Proxies in Late Cenozoic Paleoceanography

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出版者:Elsevier Science Ltd 作者:Hillaire-Marcel 出品人: 页数:862 译者: 出版时间:2007-7 价格:891.00元 装帧:HRD isbn号码:9780444527554 丛书系列:
图书标签
  • 古海洋学
  • 晚新生代
  • 古代理论
  • 海洋沉积
  • 气候变化
  • 地球化学
  • 同位素地球化学
  • 海洋学
  • 古环境
  • 深海钻探
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The present volume is the first in a series of two books dedicated to the paleoceanography of the Late Cenozoic ocean. The need for an updated synthesis on paleoceanographic science is urgent, owing to the huge and very diversified progress made in this domain during the last decade. In addition, no comprehensive monography still exists in this domain. This is quite incomprehensible in view of the contribution of paleoceanographic research to our present understanding of the dynamics of the climate-ocean system. The focus on the Late Cenozoic ocean responds to two constraints. Firstly, most quantitative methods, notably those based on micropaleontological approaches, cannot be used back in time beyond a few million years at most. Secondly, the last few million years, with their strong climate oscillations, show specific high frequency changes of the ocean with a relatively reduced influcence of tectonics. The first volume addresses quantitative methodologies to reconstruct the dynamics of the ocean andthe second, major aspects of the ocean system (thermohaline circulation, carbon cycle, productivity, sea level etc.) and will also present regional synthesis about the paleoceanography of major the oceanic basins. In both cases, the focus is the "open ocean" leaving aside nearshore processes that depend too much onlocal conditions. In this first volume, we have gathered up-to-date methodologies for the measurement and quantitative interpretation of tracers and proxies in deep sea sediments that allow reconstruction of a few key past-properties of the ocean( temperature, salinity, sea-ice cover, seasonal gradients, pH, ventilation, oceanic currents, thermohaline circulation, and paleoproductivity). Chapters encompass physical methods (conventional grain-size studies, tomodensitometry, magnetic and mineralogical properties), most current biological proxies (planktic and benthic foraminifers, deep sea corals, diatoms, coccoliths, dinocysts and biomarkers) and key geochemical tracers (trace elements, stable isotopes, radiogenic isotopes, and U-series). Contributors to the book and members of the review panel are among the best scientists in their specialty. They represent major European and North American laboratories and thus provide a priori guarantees to the quality and updat of the entire book. Scientists and graduate students in paleoclimatology, paleoceanography, climate modeling, and undergraduate and graduate students in marine geology represent the target audience. This volume should be of interest for scientists involved in several international programs, such as those linked to the IPCC (IODP - Integrated Ocean Drilling Program; PAGES - Past Global Changes; IMAGES - Marine Global Changes; PMIP: Paleoclimate Intercomparison Project; several IGCP projects etc.), That is, all programs that require access to time series illustrating changes in the climate-ocean system.

* Presents updated techniques and methods in paleoceanography * Reviews the state-of-the-art interpretation of proxies used for quantitative reconstruction of the climate-ocean system * Acts as a supplement for undergraduate and graduate courses in paleoceanography and marine geology

《Proxies in Late Cenozoic Paleoceanography》是一本旨在深入探讨地质历史末期海洋环境变化的专著。本书系统地整合了多学科研究成果,从地层分析、沉积物记录到古生物数据,全面解析晚更新世至全新世期间海洋生态系统的演变过程。作者通过详细的案例研究,揭示了不同地区和时期海洋环境的动态变化,强调了古代气候波动与海洋条件之间复杂的相互作用。 书中首先全面梳理了晚更新世到全新世期间地球环境的重大转变,如冰期-间冰期循环、温度上升和海平面波动等现象。这些内容通过大量实证数据支持,帮助读者理解这些自然变化对地球系统的深远影响。书的结构特别注重逻辑严谨性,每一章均以具体案例为核心,将理论与实际研究紧密结合。 在分析过程中,作者深入探讨了海洋生物的响应机制,包括物种分布、生态位转换以及古气候信号的保存方式。这部分内容特别具有学术价值,为理解古环境重建提供了坚实基础。书中还详细讨论了沉积物记录中的关键指标,如微化石分析、同位素比值测定及有机质含量,这些方法为研究古海洋条件奠定了科学依据。 书的另一重要特点是其跨学科视野,融合了地质学、生物学和气候学的最新发现,使读者能够从多个角度审视晚更新世海洋演变。作者通过大量图表和数据图示,使复杂的信息更易于理解,并详细解释了各类研究方法的适用场景和局限性,帮助读者建立科学判断能力。 书中对不同地区海洋变化进行了深入对比,不仅展示了全球趋势,也强调了区域差异的重要性。这种综合性的分析方式,提升了研究者对古环境变化机制的认识深度。此外,书中还特别关注人类活动对晚更新世海洋系统的潜在影响,为理解自然与人为因素交互提供了新的视角。 对于读者而言,这本书不仅是一部理论性的学术著作,更是一个引导性参考资料。通过系统的研究框架和丰富的数据支持,书中帮助读者建立全面的知识体系,并激发进一步探索的兴趣。作者特别注重将复杂的科学概念转化为易于理解的内容,使专业领域的研究更具可操作性。 这一书的价值不仅体现在其内容的丰富性和研究深度上,还在于它对读者提供了一个全面、逻辑清晰的参考框架。无论是环境科学初学者,还是专业研究人员,这本书都具备极高的教育意义和实际应用价值。通过仔细阅读,人们可以深入领会晚更新世海洋系统的演变规律,并为未来的环境变化预测提供重要依据。这一著作因此成为古海洋学领域的重要参考文献之一。

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