Augusto Mangini
About
In The Last Decade
Augusto Mangini
208 papers receiving 11.8k citations
Hit Papers
Peers
Comparison fields: 5 of 113
- Atmospheric Science 10.1k
- Earth-Surface Processes 4.2k
- Paleontology 2.7k
- Ecology 2.6k
- Geochemistry and Petrology 2.1k
Countries citing papers authored by Augusto Mangini
This map shows the geographic impact of Augusto Mangini'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 Augusto Mangini with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Augusto Mangini more than expected).
Fields of papers citing papers by Augusto Mangini
This network shows the impact of papers produced by Augusto Mangini. 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 Augusto Mangini. The network helps show where Augusto Mangini may publish in the future.
Co-authorship network of co-authors of Augusto Mangini
This figure shows the co-authorship network connecting the top 25 collaborators of Augusto Mangini. A scholar is included among the top collaborators of Augusto Mangini 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 Augusto Mangini. Augusto Mangini is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 19 | |
| 2 | Climatic variability during the last deglaciation: A stalagmite-based multi-proxy record from Mawmluh cave, India | 1 |
| 3 | 8 | |
| 4 | 32 | |
| 5 | 54 | |
| 6 | 85 | |
| 7 | Decoupled evolution of temperature and precipitation in western Germany during the Last Interglacial reconstructed from a precisely dated speleothem | 3 |
| 8 | Monitoring of Bunker Cave (NW Germany): Assessing the complexity of cave environmental parameters | 1 |
| 9 | The influence of soil organic matter age spectrum on the reconstruction of atmospheric 14C levels via stalagmites | 3 |
| 10 | Climate variability during MIS 7, MIS 5 and the Holocene recorded in a stalagmite from western Germany | 1 |
| 11 | Water mass properties and circulation in the Cape Basin - A multiproxy approach | 1 |
| 12 | 14 C variability in two late Holocene stalagmites and the implications for climate forcing mechanisms | 1 |
| 13 | Assessing the variability of precipitation during the Holocene from stalagmite records | 1 |
| 14 | Solar Forcing of Abrupt Glacial Climate Change in a Coupled Climate System Model | 3 |
| 15 | Holocene Sun-Monsoon Linkage Recorded in Stalagmites From Oman | 1 |
| 16 | Holocene ITCZ Migration Recorded in Stalagmites From Oman (Southern Arabia) | 2 |
| 17 | Climate change in Southern Arabia: Speleothems from Yemen and Oman as archives for monsoon rainfall over the last 330,000 years | 3 |
| 18 | Holocene ITCZ Migration Recorded in Stalagmites from Southern Oman | 1 |
| 19 | 4 | |
| 20 | Strong coherence between solar variability and the monsoon in Oman between 9 and 6 kyr ago breakdown → | 602 |
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.