Literature DB >> 35046047

Is there solid evidence of widespread landscape disturbance in the Azores before the arrival of the Portuguese?

Rui B Elias1, Simon E Connor2, Carlos A Góis-Marques3,4, Hanno Schaefer5, Luís Silva6, Miguel M Sequeira3, Mónica Moura6, Paulo A V Borges7, Rosalina Gabriel7.   

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Year:  2022        PMID: 35046047      PMCID: PMC8794843          DOI: 10.1073/pnas.2119218119

Source DB:  PubMed          Journal:  Proc Natl Acad Sci U S A        ISSN: 0027-8424            Impact factor:   12.779


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Raposeiro et al. (1) conclude that human occupation of the Azores islands began between 700 and 850 CE, causing widespread landscape disturbance and raising doubts about the islands’ presumed pristine nature when the Portuguese arrived. However, previous paleoecological studies from Flores, Pico, and São Miguel Islands (Table 1) show that permanent changes in the vegetation occurred only after the early 15th century. The authors’ work also shows the permanent decline, to the lowest levels, in arboreal pollen on Corvo and Flores occurring during Portuguese occupation, not before. So, how would cereal cultivation, livestock grazing, and settlements be possible without deforestation—the hallmark of Norse settlements elsewhere (2)?
Table 1.

Evidence of major permanent vegetation changes around sites located on Flores, Pico, and São Miguel Islands

SiteTime of major vegetation change (approximate)Evidence (decline of the dominant tree pollen and increasing abundance of light-demanding taxa)Ref.
Lagoa Rasa1500 CEDecline of trees 3
(Flores Island, 530 m a.s.l.)Decline of Juniperus
Increase of Poaceae and Ericaceae
Lagoa do Caveiro1550 CEDecline of Juniperus and Ilex 3
(Pico Island, 903 m a.s.l.)Increase in Poaceae and Ericaceae
Presence of Sphagnum
Pico Bog1600 CEGreat decrease of Ilex 3
(Pico Island, 873 m a.s.l.)Decline of Juniperus
Increase in Poaceae, Ericaceae, and Pteridium
Presence of Sphagnum
Alagoínha1515–1680 CEDecline of Juniperus 4
(Flores Island, 270 m a.s.l.)Disappearance of Picconia
Lagoa Azul1420 CE ± 40Disappearance of Juniperus and Picconia 5
(São Miguel Island, 260 m a.s.l.)Increase in Ericaceae

Juniperus = Juniperus brevifolia (Seub.) Antoine; Ilex = Ilex azorica Gand.; Picconia = Picconia azorica (Tutin) Knobl. a.s.l., above sea level.

Evidence of major permanent vegetation changes around sites located on Flores, Pico, and São Miguel Islands Juniperus = Juniperus brevifolia (Seub.) Antoine; Ilex = Ilex azorica Gand.; Picconia = Picconia azorica (Tutin) Knobl. a.s.l., above sea level. The authors argue that these early settlements were extensive. Citing Nogué et al. (6), who never mention such early settlements, they argue that these led to profound environmental and ecological disturbance. Nevertheless, they do recognize that such extensive occupation, persisting up to the 15th century, should have 1) been detected by the arriving Portuguese and mentioned in historical reports and 2) left clear archeological evidence. A major discrepancy also exists between ages assigned to the arboreal pollen decline at Lagoa do Peixinho and the same decline in a neighboring peat bog (Fig. 1). Radiocarbon dates from Azorean crater lake sediments are potentially contaminated with “old” volcanic carbon (7). Pollen concentrates, as used by the authors, are known to produce dating anomalies (8). If the authors’ dates are anomalously old, evidence for early colonization crumbles.
Fig. 1.

Arboreal pollen trends and tephra layers at Lagoa do Peixinho (LP, ref. 1) and Pico Bog (PB, ref. 3) showing the mismatch between chronologies based on pollen concentrates (LP) and macrofossils/bulk dates (PB).

Arboreal pollen trends and tephra layers at Lagoa do Peixinho (LP, ref. 1) and Pico Bog (PB, ref. 3) showing the mismatch between chronologies based on pollen concentrates (LP) and macrofossils/bulk dates (PB). Secale pollen is interpreted as evidence of cultivation, but Secale disperses significantly more pollen than other cereals (9). With dominant winds blowing directly from Europe, occasional Secale pollen likely reached the Azores. However, the authors do not provide any raw data and the datasets lack sample depths. Were enough cereal pollen recorded to indicate local cropping? Were other exotic pollen blown from the continents (e.g., Alnus, Betula, or Artemisia) (3)? The authors use Plantago pollen as an anthropogenic indicator, but it likely indicates the indigenous Plantago coronopus, a common species of coastal and high-altitude vegetation. Could lightning fires or volcanic eruptions (3) explain some of the early charcoal peaks? Could these and other natural disturbances explain some of the pre-Portuguese declines in arboreal pollen? Furthermore, why are fecal biomarkers in L. Peixinho before 700 CE, between tephra layers? Could biomarkers be related to the presence of large bird colonies (as reported by the first Portuguese colonizers)? Based on the available information, not denying the possibility of earlier human presence (10), we argue that there is no solid empirical evidence for a widespread landscape disturbance caused by pre-Portuguese settlers. Additional multidisciplinary work is required to deny the historical records that the islands were occupied by dense native forests in the 15th century. Until more convincing evidence emerges, Norse presence remains an “intriguing possibility” (10). Not merely an academic question, the assumption of extensive human impact on the Azores, from as early as the eighth century, may lead to a decrease in current conservation efforts to preserve endemic species and unique habitats.
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Authors:  S I Gabriel; M L Mathias; J B Searle
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Journal:  Proc Natl Acad Sci U S A       Date:  2021-10-12       Impact factor: 11.205

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