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.2021 Oct 12;118(41):e2108236118.
doi: 10.1073/pnas.2108236118.

Climate change facilitated the early colonization of the Azores Archipelago during medieval times

Pedro M Raposeiro  1  2Armand Hernández  3Sergi Pla-Rabes  4Vítor Gonçalves  5  2Roberto Bao  6Alberto Sáez  7Timothy Shanahan  8Mario Benavente  3Erik J de Boer  7Nora Richter  9  10Verónica Gordon  10Helena Marques  5  2Pedro M Sousa  11  12Martín Souto  5  2Miguel G Matias  13  14Nicole Aguiar  2Cátia Pereira  13  14Catarina Ritter  5María Jesús Rubio  3Marina Salcedo  2David Vázquez-Loureiro  6Olga Margalef  4  7  15Linda A Amaral-Zettler  9  10  16Ana Cristina Costa  5  2Yongsong Huang  10Jacqueline F N van Leeuwen  17Pere Masqué  18  19  20Ricardo Prego  21Ana Carolina Ruiz-Fernández  22Joan-Albert Sanchez-Cabeza  22Ricardo Trigo  12  23Santiago Giralt  3
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Climate change facilitated the early colonization of the Azores Archipelago during medieval times

Pedro M Raposeiro et al. Proc Natl Acad Sci U S A..

Abstract

Humans have made such dramatic and permanent changes to Earth's landscapes that much of it is now substantially and irreversibly altered from its preanthropogenic state. Remote islands, until recently isolated from humans, offer insights into how these landscapes evolved in response to human-induced perturbations. However, little is known about when and how remote systems were colonized because archaeological data and historical records are scarce and incomplete. Here, we use a multiproxy approach to reconstruct the initial colonization and subsequent environmental impacts on the Azores Archipelago. Our reconstructions provide unambiguous evidence for widespread human disturbance of this archipelago starting between 700-60+50 and 850-60+60 Common Era (CE), ca. 700 y earlier than historical records suggest the onset of Portuguese settlement of the islands. Settlement proceeded in three phases, during which human pressure on the terrestrial and aquatic ecosystems grew steadily (i.e., through livestock introductions, logging, and fire), resulting in irreversible changes. Our climate models suggest that the initial colonization at the end of the early Middle Ages (500 to 900 CE) occurred in conjunction with anomalous northeasterly winds and warmer Northern Hemisphere temperatures. These climate conditions likely inhibited exploration from southern Europe and facilitated human settlers from the northeast Atlantic. These results are consistent with recent archaeological and genetic data suggesting that the Norse were most likely the earliest settlers on the islands.

Keywords: biomarkers; climate simulations; ecosystem disruption; island colonization; paleolimnology.

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Conflict of interest statement

The authors declare no competing interest.

Figures

Fig. 1.
Fig. 1.
(A) Inset: Location of the Azores Archipelago in the North Atlantic. Red lines, triple junction between North American, the Eurasian, and the Nubian plates. (B) Large figure: Distribution of the islands in the Western Group (Corvo and Flores Islands), Central Group (São Jorge, Faial, Graciosa, Terceira, and Pico Islands), and Eastern Group (São Miguel and Santa Maria Islands). Islands and lakes from which sediment records have been studied are indicated. The dates for each lake correspond to the first appearance of unequivocal evidence of human activities (seeResults and Discussion for further details).
Fig. 2.
Fig. 2.
(Left) Fecal sterol biomarkers coprostanol (blue bar) (5β-cholestan-3β-ol) and 5β-stigmastanol flux (magenta bar) (ng cm−2 y−1), Coprophilous fungi flux (orange bar) (spores cm−2 y−1), Arboreal pollen (%; green line and silhouette), presence of Cerealea pollen (yellow dot) andSporormiella-type fungi (star). (Right) Total pyrolytic PAHs flux (black bar) (ng cm−2 y−1) and charcoal flux (orange bar) (particles cm−2 y−1). Western Group, (A) Lake Caldeirão (Corvo Island) and (B) Lake Funda (Flores Island); Central Group, (C) Lake Peixinho (Pico Island) and (D) Lake Ginjal (Terceira Island); and Eastern Group, (E) Lake Azul (São Miguel Island). Phases: I, absence of fecal biomarkers; II, first appearance of fecal biomarkers; III, first appearance of coprostanol (5β-cholestan-3β-ol); IV, official Portuguese arrival to Azores Archipelago. Gray bars represent tephra layers.
Fig. 3.
Fig. 3.
North Atlantic average anomalies for MSLP (blue/red lines), 2 m temperature (shading), and 925 hPa horizontal wind (vectors) during the 850 to 1500 CE period. (A) Average anomalies for MSLP (blue/red lines), 2 m temperature (shading), and 925 hPa horizontal wind (vectors) during NAO/EA prevailing conditions. Green line, Norse maritime routes during the ninth to eleventh century. Blue rectangle, location of the Azores Archipelago (AZO). Dotted orange, a possible route of Norse reaching the Azores Archipelago. (B) Average anomalies for MSLP (blue/red lines), 2 m temperature (shading), and 925 hPa horizontal wind (vectors) during NAO/EA+ prevailing conditions. Magenta line, Portuguese maritime routes during fifteenth century. Blue rectangle, Azores Archipelago location.
Fig. 4.
Fig. 4.
Summary of evidence for earlier human activities and the timing of the Portuguese arrival in the Azorean Archipelago between 500 to 1800 CE.
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References

    1. Adam J., Ronnby J., “The consequences of new warships–From medieval to modern and our dialectical relationship with things” in On War on Board–Archaeological and Historical Perspectives on Early Modern Maritime Violence and Warfare, Ronnby J., Ed. (Södertörns högskola, 2019), pp. 163–198.
    1. Frutuoso G., Livro Quarto das Saudades da Terra (Instituto Cultural de Ponta Delgada, 1981).
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    1. Matos A. T., “Povoamento e colonização dos Açores” in Portugal No Mundo, de Albuquerque L., Ed. (Alfa, 1989), pp. 176–188.

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