Marine invertebrate migrations trace climate change over 450 million years (vol 27, pg 704, 2018)

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Marine invertebrate migrations trace climate change over 450 million years (vol 27, pg 704, 2018)

机译：海洋无脊椎动物迁移追踪气候变化超过4.5亿年（第27卷，PG 704,2018）

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《Global ecology and biogeography》 |2020年第8期|共3页
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1. Marine invertebrate migrations trace climate change over 450 million years (vol 27, pg 704, 2018) [J] . Global ecology and biogeography . 2020,第7a8期

机译：海洋无脊椎动物迁移追踪气候变化超过4.5亿年（第27卷，PG 704,2018）
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3. Climate Change 2018 Antarctic marine biodiversity and climate change- Simon A Morley- University of Bangor [J] . Simon A Morley Journal of Biodiversity, Bioprospecting and Development . 2020,第1期

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4. PHOTON ACTIVATION ANALYSIS OF TRACE ELEMENTS IN THE SEVERAL KINDS OF MARINE INVERTEBRATES [C] . MICHIKO FUKUSHIMA, HIDETOSHI TAMATE International conference on nuclear analytical methods in the life sciences(NAMLS) : Abstracts . 1998

机译：几种海洋无脊椎动物中微量元素的光子活化分析
5. Early embryonic motility in broadcast-spawning marine invertebrates: Ciliary swimming, risk, and migration in the plankton [D] . McDonald, Kathryn A. 2007

机译：繁殖产生的海洋无脊椎动物的早期胚胎运动：纤毛游泳，浮游生物的风险和迁移
6. Rethinking the conceptual terrain of AIDS scholarship: lessons from comparing 27 years of AIDS and climate change research [O] . May Chazan, Michael Brklacich, Alan Whiteside 2009

机译：重新思考艾滋病研究的概念领域：比较27年艾滋病与气候变化研究的经验教训
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

Marine invertebrate migrations trace climate change over 450 million years (vol 27, pg 704, 2018)

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