Southern Italy provides a tree ring chronology dataset for paleoclimate reconstruction. The data covers the period from 106 to -30 calendar years before present. NOAA National Centers for Environmental Information archived this study, last updated in 1980.
Use Cases
- Calibrating climate models using tree ring width as a proxy for past temperature or precipitation in Southern Europe.
- Analyzing growth anomaly patterns within the chronology to identify volcanic or climatic events.
- Cross-dating this Italian chronology with other regional series to validate hemispheric climate reconstructions.
- Studying the response of Pinus species (PINI) to environmental stressors over a 136-year period.
Strengths
- Chronology spans 136 calendar years (106 to -30 BP), providing a continuous time series.
- Data is curated and archived by NOAA NCEI, an authoritative source for paleoclimate data.
Limitations
- The dataset is temporally stale, with a last update date of 1980.
- Sample size and replication depth are unknown, potentially limiting statistical robustness.
- Geographic coverage is limited to a single site (Monte Mattone) in Italy.
Provenance
- Source
- NOAA National Centers for Environmental Information (NCEI) / World Data Service for Paleoclimatology.
- Collection Method
- Tree ring data collection and analysis (dendrochronology).
- Time Range
- 106 to -30 calendar years before present (BP).
- Freshness
- null
- Geography
- Monte Mattone, Italy, Southern Europe.