Richard M. Forester
About
In The Last Decade
Richard M. Forester
57 papers receiving 1.6k citations
Peers
Comparison fields: 5 of 61
- Atmospheric Science 1.3k
- Ecology 696
- Earth-Surface Processes 538
- Paleontology 403
- Oceanography 235
Countries citing papers authored by Richard M. Forester
This map shows the geographic impact of Richard M. Forester'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 Richard M. Forester with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Richard M. Forester more than expected).
Fields of papers citing papers by Richard M. Forester
This network shows the impact of papers produced by Richard M. Forester. 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 Richard M. Forester. The network helps show where Richard M. Forester may publish in the future.
Co-authorship network of co-authors of Richard M. Forester
This figure shows the co-authorship network connecting the top 25 collaborators of Richard M. Forester. A scholar is included among the top collaborators of Richard M. Forester 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 Richard M. Forester. Richard M. Forester is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 40 | |
| 2 | Mg/Ca of Continental Ostracode Shells | 2 |
| 3 | 4 | |
| 4 | 43 | |
| 5 | Assessing the Value of Presence/Absence Data for Ostracode-Based Paleoenvironmental Reconstructions | 3 |
| 6 | Climate Record in a 240 kyr Sediment Core From Bear Lake, Utah/Idaho | 2 |
| 7 | The last Pluvial Highstand (Late Wisconsin, Tioga Age) in Panamint Valley, Southeast California | 1 |
| 8 | Late glacial climate estimates for southern Nevada the ostracode fossil record | 5 |
| 9 | Estimating past precipitation and temperature from fossil ostracodes | 12 |
| 10 | Molluscs as Climate Indicators: Preliminary Stable Isotope and Community Analysis | 4 |
| 11 | Late Glacial to Modern Climate Near Yucca Mountain Nevada | 4 |
| 12 | A regional relationship between effective moisture, lake chemistry, and ostracodes | 1 |
| 13 | 90 | |
| 14 | 42 | |
| 15 | 36 | |
| 16 | Hydrochemical parameters governing the occurrence of estuarine and marginal estuarine ostracodes; an example from south-central Alasksa | 36 |
| 17 | Limnocythere bradburyi n.sp.; a modern ostracode from central Mexico and a possible Quaternary paleoclimatic indicator | 27 |
| 18 | 45 | |
| 19 | 96 | |
| 20 | Paleoenvironmental Implications of Some Estuarine and Non-Marine Ostracodes from Ridge Basin, Southern California | 3 |
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.