2018
DOI: 10.1016/j.margeo.2018.01.012
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The last interglacial (MIS 5e) sea level highstand from a tectonically stable far-field setting, Yorke Peninsula, southern Australia

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Cited by 34 publications
(18 citation statements)
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“…In temperate-latitude locations there is no evidence for local LIG RSL oscillations 2,99 . Without unequivocal empirical evidence for locally falling sea level 96,98 , and considering the uncertainties in coral-growth distributions 90 , the local RSL data provides limited support for >4 m fluctuations in GMSL during the middle of the LIG.…”
Section: Last Interglacial Relative Sea-level Datamentioning
confidence: 93%
See 1 more Smart Citation
“…In temperate-latitude locations there is no evidence for local LIG RSL oscillations 2,99 . Without unequivocal empirical evidence for locally falling sea level 96,98 , and considering the uncertainties in coral-growth distributions 90 , the local RSL data provides limited support for >4 m fluctuations in GMSL during the middle of the LIG.…”
Section: Last Interglacial Relative Sea-level Datamentioning
confidence: 93%
“…A mid-interglacial falling RSL is suggested by a survey of palaeo-shorelines in Western Australia, but the authors explain this by regional solid Earth processes 13 . In Southern Australia, sedimentary evidence points to a single phase of sea-level rise 96 , while on the Yucatán peninsula, Mexico, LIG RSL was stable until a rapid late-interglacial sea-level rise 97 . Such records could be produced if falling GMSL was matched by local land subsidence.…”
Section: Last Interglacial Relative Sea-level Datamentioning
confidence: 99%
“…Last Interglacial coral ages were reported for subtidal deposits on the Yorke Peninsula near Adelaide, South Australia (Pan et al, 2018). Four U-series ages were reported by the authors from 4 unique specimens of the solitary coral Plesiastrea versipora.…”
Section: South Australiamentioning
confidence: 99%
“…Estudis recents, com els de Pan et al (2018), posen de manifest l'existència de testimonis erosius o sedimentaris transgressius part damunt del nivell marí actual, així com Brooke et al (2017) n'identifiquen alguns de transgressius o bé de regressius sotaiguats i que, en concret, a la nostra zona d'estudi es materialitzen en romanents de penya-segats, plataformes litorals i estaques a mitjan plataforma continental, entre 46 i 60 m de profunditat. Les corbes glacioeustàtiques d'abast global, contrastades a l'àmbit regional d'estudi, apunten que els darrers 500 ka BP el registre del nivell marí ha experimentat un mínim de cinc períodes glacials (Grant et al, 2014).…”
Section: Canvis Del Nivell Marí I Carstificacióunclassified
“…Les corbes glacioeustàtiques d'abast global, contrastades a l'àmbit regional d'estudi, apunten que els darrers 500 ka BP el registre del nivell marí ha experimentat un mínim de cinc períodes glacials (Grant et al, 2014). El darrer interglacial (MIS5e) arribaria a ubicar les posicions màximes del paleonivell marí gairebé a 5 m part damunt del nivell actual (ca, 135 ka BP), tot i que la majoria dels registres resten entre 2, 4 i 3 m respecte del nivell de referència hidrogràfic (Pan et al, 2018). Entre el darrer interglacial i prèviament a l'Holocè s'han donat 3 estadis de nivell marí alt (ca.…”
Section: Canvis Del Nivell Marí I Carstificacióunclassified