Automated Author ProfileHaddad, Geoffrey A
Haddad, Geoffrey A
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: 5.7 (sum of 14 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
Thick, late Quaternary sediment sections were recovered at several sites on the leeward slope of Great Bahama Bank during Leg 166 of the Ocean Drilling Program. These sections have paleoceanographic records with potentially high temporal resolution. To make an initial assessment of the records corresponding to the Holocene highstand of sea level, we have identified and dated the sediments from the four upper slope sites (1004, 1005, 1008, and 1009) that were deposited during the period of time which spans the last glaciation through the Holocene. Age identifications are based upon the abundances of the Globorotalia menardii complex of planktonic foraminifera, the stable oxygen isotopic ratios of bulk sediment and the planktonic foraminifera Globogerinoides ruber, and AMS C-14 dating of bulk sediment. Comparison of these data with the sediment lithologic and geoacoustic properties shows that consistent stratigraphic relationships exist at each site: The uppermost interval of aragonite-rich sediments corresponds to the Holocene highstand of sea level (i.e. oxygen isotope stage 1) and these sediments are underlain by a relatively thin interval of aragonite-poor, partially lithified sediments which corresponds to the last glaciation when sea level was significantly lower than today (i.e. oxygen isotope stages 2-4). The Leg 166 upper slope sites possess carbonate accumulation and paleoceanographic proxy records with very high temporal resolution, with Sites 1004, 1008, and 1009 appearing to have the greatest stratigraphic integrity. Comparison of core and high-resolution seismic profile data establishes the Holocene nature of the uppermost seismic unit in the stratigraphic package of the western slope of Great Bahama Bank.
Authors
- Slowey, Niall C ;
- Wilber, R Jude ;
- Haddad, Geoffrey A ;
- Henderson, Gideon M
No description available
Authors
- Henderson, Gideon M ;
- Slowey, Niall C ;
- Haddad, Geoffrey A
No description available
Authors
- Henderson, Gideon M ;
- Slowey, Niall C ;
- Haddad, Geoffrey A
No description available
Authors
- Henderson, Gideon M ;
- Slowey, Niall C ;
- Haddad, Geoffrey A
No description available
Authors
- Droxler, André W ;
- Haddad, Geoffrey A ;
- Kroon, Dick ;
- Gartner, Stefan ;
- Wei, Wuchang ;
- McNeill, Donald F
No description available
Authors
- Haddad, Geoffrey A ;
- Droxler, André W ;
- Kroon, Dick ;
- Müller, Daniel W
No description available
Authors
- Haddad, Geoffrey A ;
- Droxler, André W ;
- Kroon, Dick ;
- Müller, Daniel W
No description available
Authors
- Droxler, André W ;
- Haddad, Geoffrey A ;
- Kroon, Dick ;
- Gartner, Stefan ;
- Wei, Wuchang ;
- McNeill, Donald F
No description available
Authors
- Droxler, André W ;
- Haddad, Geoffrey A ;
- Kroon, Dick ;
- Gartner, Stefan ;
- Wei, Wuchang ;
- McNeill, Donald F