Quaternary Vegetation Dynamics – The African Pollen Database 2021
DOI: 10.1201/9781003162766-20
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Pollen records of the 14th and 20th centuries AD from Lake Tsizavatsy in southwest Madagascar

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Cited by 3 publications
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“…In the east, massive forest clearing occurred around AD 700-1100 (Agarwal et al, 2005). A similar gradual change in the structure of the ecosystem toward more open vegetation was recorded in the savanna woodland at Lake Tsizavatsy (Razanatsoa et al, 2021a). These suggest that although the climate initially affected the change in the vegetation as evidenced by an increase in grass and a decrease in riverine and dry forest tree taxa, it was maintained by human activities by the change in subsistence from foraging to pastoralism as indicated by the increase in herbivory and fire activities at least until AD 1600.…”
Section: Vegetation Change Fire History and Herbivory In Southwest Madagascar During The Last 2000 Yearssupporting
confidence: 57%
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“…In the east, massive forest clearing occurred around AD 700-1100 (Agarwal et al, 2005). A similar gradual change in the structure of the ecosystem toward more open vegetation was recorded in the savanna woodland at Lake Tsizavatsy (Razanatsoa et al, 2021a). These suggest that although the climate initially affected the change in the vegetation as evidenced by an increase in grass and a decrease in riverine and dry forest tree taxa, it was maintained by human activities by the change in subsistence from foraging to pastoralism as indicated by the increase in herbivory and fire activities at least until AD 1600.…”
Section: Vegetation Change Fire History and Herbivory In Southwest Madagascar During The Last 2000 Yearssupporting
confidence: 57%
“…These records demonstrate a wetter period from AD 1300 until AD 1500, which coincides with the relatively wet period in the northwest record during the 500-year the dry phase (Scroxton et al, 2017). The tree isotope records demonstrated a significant trend in decreasing rainfall over time (Razanatsoa, 2019), which also became more pronounced in the last millennia as recorded in pollen records from the region (Burney, 1993;Razanatsoa, 2019;Razanatsoa et al, 2021a;Virah-Sawmy et al, 2016). Although pollen evidence from the region generally supports climate as a long-term driver of vegetation change (Virah-Sawmy et al, 2016), evidence of climate change is equivocal and difficult to assess due to complex interactions with anthropogenic factors.…”
Section: Introductionsupporting
confidence: 56%
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