Impediments to Understanding Seagrasses’ Response to Global Change

机译：理解海草对全球变革反应的障碍

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Brianna M. Rock; Barnabas H. Daru;
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1. Understanding phenotypic responses to global change Report from the meeting "Global change in the Mediterranean: Learning from experiences worldwide" November 2012, Seville, Spain [J] . Gangoso Laura, Marquez-Ferrando Rocio, Ramirez Francisco, BioEssays : . 2013,第5期

机译：了解对全球变化的表型响应来自“地中海的全球变化：从全球经验中学习”会议的报告，2012年11月，西班牙塞维利亚
2. Changing perspectives on terrestrial nitrogen cycling: The importance of weathering and evolved resource‐use traits for understanding ecosystem responses to global change [J] . Wooliver Rachel, Pellegrini Adam F. A., Waring Bonnie, Functional Ecology . 2019,第10期

机译：改变陆地氮循环的视角：风化和演化资源利用特征的重要性，了解生态系统对全球变革的反应
3. Ecometabolomics for a Better Understanding of Plant Responses and Acclimation to Abiotic Factors Linked to Global Change [J] . Jordi Sardans, Albert Gargallo-Garriga, Otmar Urban, Metabolites . 2020,第6期

机译：Ecometabolomics为了更好地理解植物反应和对全球变革相关的非生物因素的驯化
4. Understanding the change in streamflow of an inland river as a response to regional climate change in Northwest China [C] . Xu Yiwen, Xu Jianhua International Conference on Geoinformatics . 2013

机译：了解内陆河流的水流变化以响应中国西北地区的气候变化
5. Understanding forest landscape response to global climatic change: An uncertainty evaluation based on spatial modeling. [D] . Xu, Chonggang. 2009

机译：了解森林景观对全球气候变化的响应：基于空间模型的不确定性评估。
6. Ecometabolomics for a Better Understanding of Plant Responses and Acclimation to Abiotic Factors Linked to Global Change [O] . Jordi Sardans, Albert Gargallo-Garriga, Otmar Urban, 2020

机译：生态代谢组学以更好地理解植物的响应并适应与全球变化有关的非生物因素
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。
8. Global change and biodiversity loss: Some impediments to response [R] . Borza, Karen, Jamieson, Dale 1991

机译：全球变化和生物多样性丧失：应对的一些障碍

Impediments to Understanding Seagrasses’ Response to Global Change

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