Strengthening the evidence for seasonal intertidal exploitation in Mesolithic Europe and new insights into Early Holocene environmental conditions in the Bay of Biscay from the oxygen isotope composition of Phorcus lineatus (da Costa, 1778) shells

IF 2.7 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL Palaeogeography, Palaeoclimatology, Palaeoecology Pub Date : 2025-02-01 DOI:10.1016/j.palaeo.2024.112624
Asier García-Escárzaga , Alejandro León-Cristóbal , Esteban Álvarez-Fernández , André C. Colonese , Alvaro Arrizabalaga , María José Iriarte-Chiapusso , Eneko Iriarte , Miguel Ángel Fano
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Abstract

Marine molluscs have been exploited by human societies since prehistoric times. Such practices have often resulted in large accumulations of shell remains in archaeological sites that offer unique information on biological, ecological and cultural aspects of human interaction with coastal systems in the past. In this study, stable oxygen isotope (δ18O) analysis was carried out on archaeological shells of Phorcus lineatus (da Costa, 1778) from the Mesolithic shell midden site of J3 (northern Iberian coast) to determine the seasonality of intertidal collection. The results indicate a consistent pattern of winter exploitation, supporting the emerging view that collections were governed by cost-benefit and management principles that are now widespread documented in other coastal Mesolithic sites in Europe. The consistent seasonal collections of P. lineatus during colder months can be taken as evidence of specie-specific management strategy to optimize yield while preserving local populations for future exploitation. Our results reinforce the view that European hunter-gatherers developed ecological knowledge on specific animal resources that persisted over large geographic areas. Additionally, from a palaeoenvironmental perspective, the sea surface temperatures (SST) inferred from δ18O values derived from mollusc shells (SSTδ18O) indicate that coastal marine waters during the Early Holocene in the southern Bay of Biscay were warmer than those observed today. These environmental conditions are evaluated in relation to changes in insolation and ocean currents over time.
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从Phorcus lineatus (da Costa, 1778)贝壳的氧同位素组成加强了中石器时代欧洲季节性潮间带开发的证据和对比斯开湾早全新世环境条件的新见解
自史前时代以来,人类社会就开始开发海洋软体动物。这种做法往往导致考古遗址中大量贝壳残骸的堆积,这些遗址提供了关于过去人类与沿海系统相互作用的生物、生态和文化方面的独特信息。本文采用稳定氧同位素(δ18O)分析方法,对来自伊比利亚北部海岸J3中石器时代贝壳中心遗址的Phorcus lineatus (da Costa, 1778)考古贝壳进行了分析,以确定潮间带采集的季节性。研究结果表明了一种一致的冬季开采模式,支持了一种新兴的观点,即收集是由成本效益和管理原则控制的,这种原则现在在欧洲其他沿海中石器时代遗址中得到了广泛的记录。在较冷的月份持续的季节采集可以作为物种特定管理策略的证据,以优化产量,同时保留当地种群以供未来开发。我们的研究结果强化了这样一种观点,即欧洲狩猎采集者发展了关于特定动物资源的生态知识,这些知识在大的地理区域内持续存在。此外,从古环境的角度来看,由软体动物壳的δ18O值(SSTδ18O)推断的海表温度(SST)表明,比斯开湾南部早全新世的沿海海水比今天的温度要高。这些环境条件是根据日晒和洋流随时间的变化来评估的。
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来源期刊
CiteScore
5.90
自引率
10.00%
发文量
398
审稿时长
3.8 months
期刊介绍: Palaeogeography, Palaeoclimatology, Palaeoecology is an international medium for the publication of high quality and multidisciplinary, original studies and comprehensive reviews in the field of palaeo-environmental geology. The journal aims at bringing together data with global implications from research in the many different disciplines involved in palaeo-environmental investigations. By cutting across the boundaries of established sciences, it provides an interdisciplinary forum where issues of general interest can be discussed.
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