Abstract
We have applied the TEX86 paleothermometer to produce a surface water temperature record for LakeMalawi spanning the past 700 years. Over much oftherecord temperature fluctuates from ~ 24–27 °C with a mean of ~ 25 °C ; however, there has been a substantial increase in temperature of ~ 2.0 °C duringthe past ~ 100 years. The TEX86 temperature record reveals a strong similarity to the instrumental record; both records demonstrate warming (~ 0.7–1.4 °C) over the past ~ 50 years as well as a cooling anomaly around 1959. Comparison ofthe TEX86 temperature record with the proxy recordsof primary productivity suggests that wind induced upwelling and/or precipitation have a strong influence on the surface temperature of LakeMalawi
| Original language | English |
|---|---|
| Pages (from-to) | 133-139 |
| Number of pages | 7 |
| Journal | Palaeogeography, Palaeoclimatology, Palaeoecology |
| Volume | 303 |
| Issue number | 1-4 |
| DOIs | |
| Publication status | Published - 2011 |
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