Sea-level fluctuations during the last glacial cycle

By Mark Siddall, E. Rohling, A. Almogi‐Labin, C. Hemleben, D. Meischner, I. Schmelzer, D. Smeed. Nature, 2003

1,622 citations recorded by the source corpus.

Subfields: Archeology, Atmospheric Science, Ecology

View Paper: https://www.semanticscholar.org/paper/a39f90726c48d2307b1e2e2f9ad621a4b6a1ba5e

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Citations in the corpus

ASSESSING THE TAXONOMIC STATUS OF THE PALAWAN PANGOLIN MANIS CULIONENSIS (PHOLIDOTA) USING DISCRETE MORPHOLOGICAL CHARACTERS (2005, background): “Because water depth between Borneo and Palawan approximates 145 m, subsequent lowering of sea levels during the 4 last glacial cycles is unlikely to have allowed transmigrations between the 2 islands (Meijaard 2003; Petit et al. 1999; Siddall et al. 2003).”
The process, biotic impact, and global implications of the human colonization of Sahul about 47,000 years ago (2015, background): “…attractive to foragers, despite the frequent, high amplitude changes in sea level characteristic of this period (Marine Isotope Stage 3 [MIS-3], 30e60 ka; Siddall et al., 2003), given the capacities of resident fauna (specifically shellfish) to adjust to those changes in real time (Beaton, 1995).”
Absence of post‐Miocene Red Sea land bridges: biogeographic implications (2006, methodology): “A combined model of Red Sea exchange over Hanish Sill and stable oxygen isotope fractionation in the basin ( Siddall et al., 2003 ) can be used to calculate the relationship between Red Sea stable oxygen isotope ratios and water depth above Hanish Sill.”
Mass extinctions and ocean acidification: biological constraints on geological dilemmas (2008, background): “We have specific data on this subject from the last glacial cycle, when the sea dropped 130 m (Lambeck and Chappell 2001; Siddall et al. 2003 ).”
Sea-level rise due to polar ice-sheet mass loss during past warm periods (2015, background): “On the other hand, the Red Sea planktic d(18)O record suggests that RSL reached just above present (1 ± 12 m at 2s) (55, 56).”
Marine isotope stage 3 sea level fluctuations: Data synthesis and new outlook (2008, methodology): “[40] This method was developed for planktic foraminiferal records [Siddall et al., 2003, 2004] because the long seawater residence times in the Red Sea at times of low sea levels would cause a long time integration in benthic records.”
Target atmospheric CO2: Where should humanity aim? (2008, neutral): “Equilibrium sea level rise for today’s 385 ppm CO2 is at least several meters, judging from paleoclimate history [19, 32-34].”
Isotope calibrated Greenland temperature record over Marine Isotope Stage 3 and its relation to CH4 (2006, background): “2, before DO 14, cannot clearly be associated with a H-event, but some sediment proxies as well as sea level changes show Hlike behaviour [41,42,13].”
The mammals of Palawan Island, Philippines (2004, background): “Reis & Garong (2001) reported a specimen from sediments in a rock-shelter near Tabon Cave, Quezon Municipality dated to 11,130 BP.”
The roles of geological history and colonization abilities in genetic differentiation between mammalian populations in the Philippine archipelago (2005, background): “During the most recent period of low sea level in the Pleistocene, c. 18,000 years ago (Fairbanks, 1989; Siddall et al., 2003), many current islands merged into four large islands: Greater Luzon, Greater Mindanao, Greater NegrosPanay, and Greater Palawan (Fig.”
An Unshakable Middle Paleolithic? (2013, background): “Siddall and colleagues (Siddall, Chappell, and Potter 2006; Siddall et al. 2003) identify the climate intervals of 40–80, 120–140, and 160–200 ka as particularly variable based on Red Sea–Ocean proxies for global sea level changes.”
Sea-level probability for the last deglaciation: A statistical analysis of far-field records (2011, background): “Since the Last Glacial Maximum (LGM), sea level has risen by around 120 m or so (e.g., Fairbanks, 1989; Bard et al., 1990a,b, 1996; Lambeck et al., 2002; Siddall et al., 2003; Peltier and Fairbanks, 2006).”
Dangerous human-made interference with climate: a GISS modelE study (2006, background): “Other studies provide evidence of large ( ∼ 10 m or more) changes of sea level on “sub-orbital” time scales (Siddall et al., 2003; Potter et al., 2004; Thompson and Goldstein, 2005), i.e. sea level changes occurring much more rapidly than changes of the Earth’s orbital elements.”