Titre du document / Document title
Instability of seawater pH in the South China Sea during the mid-late Holocene : Evidence from boron isotopic composition of corals
Auteur(s) / Author(s)
YI LIU ;
WEIGUO LIU ;
ZICHENG PENG ;
YINGKAI XIAO ;
GANGJIAN WEI ;
WEIDONG SUN ;
JIANFENG HE ;
GUIJIAN LIU ;
CHOU Chen-Lin ;
Résumé / Abstract
We used positive thermal ionization mass spectrometry (PTIMS) to generate high precision δ
11B records in Porites corals of the mid-late Holocene from the South China Sea (SCS). The δ
11B values of the Holocene corals vary significantly, ranging from 22.2‰ to 25.5‰. The paleo-pH records of the SCS, reconstructed from the δ
11B data, were not stable as previously thought but show a gradual increase from the Holocene thermal optimal and a sharp decrease to modern values. The latter is likely caused by the large amount of anthropogenic CO
2 emissions since the Industrial Revolution but variations of atmospheric pCO
2 cannot explain the pH change of the SCS before the Industrial Revolution. We suggest that variations of monsoon intensity during the mid-late Holocene may have driven the sea surface pH increase from the mid to late Holocene. Results of this study indicate that the impact of anthropogenic atmospheric CO
2 emissions may have reversed the natural pH trend in the SCS since the mid-Holocene. Such ocean pH records in the current interglacial period can help us better understand the physical and biological controls on ocean pH and possibly predict the long-term impact of climate change on future ocean acidification.
Revue / Journal Title
Geochimica et cosmochimica acta
ISSN
0016-7037
CODEN GCACAK
Source / Source
2009, vol. 73, n
o5, pp. 1264-1272 [9 page(s) (article)]
Langue / Language
Anglais
Editeur / Publisher
Elsevier, Kidlington, ROYAUME-UNI
(1950)
(Revue)
Localisation / Location
INIST-CNRS, Cote INIST : 5743, 35400018696964.0040
Nº notice refdoc (ud4) : 21191320