
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: 6.0 (sum of 14 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
No description available
Authors
- Chambers, Steven R
No description available
Authors
- Chambers, Steven R ;
- Cranston, Ray E
No description available
Authors
- Chambers, Steven R ;
- Cranston, Ray E
No description available
Authors
- Chambers, Steven R
No description available
Authors
- Chambers, Steven R
No description available
Authors
- Chambers, Steven R
We present carbon and oxygen isotope values and planktonic/benthic ratios for middle Miocene (11-17.5 Ma) foraminifers deposited at Ocean Drilling Program Hole 744B in the Southern Ocean. Major features of the isotope records are similar to those of other middle Miocene open-ocean records. The portion of the sequence containing the major middle Miocene d18O increase (between 60 and 52 m below seafloor) is a relatively condensed zone characterized by low planktonic/benthic ratios and several hiatuses.The isotopic record is of sufficiently high resolution to date the d18O minima and the d13C maxima to within 200,000 yr. Ages determined using the oxygen and carbon isotope stratigraphy are similar to those obtained using diatom, radiolarian, and paleomagnetic stratigraphy, but are approximately 1 m.y. younger than those determined using the strontium isotope stratigraphy published in this volume.The average middle Miocene sediment-accumulation rate for Hole 744B is approximately 4 m/m.y.
Authors
- Woodruff, Fay ;
- Chambers, Steven R
No description available
Authors
- Chambers, Steven R ;
- Cranston, Ray E
No description available
Authors
- Vrolijk, Peter J ;
- Chambers, Steven R ;
- Gieskes, Joris M ;
- O´Neil, J R