淡水贻贝(Unio pictorum)贝壳揭示了公元前 1300 年至今的水文和环境变化。

IF 10.8 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Global Change Biology Pub Date : 2024-10-22 DOI:10.1111/gcb.17532
Isobel Ollard, Rachel Ballantyne, David C. Aldridge
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引用次数: 0

摘要

保存下来的生物群落可以提供有关历史生态系统和近期人为改变之前的环境条件的基线数据。淡水贻贝贝壳的保存尤为完好,考古发掘中常见的贝壳组合可以帮助人们了解过去的生态系统。我们研究了与英格兰东部 Must Farm 青铜时代晚期遗址(约公元前 850 年)相关的古河道淤泥中的 Unio pictorum 蚌壳组合,该遗址位于现代内内河的一条古老支流上。我们将两个沉积层(大致为公元前 1300-700 年)中的考古贝壳与从现今内河上两个类似遗址中采集的活体贝壳进行了比较。我们比较了两个种群的大小和生长速度、年际生长变异性和稳定同位素(δ18O 和 δ13C)组成。四个种群的个体大小和冯-贝塔朗菲生长参数 L∞ 均不相同。两个现代种群(平均体长 77.3 ± SE 0.8 mm 和 73.8 ± SE 1.1 mm,L∞ 91.8 ± 5.4 mm 和 79.0 ± 8.1 mm)的平均体长和 L∞ 均高于古代种群(平均体长 58.1 ± SE 1.6 mm 和 68.4 ± SE 0.9 mm,L∞ 71.5 ± 16.9 mm 和 76.8 ± 6.2 mm)。现代个体经年龄校正后的年际生长差异也较大。现代贝壳的δ13C较低(现代贝壳为-11.8‰,古代贝壳为-9.03‰和-9.02‰),这可能反映了水文和营养系统的改变。除一个古贝壳样本外,其他所有古贝壳的δ18O 和 δ13C均呈正相关,而现代贝壳则不然。这些结果反映了当地环境条件的变化,特别是从水浅、流速缓慢的支流向水深、流速较快的渠化河流的过渡,以及人为营养富集的影响。研究结果表明,长期数据对于研究人为生态系统改变和避免保护规划中基线综合征的变化非常重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Freshwater Mussel (Unio pictorum) Shells Reveal Hydrological and Environmental Change From 1300 BC to the Present Day

Preserved biological communities can provide baseline data about the historical ecosystems and environmental conditions that preceded recent anthropogenic alteration. Freshwater mussel shells show particularly good preservation, and the shell assemblages commonly found during archaeological excavations can offer insights into past ecosystems. We studied assemblages of Unio pictorum mussel shells from palaeochannel silts associated with the Late Bronze Age site of Must Farm in eastern England (c. 850 BC), on an ancient tributary of the modern-day River Nene. We compared archaeological shells from two sediment horizons (broadly 1300–700 BC) to live individuals collected from two analogous sites on the present-day Nene. Size and growth rate, interannual growth variability and stable isotope (δ18O and δ13C) composition were compared between the populations. Size and the von Bertalanffy growth parameter L differed among all four populations. Mean lengths and L were higher in the two modern populations (mean lengths 77.3 ± SE 0.8 and 73.8 ± SE 1.1 mm, L 91.8 ± 5.4 and 79.0 ± 8.1 mm) than the ancient populations (mean lengths 58.1 ± SE 1.6 mm and 68.4 ± SE 0.9 mm; L 71.5 ± 16.9 and 76.8 ± 6.2 mm). Modern individuals also showed greater variation in age-corrected year-to-year growth. δ13C was lower in modern shells (−11.8‰ for modern shells, −9.03‰ and −9.02‰ for ancient shell populations), potentially reflecting altered hydrological and nutrient regimes. δ18O and δ13C were positively correlated for all but one sampled ancient shell, but not modern shells. These results reflect changes in local environmental conditions, particularly the transition from a shallow, slow-flowing tributary to a deeper, canalised river with faster flow, as well as effects of anthropogenic nutrient enrichment. The findings demonstrate the importance of long-term data in studying anthropogenic ecosystem alteration and avoiding shifting baseline syndrome in conservation planning.

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来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
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