2001
DOI: 10.1016/s0031-0182(01)00202-4
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Warmer or cooler late Holocene marine palaeoenvironments?: interpreting southeast Australian and Brazilian sea-level changes using fixed biological indicators and their δ18O composition

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Cited by 49 publications
(56 citation statements)
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“…This coincides with a time at which higher temperatures have been indicated by isotopic proxies in corals on the Great Barrier Reef (Gagan et al, 1998), and in worm tubes in eastern Australia (Baker et al, 2001). It remains unproven, however, whether sea-surface temperatures were higher at Lord Howe Island.…”
Section: Discussionsupporting
confidence: 64%
“…This coincides with a time at which higher temperatures have been indicated by isotopic proxies in corals on the Great Barrier Reef (Gagan et al, 1998), and in worm tubes in eastern Australia (Baker et al, 2001). It remains unproven, however, whether sea-surface temperatures were higher at Lord Howe Island.…”
Section: Discussionsupporting
confidence: 64%
“…This is further expanded by Baker et al (2001a) et al ( 1979) suggest that the area was not affected by tectonic subsidence or uplift at least during the Holocene.…”
Section: Lithostratigraphic Approachmentioning
confidence: 67%
“…This period is characterized by a net lowering of sea level, possibly with less fluctuation than the early period (Baker, Haworth and Flood, 2001), but still impacting on vertical growth of the reef surfaces. Reef growth would be inhibited with a slow and relatively steady sea level fall.…”
Section: Years Bp To 1500 Years Admentioning
confidence: 99%