{"title":"热带西太平洋浮游有孔虫稳定氧同位素比值的垂直和季节变化及栖息地深度估算","authors":"Tae Wook Ko , Kyung Eun Lee , Ryoung Ah Kim","doi":"10.1016/j.dsr.2024.104440","DOIUrl":null,"url":null,"abstract":"<div><div>To verify the habitat depth of planktonic foraminifera, the variability of foraminiferal δ<sup>18</sup>O (δ<sup>18</sup>O<sub>pforam</sub>) by depth, season, day and night was investigated over a water depth of 0–600 m in the western tropical Pacific region. Species that inhabit the surface mixed layer in April include <em>Globigerinoides sacculifer, Globigerinoides ruber</em> white<em>, Globigerinoides conglobatus, Globigerinella siphonifera,</em> and <em>Orbulina universa</em> (δ<sup>18</sup>O<sub>pforam</sub>, −2.2‰ to –2.9‰). Meanwhile, <em>Globorotalia hirsuta</em> and <em>Globorotaloides hexagonus</em> inhabit the upper thermocline (δ<sup>18</sup>O<sub>pforam</sub>, −0.3‰to –1.2‰) and lower thermocline (δ<sup>18</sup>O<sub>pforam</sub>, 1.2‰), respectively. In August, various species inhabit the uppermost thermocline during the day (<em>G. sacculifer</em>, <em>G. ruber</em> white, <em>G. siphonifera</em>, <em>G. conglobatus</em>, <em>O. universa</em>, <em>Globorotalia menardii</em>, <em>Hastigerina pelagica</em>, <em>Neogloboquadrina dutertrei</em>, <em>Pulleniatina obliquiloculata</em>, and <em>Globoquadrina conglomerata</em>) (δ<sup>18</sup>O<sub>pforam</sub>, −2.2‰ to –3.2‰). At night, <em>G. sacculifer</em> without sac and <em>G. menardii</em> appear to inhabit the surface mixed layer (δ<sup>18</sup>O<sub>pforam</sub>, −2.9‰ to –3.4‰). <em>G. hexagonus</em> inhabits the lower thermocline (δ<sup>18</sup>O<sub>pforam</sub>, 1.3‰) in August. The vertical distribution of δ<sup>18</sup>O<sub>pforam</sub> in December was similar to that of April δ<sup>18</sup>O<sub>pforam</sub>. The habitat depths inferred from δ<sup>18</sup>O<sub>pforam</sub> were mostly consistent with those estimated from species abundance. Species that did not match were <em>Globorotalia truncatulinoides</em> (in April), <em>Globigerinoides elongatus</em> (in December), <em>G. hirsuta</em> (in August), and <em>G. hexagonus</em> (in December). The results of δ<sup>18</sup>O analysis suggest that <em>G. truncatulinoides</em> lives in the uppermost thermocline, and <em>G. elongatus</em> in the surface mixed layer. In the case of <em>G. hirsuta</em> and <em>G. hexagonus</em>, they inhabit the upper thermocline and lower thermocline, respectively. Our results contribute to research on reconstructing past thermocline structure using geochemical analysis of planktonic foraminifera in marine sediments in this region.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"216 ","pages":"Article 104440"},"PeriodicalIF":2.3000,"publicationDate":"2025-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Vertical and seasonal variations in stable oxygen isotope ratio of living planktonic foraminifera and estimation of habitat depth in the western tropical Pacific\",\"authors\":\"Tae Wook Ko , Kyung Eun Lee , Ryoung Ah Kim\",\"doi\":\"10.1016/j.dsr.2024.104440\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>To verify the habitat depth of planktonic foraminifera, the variability of foraminiferal δ<sup>18</sup>O (δ<sup>18</sup>O<sub>pforam</sub>) by depth, season, day and night was investigated over a water depth of 0–600 m in the western tropical Pacific region. Species that inhabit the surface mixed layer in April include <em>Globigerinoides sacculifer, Globigerinoides ruber</em> white<em>, Globigerinoides conglobatus, Globigerinella siphonifera,</em> and <em>Orbulina universa</em> (δ<sup>18</sup>O<sub>pforam</sub>, −2.2‰ to –2.9‰). Meanwhile, <em>Globorotalia hirsuta</em> and <em>Globorotaloides hexagonus</em> inhabit the upper thermocline (δ<sup>18</sup>O<sub>pforam</sub>, −0.3‰to –1.2‰) and lower thermocline (δ<sup>18</sup>O<sub>pforam</sub>, 1.2‰), respectively. In August, various species inhabit the uppermost thermocline during the day (<em>G. sacculifer</em>, <em>G. ruber</em> white, <em>G. siphonifera</em>, <em>G. conglobatus</em>, <em>O. universa</em>, <em>Globorotalia menardii</em>, <em>Hastigerina pelagica</em>, <em>Neogloboquadrina dutertrei</em>, <em>Pulleniatina obliquiloculata</em>, and <em>Globoquadrina conglomerata</em>) (δ<sup>18</sup>O<sub>pforam</sub>, −2.2‰ to –3.2‰). At night, <em>G. sacculifer</em> without sac and <em>G. menardii</em> appear to inhabit the surface mixed layer (δ<sup>18</sup>O<sub>pforam</sub>, −2.9‰ to –3.4‰). <em>G. hexagonus</em> inhabits the lower thermocline (δ<sup>18</sup>O<sub>pforam</sub>, 1.3‰) in August. The vertical distribution of δ<sup>18</sup>O<sub>pforam</sub> in December was similar to that of April δ<sup>18</sup>O<sub>pforam</sub>. The habitat depths inferred from δ<sup>18</sup>O<sub>pforam</sub> were mostly consistent with those estimated from species abundance. Species that did not match were <em>Globorotalia truncatulinoides</em> (in April), <em>Globigerinoides elongatus</em> (in December), <em>G. hirsuta</em> (in August), and <em>G. hexagonus</em> (in December). The results of δ<sup>18</sup>O analysis suggest that <em>G. truncatulinoides</em> lives in the uppermost thermocline, and <em>G. elongatus</em> in the surface mixed layer. In the case of <em>G. hirsuta</em> and <em>G. hexagonus</em>, they inhabit the upper thermocline and lower thermocline, respectively. Our results contribute to research on reconstructing past thermocline structure using geochemical analysis of planktonic foraminifera in marine sediments in this region.</div></div>\",\"PeriodicalId\":51009,\"journal\":{\"name\":\"Deep-Sea Research Part I-Oceanographic Research Papers\",\"volume\":\"216 \",\"pages\":\"Article 104440\"},\"PeriodicalIF\":2.3000,\"publicationDate\":\"2025-02-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Deep-Sea Research Part I-Oceanographic Research Papers\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0967063724002103\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"OCEANOGRAPHY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Deep-Sea Research Part I-Oceanographic Research Papers","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0967063724002103","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"OCEANOGRAPHY","Score":null,"Total":0}
Vertical and seasonal variations in stable oxygen isotope ratio of living planktonic foraminifera and estimation of habitat depth in the western tropical Pacific
To verify the habitat depth of planktonic foraminifera, the variability of foraminiferal δ18O (δ18Opforam) by depth, season, day and night was investigated over a water depth of 0–600 m in the western tropical Pacific region. Species that inhabit the surface mixed layer in April include Globigerinoides sacculifer, Globigerinoides ruber white, Globigerinoides conglobatus, Globigerinella siphonifera, and Orbulina universa (δ18Opforam, −2.2‰ to –2.9‰). Meanwhile, Globorotalia hirsuta and Globorotaloides hexagonus inhabit the upper thermocline (δ18Opforam, −0.3‰to –1.2‰) and lower thermocline (δ18Opforam, 1.2‰), respectively. In August, various species inhabit the uppermost thermocline during the day (G. sacculifer, G. ruber white, G. siphonifera, G. conglobatus, O. universa, Globorotalia menardii, Hastigerina pelagica, Neogloboquadrina dutertrei, Pulleniatina obliquiloculata, and Globoquadrina conglomerata) (δ18Opforam, −2.2‰ to –3.2‰). At night, G. sacculifer without sac and G. menardii appear to inhabit the surface mixed layer (δ18Opforam, −2.9‰ to –3.4‰). G. hexagonus inhabits the lower thermocline (δ18Opforam, 1.3‰) in August. The vertical distribution of δ18Opforam in December was similar to that of April δ18Opforam. The habitat depths inferred from δ18Opforam were mostly consistent with those estimated from species abundance. Species that did not match were Globorotalia truncatulinoides (in April), Globigerinoides elongatus (in December), G. hirsuta (in August), and G. hexagonus (in December). The results of δ18O analysis suggest that G. truncatulinoides lives in the uppermost thermocline, and G. elongatus in the surface mixed layer. In the case of G. hirsuta and G. hexagonus, they inhabit the upper thermocline and lower thermocline, respectively. Our results contribute to research on reconstructing past thermocline structure using geochemical analysis of planktonic foraminifera in marine sediments in this region.
期刊介绍:
Deep-Sea Research Part I: Oceanographic Research Papers is devoted to the publication of the results of original scientific research, including theoretical work of evident oceanographic applicability; and the solution of instrumental or methodological problems with evidence of successful use. The journal is distinguished by its interdisciplinary nature and its breadth, covering the geological, physical, chemical and biological aspects of the ocean and its boundaries with the sea floor and the atmosphere. In addition to regular "Research Papers" and "Instruments and Methods" papers, briefer communications may be published as "Notes". Supplemental matter, such as extensive data tables or graphs and multimedia content, may be published as electronic appendices.