Matthew w. Betts, David W. Black, B. Robinson, A. Spiess, V. Thompson
{"title":"Coastal Adaptations to the Northern Gulf of Maine and Southern Scotian Shelf","authors":"Matthew w. Betts, David W. Black, B. Robinson, A. Spiess, V. Thompson","doi":"10.2307/j.ctvwvr35j.9","DOIUrl":null,"url":null,"abstract":"The northern Gulf of Maine (NGOM) and its watershed have attracted humans for the last 12,500 years (cal BP), and evidence of Palaeoindian marine economies is well established in adjacent regions by ca. 8000 cal BP. Sea level rise (SLR) has obscured understandings of early coastal adaptations, although underwater research and some near-shore sites are providing important insights. The earliest evidence from surviving shell middens dates to ca. 5000 cal BP, and reveals that shellfish collecting and the seasonal exploitation of benthopelagic fish were important throughout the Late Maritime Archaic and Maritime Woodland periods. However, significant economic shifts have occurred. In particular, a Late Archaic focus on marine swordfish hunting was replaced by a dramatic increase in inshore seal hunting in the Maritime Woodland period. After ca. 3100 cal BP, inshore fishing for cod, flounder, sculpin, sturgeon and other species intensified. During the Late Maritime Woodland period, shellfish exploitation declined somewhat and the hunting of small seals, and, in some areas, white-tailed deer, increased sharply. The extent and nature of coastal economies in the NGOM was controlled, in part, by SLR, increasing tidal amplitude, and concomitant changes in surface-water temperatures, in tandem with broad regional cultural shifts.","PeriodicalId":127570,"journal":{"name":"The Archaeology of Human-Environmental Dynamics on the North American Atlantic Coast","volume":"5 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-11-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Archaeology of Human-Environmental Dynamics on the North American Atlantic Coast","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2307/j.ctvwvr35j.9","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The northern Gulf of Maine (NGOM) and its watershed have attracted humans for the last 12,500 years (cal BP), and evidence of Palaeoindian marine economies is well established in adjacent regions by ca. 8000 cal BP. Sea level rise (SLR) has obscured understandings of early coastal adaptations, although underwater research and some near-shore sites are providing important insights. The earliest evidence from surviving shell middens dates to ca. 5000 cal BP, and reveals that shellfish collecting and the seasonal exploitation of benthopelagic fish were important throughout the Late Maritime Archaic and Maritime Woodland periods. However, significant economic shifts have occurred. In particular, a Late Archaic focus on marine swordfish hunting was replaced by a dramatic increase in inshore seal hunting in the Maritime Woodland period. After ca. 3100 cal BP, inshore fishing for cod, flounder, sculpin, sturgeon and other species intensified. During the Late Maritime Woodland period, shellfish exploitation declined somewhat and the hunting of small seals, and, in some areas, white-tailed deer, increased sharply. The extent and nature of coastal economies in the NGOM was controlled, in part, by SLR, increasing tidal amplitude, and concomitant changes in surface-water temperatures, in tandem with broad regional cultural shifts.
北缅因湾(NGOM)和它的分水岭在过去的12500年里吸引了人类,古印度海洋经济的证据在大约8000年前就在邻近地区建立起来了。尽管水下研究和一些近岸地点提供了重要的见解,但海平面上升(SLR)掩盖了对早期沿海适应的理解。现存的贝丘最早的证据可以追溯到大约5000 cal BP,并揭示了贝类的收集和底栖鱼类的季节性开发在晚海洋古代史和海洋林地时期是重要的。然而,重大的经济变化已经发生。特别是,在海洋林地时期,对近海海豹狩猎的急剧增加取代了古代晚期对海洋剑鱼狩猎的关注。大约3100 cal BP之后,近岸捕捞鳕鱼、比目鱼、雕刻鱼、鲟鱼和其他物种的活动加强了。在海洋林地后期,贝类的开发有所减少,而小海豹的狩猎,在某些地区,白尾鹿的狩猎急剧增加。在非政府组织中,沿海经济的范围和性质在一定程度上受到SLR、潮汐振幅增加和伴随的地表水温度变化以及广泛的区域文化转变的控制。