A Dynamic History of Climate Change and Human Impact on the Environment from Keālia Pond, Maui, Hawaiian Islands
High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Keālia Pond, Maui, coupled with archaeological and historical records, provides a detailed chronology of vegetation and climate change since before human arrival. These records provide new evidence for hum...
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| Published in | Annals of the Association of American Geographers Vol. 102; no. 4; pp. 748 - 762 |
|---|---|
| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
Washington, DC
Taylor & Francis Group
01.07.2012
Association of American Geographers Taylor & Francis Ltd |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0004-5608 2469-4452 1467-8306 2469-4460 |
| DOI | 10.1080/00045608.2011.652853 |
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| Abstract | High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Keālia Pond, Maui, coupled with archaeological and historical records, provides a detailed chronology of vegetation and climate change since before human arrival. These records provide new evidence for human-environment linkages during the Hawaiian Polynesian period and subsequent European period. Prior to human arrival, the charcoal record indicates that native forests were subject to natural fires. A shift from dry to wet climate conditions marked the beginning of the Medieval Climate Anomaly (MCA) as evidenced by a precipitation reconstruction based on a pollen abundance index. Charcoal increases around AD 840-1140 signal the presence of Polynesians in the Keālia Pond region, but there is no evidence of rapid and extensive forest clearance immediately after Polynesian arrival. The greatest reduction in pollen diversity at Keālia Pond occurred during the European period (post 1778), at which point the pollen record indicates that montane forest taxa declined, native lowland taxa disappeared from the record, and nonnative taxa Prosopis and Batis made their first appearances. Accounts by early Europeans during the nineteenth and twentieth centuries provide a historical narrative supporting the interpretation that European impacts on vegetation were widespread, whereas in this region of Maui, Polynesian impacts on vegetation appear largely confined to the lowlands. |
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| AbstractList | High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Keālia Pond, Maui, coupled with archaeological and historical records, provides a detailed chronology of vegetation and climate change since before human arrival. These records provide new evidence for human:environment linkages during the Hawaiian Polynesian period and subsequent European period. Prior to human arrival, the charcoal record indicates that native forests were subject to natural fires. A shift from dry to wet climate conditions marked the beginning of the Medieval Climate Anomaly (MCA) as evidenced by a precipitation reconstruction based on a pollen abundance index. Charcoal increases around AD 840:1140 signal the presence of Polynesians in the Keālia Pond region, but there is no evidence of rapid and extensive forest clearance immediately after Polynesian arrival. The greatest reduction in pollen diversity at Keālia Pond occurred during the European period (post 1778), at which point the pollen record indicates that montane forest taxa declined, native lowland taxa disappeared from the record, and nonnative taxa Prosopis and Batis made their first appearances. Accounts by early Europeans during the nineteenth and twentieth centuries provide a historical narrative supporting the interpretation that European impacts on vegetation were widespread, whereas in this region of Maui, Polynesian impacts on vegetation appear largely confined to the lowlands. High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Kealia Pond, Maui, coupled with archaeological and historical records, provides a detailed chronology of vegetation and climate change since before human arrival. These records provide new evidence for human-environment linkages during the Hawaiian Polynesian period and subsequent European period. Prior to human arrival, the charcoal record indicates that native forests were subject to natural fires. A shift from dry to wet climate conditions marked the beginning of the Medieval Climate Anomaly (MCA) as evidenced by a precipitation reconstruction based on a pollen abundance index. Charcoal increases around AD 840-1140 signal the presence of Polynesians in the Kealia Pond region, but there is no evidence of rapid and extensive forest clearance immediately after Polynesian arrival. The greatest reduction in pollen diversity at Kealia Pond occurred during the European period (post 1778), at which point the pollen record indicates that montane forest taxa declined, native lowland taxa disappeared from the record, and nonnative taxa Prosopis and Batis made their first appearances. Accounts by early Europeans during the nineteenth and twentieth centuries provide a historical narrative supporting the interpretation that European impacts on vegetation were widespread, whereas in this region of Maui, Polynesian impacts on vegetation appear largely confined to the lowlands. Adapted from the source document. High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Kea-lia Pond, Maui, coupled with archaeological and historical records, provides a detailed chronology of vegetation and climate change since before human arrival. These records provide new evidence for human-environment linkages during the Hawaiian Polynesian period and subsequent European period. Prior to human arrival, the charcoal record indicates that native forests were subject to natural fires. A shift from dry to wet climate conditions marked the beginning of the Medieval Climate Anomaly (MCA) as evidenced by a precipitation reconstruction based on a pollen abundance index. Charcoal increases around AD 840-1140 signal the presence of Polynesians in the Kea-lia Pond region, but there is no evidence of rapid and extensive forest clearance immediately after Polynesian arrival. The greatest reduction in pollen diversity at Kea-lia Pond occurred during the European period (post 1778), at which point the pollen record indicates that montane forest taxa declined, native lowland taxa disappeared from the record, and nonnative taxa Prosopis and Batis made their first appearances. Accounts by early Europeans during the nineteenth and twentieth centuries provide a historical narrative supporting the interpretation that European impacts on vegetation were widespread, whereas in this region of Maui, Polynesian impacts on vegetation appear largely confined to the lowlands. [PUBLICATION ABSTRACT] High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Kealia Pond, Maui, coupled with archaeological and historical records, provides a detailed chronology of vegetation and climate change since before human arrival. These records provide new evidence for human-environment linkages during the Hawaiian Polynesian period and subsequent European period. Prior to human arrival, the charcoal record indicates that native forests were subject to natural fires. A shift from dry to wet climate conditions marked the beginning of the Medieval Climate Anomaly (MCA) as evidenced by a precipitation reconstruction based on a pollen abundance index. Charcoal increases around AD 840-1140 signal the presence of Polynesians in the Kealia Pond region, but there is no evidence of rapid and extensive forest clearance immediately after Polynesian arrival. The greatest reduction in pollen diversity at Kealia Pond occurred during the European period (post 1778), at which point the pollen record indicates that montane forest taxa declined, native lowland taxa disappeared from the record, and nonnative taxa Prosopis and Batis made their first appearances. Accounts by early Europeans during the nineteenth and twentieth centuries provide a historical narrative supporting the interpretation that European impacts on vegetation were widespread, whereas in this region of Maui, Polynesian impacts on vegetation appear largely confined to the lowlands. High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Keālia Pond, Maui, coupled with archaeological and historical records, provides a detailed chronology of vegetation and climate change since before human arrival. These records provide new evidence for human—environment linkages during the Hawaiian Polynesian period and subsequent European period. Prior to human arrival, the charcoal record indicates that native forests were subject to natural fires. A shift from dry to wet climate conditions marked the beginning of the Medieval Climate Anomaly (MCA) as evidenced by a precipitation reconstruction based on a pollen abundance index. Charcoal increases around AD 840—1140 signal the presence of Polynesians in the Keālia Pond region, but there is no evidence of rapid and extensive forest clearance immediately after Polynesian arrival. The greatest reduction in pollen diversity at Keālia Pond occurred during the European period (post 1778), at which point the pollen record indicates that montane forest taxa declined, native lowland taxa disappeared from the record, and nonnative taxa Prosopis and Batis made their first appearances. Accounts by early Europeans during the nineteenth and twentieth centuries provide a historical narrative supporting the interpretation that European impacts on vegetation were widespread, whereas in this region of Maui, Polynesian impacts on vegetation appear largely confined to the lowlands. 从对毛伊岛Keālia池塘的沉积物岩心的高分辨率孢粉，木炭，和沉积分析，加上考古和历史记录，提供了一个自人类到来之前的植被与气候变化的详细年表。这些记录给在夏威夷的波利尼西亚期间和随后的欧洲期间人类与环境的联系提供了新的证据。在人类到来之前，木炭记录表明，天然森林遭受自然火灾。以花粉丰度指数为基础的降水重建证明，从干燥到潮湿的气候条件的转换，标志着中世纪气候异常（MCA）的开始。在约公元840-1140 时期木炭的增加示意了波利尼西亚人在Keālia池塘地区的存在，但是没有证据表明在波利尼西亚抵达后存在立即迅速和广泛的森林砍伐。Keālia 池塘最大的花粉多样性的减少发生在欧洲期间（1778后），在这一时期的花粉记录表明，山地森林类群下降，本土低地类群从记录中消失，外来类群牧豆和腌藜草第一次出现。在十九世纪和二十世纪早期的欧洲人的帐户提供了一个历史叙事，支持欧洲对植被的影响是广泛的这一解释，而在毛伊岛地区，波利尼西亚对植被的影响主要局限于低地。 Los análisis palinológico, de carbón vegetal y sedimentológico a alta resolución de un núcleo de sedimento de Keālia Pond, Maui, junto con registros arqueológicos e históricos, permiten derivar una cronología detallada del cambio de vegetación y clima, desde antes de la llegada del hombre. Estos registros suministran nueva evidencia de los vínculos hombre-medio ambiente durante el período hawaiiano-polinésico y el subsiguiente período europeo. El registro del carbón vegetal indica que, antes de la llegada del hombre, los bosques nativos estuvieron sujetos a incendios naturales. Un cambio de clima, que pasó de condiciones secas a húmedas, marca el comienzo de la Anomalía Climática Medieval (MCA), como se evidencia por una reconstrucción del cuadro de precipitaciones a base de un índice de abundancia de polen. Los aumentos de carbón vegetal durante el período que se extiende aproximadamente del año 840 hasta el 1140, indican la presencia de polinesios en la región Keālia Pond, pero no hay evidencia de una rápida y extensa eliminación del bosque inmediatamente después de la llegada de aquella gente. La más grande reducción en la diversidad del polen en la región de Keālia Pond ocurrió durante el período europeo (después de 1778, etapa en la cual el registro del polen indica una declinación de las taxa del bosque montano y las taxa nativas de las tierras bajas desaparecen del registro, en tanto que las taxas no nativas Prosopis y Batis hacen sus primeras apariciones. Los informes de los primeros europeos durante los siglos XIX y XX proveen una narrativa histórica que apoya la interpretación de que los impactos europeos sobre la vegetación fueron vastos, en tanto que en esta isla de Maui los impactos polinesios sobre la vegetación aparecen confinados en las tierras bajas. |
| Author | Pau, Stephanie Gillespie, Thomas W. MacDonald, Glen M. |
| Author_xml | – sequence: 1 givenname: Stephanie surname: Pau fullname: Pau, Stephanie organization: National Center for Ecological Analysis and Synthesis (NCEAS) – sequence: 2 givenname: Glen M. surname: MacDonald fullname: MacDonald, Glen M. organization: Department of Geography , University of California – sequence: 3 givenname: Thomas W. surname: Gillespie fullname: Gillespie, Thomas W. organization: Department of Geography , University of California |
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| Snippet | High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Keālia Pond, Maui, coupled with archaeological and historical... High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Kea-lia Pond, Maui, coupled with archaeological and historical... High-resolution palynological, charcoal, and sedimentological analysis of a sediment core from Kealia Pond, Maui, coupled with archaeological and historical... |
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| SubjectTerms | 20th century Anomalía Climática Medieval Batis Bgi / Prodig bosques secos submontanos Charcoal Climate Climate change Climate models Climatic conditions Climatic oscillations. Historical climates. Palaeoclimates Climatology crecimiento de la población polinesia desmonte Environment Environmental impact Environmental policy Environmental science Environmental Sciences Fire Fires forest clearance Forest fires Forests Global warming Hawaii Hawaiian Islands History Human environment Human influences Human-environment relationship Humans Indexes Islands islas de Hawaii lowland dry forests Lowlands Medieval Climate Anomaly Montane forests Mountain forests Narratives Natural history Physical geography Pollen Polynesian population growth Polynesian studies Polynesians Ponds Prosopis Records Sedimentary geology Taxa Taxonomy Vegetation Wet climates 中世纪气候异常 低地干燥森林 夏威夷群岛 森林砍伐 波利尼西亚的人口增长 |
| Title | A Dynamic History of Climate Change and Human Impact on the Environment from Keālia Pond, Maui, Hawaiian Islands |
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