Journal Title：Paleoceanography And Paleoclimatology

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.

古海洋學(xué)和古氣候?qū)W (PALO) 發(fā)表有關(guān)過去環(huán)境、生物群和氣候記錄的論文。要了解過去的地球系統(tǒng)，需要采用多種方法，包括海洋和湖泊沉積學(xué)和洞穴沉積物；冰蓋的形成和流動；穩(wěn)定同位素、微量元素和有機(jī)地球化學(xué)；古生物學(xué)和分子古生物學(xué)；進(jìn)化過程；生物體內(nèi)的礦化作用；了解樹木年輪的形成；地震地層學(xué)；物理、化學(xué)和生物海洋學(xué)；地球化學(xué)、氣候和地球系統(tǒng)建模等。該期刊的范圍是區(qū)域到全球，而不是本地，包括任何地質(zhì)時(shí)代的研究（前寒武紀(jì)到第四紀(jì)，包括現(xiàn)代類似物）。在此框架內(nèi)，將包括以下主題的論文：年代學(xué)、地層學(xué)（與古海洋學(xué)事件的相關(guān)性相關(guān)）、古構(gòu)造、古海洋學(xué)建模、古環(huán)流（深、中、淺）、古氣候?qū)W（例如古風(fēng)和冰凍圈歷史）、全球沉積物和地球化學(xué)循環(huán)、缺氧、海平面變化和影響、生物進(jìn)化與古海洋學(xué)的關(guān)系、生物危機(jī)、古生物學(xué)（例如古海洋學(xué)中使用的“微化石”生態(tài)學(xué)）、古海洋學(xué)推斷的技術(shù)和方法、現(xiàn)代古海洋學(xué)類似物、以及耦合海洋-大氣-生物圈過程的定量和綜合分析。古海洋學(xué)和古氣候研究使我們能夠利用過去來獲取有關(guān)未來氣候和生物發(fā)展的信息：過去是未來的關(guān)鍵，就像現(xiàn)在是過去的關(guān)鍵一樣，甚至可能比現(xiàn)在更重要。

Paleoceanography And Paleoclimatology創(chuàng)刊于2018年，由Wiley-Blackwell出版商出版，收稿方向涵蓋Earth and Planetary Sciences - Atmospheric Science全領(lǐng)域，此刊是該細(xì)分領(lǐng)域中屬于非常不錯(cuò)的SCI期刊，在行業(yè)細(xì)分領(lǐng)域中學(xué)術(shù)影響力較大，專業(yè)度認(rèn)可很高，所以對原創(chuàng)文章要求創(chuàng)新性較高，如果您的文章質(zhì)量很高，可以嘗試。平均審稿速度 ，影響因子指數(shù)3.2，該期刊近期沒有被列入國際期刊預(yù)警名單，廣大學(xué)者值得一試。