Thank You to Our 2022 Peer Reviewers

IF 3.2 2区地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY

Paleoceanography and Paleoclimatology Pub Date : 2023-04-01 DOI:10.1029/2023pa004653

M. Huber, U. Röhl

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引用次数: 0

Abstract

Once a year we take the opportunity to thank the reviewers whose difficult, important work is never sufficiently recognized. Three years into the COVID-19 pandemic, reviewers continued to show deep resolve to support their community, by providing thorough, timely reviews aiming to improve manuscripts, while simultaneously dealing with very difficult personal and professional circumstances. Without their intense, robust, and helpful attention, all the science we do would be diminished. Matthew and Ulla would like to express their gratitude and appreciation for your efforts this year and their hope for improvement in 2023 and beyond. Thank you to the 339 reviewers who submitted 473 reviews in the journal last year. Individuals in italics provided three or more reviews for Paleoceanography and Paleoclimatology during the year. Abbott, April Abell, Jordan Acosta, Rene Paul Agnini, Claudia Ai, Xuyuan Allen, Katherine Anagnostou, Eleni Anchukaitis, Kevin Anderson, Robert Arbic, Brian Archer, David Arreguín-Rodríguez, Gabriela Atwood, Alyssa Babila, Tali Baker, Paul Bakker, Pepijn Barron, John Barth, Aaron Bassinot, Franck Batenburg, Sietske Baumgartner, Aly Belanger, Christina Berenice, Sophie Bhattacharya, Tripti

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感谢我们2022年的同行评审

每年一次，我们借此机会感谢审稿人，他们艰难而重要的工作从未得到充分的认可。在2019冠状病毒病大流行的第三年里，审稿人继续表现出坚定的决心，通过提供全面、及时的审稿来改进稿件，同时处理非常困难的个人和职业环境。如果没有他们强烈、有力和有益的关注，我们所做的所有科学研究都会减少。马修和乌拉对您今年的努力表示感谢和赞赏，并希望在2023年及以后有所改善。感谢去年在期刊上提交了473篇评论的339位审稿人。用斜体表示的个人在这一年中提供了三篇或更多关于古海洋学和古气候学的评论。阿博特、阿贝尔、乔丹·阿科斯塔、雷内·保罗·阿格尼尼、克劳迪娅·艾、徐媛·艾伦、凯瑟琳·阿纳格诺斯、埃莱尼·安丘卡提斯、凯文·安德森、罗伯特·阿尔比奇、布莱恩·阿切尔、大卫Arreguín-Rodríguez、加布里埃拉·阿特伍德、艾莉莎·巴比拉、塔利·贝克、保罗·巴克、佩皮因·巴伦、约翰·巴特、亚伦·巴辛诺、弗兰克·巴登堡、西茨克·鲍姆加特纳、阿里·贝兰格、克里斯蒂娜·贝莱尼斯、索菲·巴塔查里亚、特里普提

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来源期刊

Paleoceanography and Paleoclimatology Earth and Planetary Sciences-Atmospheric Science

CiteScore

6.20

自引率

11.40%

发文量

107

期刊介绍： Paleoceanography and Paleoclimatology (PALO) publishes papers dealing with records of past environments, biota and climate. Understanding of the Earth system as it was in the past requires the employment of a wide range of approaches including marine and lacustrine sedimentology and speleothems; ice sheet formation and flow; stable isotope, trace element, and organic geochemistry; paleontology and molecular paleontology; evolutionary processes; mineralization in organisms; understanding tree-ring formation; seismic stratigraphy; physical, chemical, and biological oceanography; geochemical, climate and earth system modeling, and many others. The scope of this journal is regional to global, rather than local, and includes studies of any geologic age (Precambrian to Quaternary, including modern analogs). Within this framework, papers on the following topics are to be included: chronology, stratigraphy (where relevant to correlation of paleoceanographic events), paleoreconstructions, paleoceanographic modeling, paleocirculation (deep, intermediate, and shallow), paleoclimatology (e.g., paleowinds and cryosphere history), global sediment and geochemical cycles, anoxia, sea level changes and effects, relations between biotic evolution and paleoceanography, biotic crises, paleobiology (e.g., ecology of “microfossils” used in paleoceanography), techniques and approaches in paleoceanographic inferences, and modern paleoceanographic analogs, and quantitative and integrative analysis of coupled ocean-atmosphere-biosphere processes. Paleoceanographic and Paleoclimate studies enable us to use the past in order to gain information on possible future climatic and biotic developments: the past is the key to the future, just as much and maybe more than the present is the key to the past.