Sr‐O‐C isotope signatures reveal herbivore niche‐partitioning in a Cretaceous ecosystem

IF 2.5 2区 地球科学 Q1 PALEONTOLOGY
Palaeontology Pub Date : 2022-03-01 DOI:10.1111/pala.12591
T. Cullen, Shuangquan Zhang, Joseph Spencer, B. Cousens
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引用次数: 6

Abstract

Stable and radiogenic isotopes represent powerful tools for reconstructing ecological and environmental patterns in ancient ecosystems. The Cretaceous of North America preserves a diverse record of fossil vertebrates well‐suited to analysis using these proxies, contained within many well‐sampled and stratigraphically well‐characterized intervals. Multiple hypotheses have been offered to explain the diverse assemblages of megaherbivores that co‐occurred in the relatively restricted available landmass here, including various forms of niche‐partitioning related to habitat preference, dietary specialization and feeding height stratification. Here we analyse the 87Sr/86Sr, δ13C and δ18O of bioapatite samples obtained from a range of herbivores, faunivores and endemic taxa, from a spatiotemporally‐constrained and intensively‐sampled site in the upper Oldman Formation, to test if megaherbivores partitioned their niches based on spatial patterns of occupation and resource‐use. We also compare measured strontium values to regional 87Sr/86Sr data to assess biogeographical range sizes, habitat breadth and migration potential. We find that hadrosaurs had broad ranges, whereas ankylosaurs and ceratopsids were more spatially restricted. The 87Sr/86Sr ranges of hadrosaurs are much wider and do not overlap with those of other ornithischians, potentially related to dietary differences driven by a combination of feeding height‐stratification and habitat breadth differences. Ankylosaurs and ceratopsids overlapped extensively in 87Sr/86Sr, δ13C and δ18O, indicating overlap in the same habitats and intake of similar resources, and suggesting more complex spatiotemporal variation in resource‐use patterns, fine‐scale dietary differences, and/or sufficient resource‐availability to reduce the degree of competition given this theoretical niche overlap. Additional analyses integrating ecomorphological proxies may elucidate these patterns further.
Sr - O - C同位素特征揭示了白垩纪生态系统中食草动物的生态位划分
稳定和放射性同位素是重建古代生态系统生态和环境模式的有力工具。北美洲白垩纪保存了脊椎动物化石的多样性记录,非常适合使用这些替代物进行分析,包含在许多采样良好、地层特征良好的层段中。已经提出了多种假设来解释在相对有限的可用陆地上共同出现的巨型食草动物的不同组合,包括与栖息地偏好、饮食专门化和进食高度分层相关的各种形式的生态位划分。在这里,我们分析了从一系列食草动物、动物群和特有分类群中获得的生物磷灰石样本的87Sr/86Sr、δ13C和δ18O,这些样本来自Oldman组上部的时空约束和密集采样点,以测试巨型食草动物是否根据占据和资源利用的空间模式划分其生态位。我们还将测得的锶值与区域87Sr/86Sr数据进行了比较,以评估生物地理范围大小、栖息地宽度和迁移潜力。我们发现鸭嘴龙的活动范围很广,而甲龙和角龙类的活动范围更广。鸭嘴龙的87Sr/86Sr范围要宽得多,与其他鸟臀目恐龙没有重叠,这可能与进食高度分层和栖息地宽度差异共同驱动的饮食差异有关。甲龙类和角龙类在87Sr/86Sr、δ13C和δ18O中广泛重叠,表明在相同的栖息地和相似的资源摄入中存在重叠,并表明在这种理论生态位重叠的情况下,资源使用模式、精细的饮食差异和/或足够的资源可得性存在更复杂的时空变化,以降低竞争程度。整合生态形态代理的额外分析可能会进一步阐明这些模式。
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来源期刊
Palaeontology
Palaeontology 地学-古生物学
CiteScore
5.60
自引率
3.80%
发文量
43
审稿时长
6 months
期刊介绍: Palaeontology publishes a wide variety of papers on palaeontological topics covering: palaeozoology palaeobotany systematic studies palaeoecology micropalaeontology palaeobiogeography functional morphology stratigraphy taxonomy taphonomy palaeoenvironmental reconstruction palaeoclimate analysis and biomineralization studies.
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