{"refrec":{"BRefID":361508,"RR":"<b>Lo, L.; Shen, C.-C.; Zeeden, C.; Tsai, Y.-H.; Yin, Q.; Yang, C.-C.; Chang, T.-L.; Su, Y.-C.; Mii, H.-S.; Chuang, C.-K.; Chen, Y.-C.</b> (2022). Orbital control on the thermocline structure during the past 568 kyr in the Solomon Sea, southwest equatorial Pacific. <i>Quat. Sci. Rev. 295</i>: 107756. <a href=\"https://dx.doi.org/10.1016/j.quascirev.2022.107756\" target=\"_blank\">https://dx.doi.org/10.1016/j.quascirev.2022.107756</a>","BEntID":359224,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Quat. Sci. Rev. 295</i>: 107756. <a href=\"https://dx.doi.org/10.1016/j.quascirev.2022.107756\" target=\"_blank\">https://dx.doi.org/10.1016/j.quascirev.2022.107756</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lo, L.; Shen, C.-C.; Zeeden, C.; Tsai, Y.-H.; Yin, Q.; Yang, C.-C.; Chang, T.-L.; Su, Y.-C.; Mii, H.-S.; Chuang, C.-K.; Chen, Y.-C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lo, L. <i>et al.</i>","Englishabstract":"The Solomon Sea is the main source of the equatorial undercurrent and the main crossroad of the equatorial region and the South Pacific Ocean. Based on multi-species planktonic foraminiferal geochemical proxies, here we reconstruct the vertical thermal-hydrological variabilities over the last 568,000 years in the Solomon Sea. The proxies used include the differences between δ<sup>18</sup>O data of the surface dweller <i>Globigerinoides ruber</i> (white) and the subsurface dweller <i>Pulleniatina obliquiloculata</i> (Δδ<sup>18</sup>O<sub>c</sub>), the sea surface temperature (SST) and the upper thermocline temperature (UTT) as well as their differences (ΔT), and the seawater oxygen isotope differences (Δδ<sup>18</sup>O<sub>w</sub>). Both the SST and UTT records feature similar timing of warming, which is 2–4 kyr earlier than the G/IG boundaries for the past six terminations. Different from the other five terminations, both SST and UTT records of Termination V show a persistent and early increase of 5–7 °C in 10 kyr since ∼440 ka. On the obliquity band, higher SST and UTT correspond to larger obliquity, suggesting higher subtropical South Pacific input. This argument is supported by lower ΔT and higher Δδ<sup>18</sup>O<sub>w</sub>. In the meantime, higher SST and UTT also correspond to precession minimum, suggesting an expansion of the mixed layer with lower ΔT and greater Δδ<sup>18</sup>O<sub>w</sub>. Our results show complex interactions between precipitation-evaporation and water masses exchange in the Solomon Sea. The clear obliquity signal observed in multiple proxies reveals strong interactions between the Solomon Sea and the mid-high latitude South Pacific regions.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Orbital control on the thermocline structure during the past 568 kyr in the Solomon Sea, southwest equatorial Pacific","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-23 01:33:20.603435","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Thermocline structure; Orbital forcing; Western pacific warm pool; Terminations","OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2023-02-28","DateCreate":"2023-02-27","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000866402400008","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.quascirev.2022.107756"},"refs":null,"anarec":{"AnaID":361508,"PubliDate":2022,"Pagination":"107756","XtraPublOfAnaID":null,"ISBN":null,"Volume":"295","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45667,"SerRR":"Quaternary Science Reviews. 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