{"title":"夏季风爆发前后南沙海区上层水域放射虫群:夏季风爆发前后南沙海区上层水域放射虫群","authors":"Lanlan Zhang, Muhong Chen, Rong Xiang, S. Du","doi":"10.3724/SP.J.1140.2012.04025","DOIUrl":null,"url":null,"abstract":"28 towing samples for plankton were collected from the upper waters of the Nansha Islands and its adjacent sea areas in the spring of 2002 and 2004 for understanding the distribution pattern of modern radiolarians and their annual changes in the upper waters of Nansha sea area before and after the summer monsoon onset.The results showed that the dominant species in the spring of 2002 and 2004 were consisting of the tropical-subtropical warm species;however there were obviously annual differences in abundance distributions of radiolarians and their typical species.Noticeably,the radiolarian abundance and its dominant species were significantly different before and after the summer monsoon onset,suggesting that there was a response of radiolarians in upper waters to summer monsoon onset in the South China Sea;The radiolarian abundance after the summer monsoon onset was significantly higher than that before the summer monsoon onset,indicating that the marine environment after the summer monsoon onset would be good for the survive of radiolarians.However,it is necessary to further study the mechanism of the change and try to find more direct environmental parameters to indicate the changes in distribution pattern before and after the summer monsoon onset.This study also confirmed that T.octacantha and S.glacialis could be proxies for upwelling processes in the tropic.","PeriodicalId":18188,"journal":{"name":"海洋地质与第四纪地质","volume":"32 1","pages":"25-32"},"PeriodicalIF":0.0000,"publicationDate":"2013-02-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"RADIOLARIANS IN UPPER WATERS OF NANSHA SEA AREA BEFORE AND AFTER THE SUMMER MONSOON ONSET: RADIOLARIANS IN UPPER WATERS OF NANSHA SEA AREA BEFORE AND AFTER THE SUMMER MONSOON ONSET\",\"authors\":\"Lanlan Zhang, Muhong Chen, Rong Xiang, S. Du\",\"doi\":\"10.3724/SP.J.1140.2012.04025\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"28 towing samples for plankton were collected from the upper waters of the Nansha Islands and its adjacent sea areas in the spring of 2002 and 2004 for understanding the distribution pattern of modern radiolarians and their annual changes in the upper waters of Nansha sea area before and after the summer monsoon onset.The results showed that the dominant species in the spring of 2002 and 2004 were consisting of the tropical-subtropical warm species;however there were obviously annual differences in abundance distributions of radiolarians and their typical species.Noticeably,the radiolarian abundance and its dominant species were significantly different before and after the summer monsoon onset,suggesting that there was a response of radiolarians in upper waters to summer monsoon onset in the South China Sea;The radiolarian abundance after the summer monsoon onset was significantly higher than that before the summer monsoon onset,indicating that the marine environment after the summer monsoon onset would be good for the survive of radiolarians.However,it is necessary to further study the mechanism of the change and try to find more direct environmental parameters to indicate the changes in distribution pattern before and after the summer monsoon onset.This study also confirmed that T.octacantha and S.glacialis could be proxies for upwelling processes in the tropic.\",\"PeriodicalId\":18188,\"journal\":{\"name\":\"海洋地质与第四纪地质\",\"volume\":\"32 1\",\"pages\":\"25-32\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-02-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"海洋地质与第四纪地质\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.3724/SP.J.1140.2012.04025\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"海洋地质与第四纪地质","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.3724/SP.J.1140.2012.04025","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
RADIOLARIANS IN UPPER WATERS OF NANSHA SEA AREA BEFORE AND AFTER THE SUMMER MONSOON ONSET: RADIOLARIANS IN UPPER WATERS OF NANSHA SEA AREA BEFORE AND AFTER THE SUMMER MONSOON ONSET
28 towing samples for plankton were collected from the upper waters of the Nansha Islands and its adjacent sea areas in the spring of 2002 and 2004 for understanding the distribution pattern of modern radiolarians and their annual changes in the upper waters of Nansha sea area before and after the summer monsoon onset.The results showed that the dominant species in the spring of 2002 and 2004 were consisting of the tropical-subtropical warm species;however there were obviously annual differences in abundance distributions of radiolarians and their typical species.Noticeably,the radiolarian abundance and its dominant species were significantly different before and after the summer monsoon onset,suggesting that there was a response of radiolarians in upper waters to summer monsoon onset in the South China Sea;The radiolarian abundance after the summer monsoon onset was significantly higher than that before the summer monsoon onset,indicating that the marine environment after the summer monsoon onset would be good for the survive of radiolarians.However,it is necessary to further study the mechanism of the change and try to find more direct environmental parameters to indicate the changes in distribution pattern before and after the summer monsoon onset.This study also confirmed that T.octacantha and S.glacialis could be proxies for upwelling processes in the tropic.