Hit papers significantly outperform the citation benchmark for their cohort. A paper qualifies
if it has ≥500 total citations, achieves ≥1.5× the top-1% citation threshold for papers in the
same subfield and year (this is the minimum needed to enter the top 1%, not the average
within it), or reaches the top citation threshold in at least one of its specific research
topics.
This map shows the geographic impact of H. Elderfield's research. It shows the number of citations coming from papers published by authors working in each country. You can also color the map by specialization and compare the number of citations received by H. Elderfield with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites H. Elderfield more than expected).
This network shows the impact of papers produced by H. Elderfield. Nodes represent research fields, and links connect fields that are likely to share authors. Colored nodes show fields that tend to cite the papers produced by H. Elderfield. The network helps show where H. Elderfield may publish in the future.
Co-authorship network of co-authors of H. Elderfield
This figure shows the co-authorship network connecting the top 25 collaborators of H. Elderfield.
A scholar is included among the top collaborators of H. Elderfield based on the total number of
citations received by their joint publications. Widths of edges
represent the number of papers authors have co-authored together.
Node borders
signify the number of papers an author published with H. Elderfield. H. Elderfield is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
All Works
20 of 20 papers shown
1.
Hillenbrand, Claus‐Dieter, James A Smith, Gerhard Kühn, et al.. (2013). West Antarctic Ice Sheet retreat from Pine Island Bay during the Holocene: New insights into forcing mechanisms. EGUGA.1 indexed citations
2.
Davis, Earl E. & H. Elderfield. (2013). Hydrogeology of the Oceanic Lithosphere. Cambridge University Press eBooks. 726.15 indexed citations
3.
Allen, Katherine A., et al.. (2009). Validating the B/Ca proxy for seawater carbonate chemistry: evidence from culture experiments with the planktic foraminifer Orbulina universa. AGUFM. 2009.1 indexed citations
4.
Pais, João, et al.. (2009). The Neogene of Algarve (Portugal). Portuguese National Funding Agency for Science, Research and Technology (RCAAP Project by FCT). 14(14). 277–288.20 indexed citations
Hoogakker, Babette, G. P. Klinkhammer, H. Elderfield, Eelco J. Rohling, & Chris Hayward. (2009). Mg/Ca paleothermometry in high salinity environments. Earth and Planetary Science Letters. 284(3-4). 583–589.50 indexed citations
7.
Galy, Αlbert, et al.. (2006). Insights From Magnesium Isotopic Compositions on the Oceanic Hydrothermal Circulation: Is Seamount Weathering the Solution?. AGUFM. 2006.2 indexed citations
Yu, Jimin & H. Elderfield. (2005). B/Ca in Foraminiferal Calcium Carbonate and its Potential as a Paleo-pH Proxy. AGU Fall Meeting Abstracts. 2005.1 indexed citations
Barker, S., Mervyn Greaves, & H. Elderfield. (2003). A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry. Geochemistry Geophysics Geosystems. 4(9).818 indexed citations breakdown →
13.
Barker, S. & H. Elderfield. (2001). Core-top Calibrations of Foraminiferal Mg/Ca From a North Atlantic Transect: Refining Mg/Ca Paleothermometry. AGUFM. 2001.3 indexed citations
14.
Cann, J. R., H. Elderfield, & A. S. Laughton. (1999). Mid-Ocean Ridges.3 indexed citations
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive
bibliographic database. While OpenAlex provides broad and valuable coverage of the global
research landscape, it—like all bibliographic datasets—has inherent limitations. These include
incomplete records, variations in author disambiguation, differences in journal indexing, and
delays in data updates. As a result, some metrics and network relationships displayed in
Rankless may not fully capture the entirety of a scholar's output or impact.