Alvaro Castilla‐Beltrán, A. Monteath, B. Jensen, L. Nascimento, José María Fernández-Palacios, Nichola A. Strandberg, M. Edwards, Sandra Nogué
{"title":"塔明福戈岛:佛得角火山锥沉积物序列中记录的全新世晚期火山活动、自然火灾和土地利用","authors":"Alvaro Castilla‐Beltrán, A. Monteath, B. Jensen, L. Nascimento, José María Fernández-Palacios, Nichola A. Strandberg, M. Edwards, Sandra Nogué","doi":"10.1177/09596836221145442","DOIUrl":null,"url":null,"abstract":"Cabo Verde remained uninhabited until 1460 CE, when European sailors founded a settlement in Santiago, and soon after in Fogo island. The degree to which different island ecosystems in Cabo Verde have been transformed by humans remains uncertain because of a scarcity of historical information and archaeological evidence. Disentangling these processes from natural ones is complicated in islands with a history of volcanic impacts and other natural hazards. In this paper, we apply microfossil (pollen, non-pollen palynomorphs and phytoliths) and sedimentological analyses (granulometry, X-ray diffraction, loss on ignition and tephrostratigraphy) to a 2-m sediment sequence deposited in a scoria cone from 4100 cal year BP (calibrated years before 1950 CE) to the present. The organic-rich basal sediments indicate that between 4100 and 2600 cal year BP the pre-settlement landscape of Fogo was an open grassland, where fire was infrequent and/or small-scale. An increase in volcanic glass deposition after 2600 cal year BP, peaking ca. 1200 cal year BP, suggests that there was a progressive activation of Fogo’s volcanic activity, contemporaneous with increased fire frequency and erosion pulses, but with little impact on local grassland vegetation. While dating uncertainty is high, the first evidence of intensive local land use by early settlers was in the form of cultivation of Zea mays, abundant spores of coprophilous fungi (i.e. Sporormiella), and peaks in charcoal concentrations between 800 and 400 cal year BP. This was followed by large increases in pollen from pigeon pea (Cajanus), a diverse array of exotic trees (Cupressus, Grevillea), and invasive shrubs (Lantana). The introduction of these taxa is part of recent human effort to ‘tame’ this steep, dry and hazardous island by reducing erosion and providing firewood. An important outcome of these efforts, however, is a loss of fragile native biodiversity.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"371 - 381"},"PeriodicalIF":1.6000,"publicationDate":"2023-01-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Taming Fogo Island: Late-Holocene volcanism, natural fires and land use as recorded in a scoria-cone sediment sequence in Cabo Verde\",\"authors\":\"Alvaro Castilla‐Beltrán, A. Monteath, B. Jensen, L. Nascimento, José María Fernández-Palacios, Nichola A. Strandberg, M. Edwards, Sandra Nogué\",\"doi\":\"10.1177/09596836221145442\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Cabo Verde remained uninhabited until 1460 CE, when European sailors founded a settlement in Santiago, and soon after in Fogo island. The degree to which different island ecosystems in Cabo Verde have been transformed by humans remains uncertain because of a scarcity of historical information and archaeological evidence. Disentangling these processes from natural ones is complicated in islands with a history of volcanic impacts and other natural hazards. In this paper, we apply microfossil (pollen, non-pollen palynomorphs and phytoliths) and sedimentological analyses (granulometry, X-ray diffraction, loss on ignition and tephrostratigraphy) to a 2-m sediment sequence deposited in a scoria cone from 4100 cal year BP (calibrated years before 1950 CE) to the present. The organic-rich basal sediments indicate that between 4100 and 2600 cal year BP the pre-settlement landscape of Fogo was an open grassland, where fire was infrequent and/or small-scale. An increase in volcanic glass deposition after 2600 cal year BP, peaking ca. 1200 cal year BP, suggests that there was a progressive activation of Fogo’s volcanic activity, contemporaneous with increased fire frequency and erosion pulses, but with little impact on local grassland vegetation. While dating uncertainty is high, the first evidence of intensive local land use by early settlers was in the form of cultivation of Zea mays, abundant spores of coprophilous fungi (i.e. Sporormiella), and peaks in charcoal concentrations between 800 and 400 cal year BP. This was followed by large increases in pollen from pigeon pea (Cajanus), a diverse array of exotic trees (Cupressus, Grevillea), and invasive shrubs (Lantana). The introduction of these taxa is part of recent human effort to ‘tame’ this steep, dry and hazardous island by reducing erosion and providing firewood. An important outcome of these efforts, however, is a loss of fragile native biodiversity.\",\"PeriodicalId\":50402,\"journal\":{\"name\":\"Holocene\",\"volume\":\"33 1\",\"pages\":\"371 - 381\"},\"PeriodicalIF\":1.6000,\"publicationDate\":\"2023-01-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Holocene\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1177/09596836221145442\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Holocene","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1177/09596836221145442","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 1
摘要
佛得角一直无人居住,直到公元1460年,欧洲水手在圣地亚哥建立了一个定居点,不久之后又在福戈岛建立了定居点。由于缺乏历史资料和考古证据,佛得角不同岛屿生态系统被人类改变的程度仍然不确定。在有火山影响和其他自然灾害历史的岛屿上,将这些过程与自然过程分开是很复杂的。在本文中,我们应用微化石(花粉、非花粉孢形态和植物岩)和沉积学分析(粒度测定、x射线衍射、燃烧损失和地层)对一个从4100 cal年BP (1950 CE之前的校准年)至今的2 m沉积层序进行了研究。富有机质的基底沉积物表明,在4100 ~ 2600 cal年BP之间,福古地区为开阔的草原景观,火灾很少发生,且规模较小。火山玻璃沉积在2600 cal - year BP之后增加,在1200 cal - year BP左右达到峰值,表明Fogo火山活动逐渐激活,同时火灾频率和侵蚀脉冲增加,但对当地草地植被的影响很小。虽然年代的不确定性很高,但早期定居者密集利用当地土地的第一个证据是以玉米的种植形式出现的,大量的粪菌孢子(即孢子菌),木炭浓度在800至400 cal year BP之间达到峰值。随后,来自鸽豆(Cajanus)、各种各样的外来树木(柏树、绿柳树)和入侵灌木(Lantana)的花粉大量增加。这些物种的引入是人类最近通过减少侵蚀和提供柴火来“驯服”这个陡峭、干燥和危险的岛屿的努力的一部分。然而,这些努力的一个重要结果是脆弱的本地生物多样性的丧失。
Taming Fogo Island: Late-Holocene volcanism, natural fires and land use as recorded in a scoria-cone sediment sequence in Cabo Verde
Cabo Verde remained uninhabited until 1460 CE, when European sailors founded a settlement in Santiago, and soon after in Fogo island. The degree to which different island ecosystems in Cabo Verde have been transformed by humans remains uncertain because of a scarcity of historical information and archaeological evidence. Disentangling these processes from natural ones is complicated in islands with a history of volcanic impacts and other natural hazards. In this paper, we apply microfossil (pollen, non-pollen palynomorphs and phytoliths) and sedimentological analyses (granulometry, X-ray diffraction, loss on ignition and tephrostratigraphy) to a 2-m sediment sequence deposited in a scoria cone from 4100 cal year BP (calibrated years before 1950 CE) to the present. The organic-rich basal sediments indicate that between 4100 and 2600 cal year BP the pre-settlement landscape of Fogo was an open grassland, where fire was infrequent and/or small-scale. An increase in volcanic glass deposition after 2600 cal year BP, peaking ca. 1200 cal year BP, suggests that there was a progressive activation of Fogo’s volcanic activity, contemporaneous with increased fire frequency and erosion pulses, but with little impact on local grassland vegetation. While dating uncertainty is high, the first evidence of intensive local land use by early settlers was in the form of cultivation of Zea mays, abundant spores of coprophilous fungi (i.e. Sporormiella), and peaks in charcoal concentrations between 800 and 400 cal year BP. This was followed by large increases in pollen from pigeon pea (Cajanus), a diverse array of exotic trees (Cupressus, Grevillea), and invasive shrubs (Lantana). The introduction of these taxa is part of recent human effort to ‘tame’ this steep, dry and hazardous island by reducing erosion and providing firewood. An important outcome of these efforts, however, is a loss of fragile native biodiversity.
期刊介绍:
The Holocene is a high impact, peer-reviewed journal dedicated to fundamental scientific research at the interface between the long Quaternary record and the natural and human-induced environmental processes operating at the Earth''s surface today. The Holocene emphasizes environmental change over the last ca 11 700 years.