Into and out of the Last Glacial Maximum: sea-level change during Oxygen Isotope Stages 3 and 2

Lambeck, Kurt; Yokoyama, Yūsuke; Purcell, Anthony

doi:10.1016/s0277-3791(01)00071-3

Cited by 663 publications

(458 citation statements)

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“…The first melt water pulse occurred at 19 cal ka BP, when sea level began to rise relatively slowly at arate of about 3.3mma-l , until16calkaBP. The melt water pulse lA (MWP-1A) of Fairbanks (1989) and Bard et al (1990) was characterised by increases of the rate of sea level rise that amounted up to 15 mm a -1, between 16 and 12.5 cal ka BP and, again, between 11.5 and 9 cal ka BP (Lambeck et al, 2002). A short duration plateau in sea level rise may have occurred at about 12.5-1 1.5 cal ka BP, corresponding to the Younger Dryas (Lambeck et al , 2002).…”

Section: E-mail Address: Rncnzc65 @Rnncncsices (E Zazo)mentioning

confidence: 99%

“…The melt water pulse lA (MWP-1A) of Fairbanks (1989) and Bard et al (1990) was characterised by increases of the rate of sea level rise that amounted up to 15 mm a -1, between 16 and 12.5 cal ka BP and, again, between 11.5 and 9 cal ka BP (Lambeck et al, 2002). A short duration plateau in sea level rise may have occurred at about 12.5-1 1.5 cal ka BP, corresponding to the Younger Dryas (Lambeck et al , 2002). Around 7 cal ka BP the surface of the ocean was approaching the present level, but did not reach it until sorne time later (Lambeck et al , 2002).…”

Section: E-mail Address: Rncnzc65 @Rnncncsices (E Zazo)mentioning

confidence: 99%

“…A short duration plateau in sea level rise may have occurred at about 12.5-1 1.5 cal ka BP, corresponding to the Younger Dryas (Lambeck et al , 2002). Around 7 cal ka BP the surface of the ocean was approaching the present level, but did not reach it until sorne time later (Lambeck et al , 2002). Since then, the distribution of oceanic water masses largely driven by superficial currents has come to replace the glacio-eustatic component as the main control of global sea level (Morner, 1996).…”

Section: E-mail Address: Rncnzc65 @Rnncncsices (E Zazo)mentioning

confidence: 99%

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The coastal archives of the last 15ka in the Atlantic–Mediterranean Spanish linkage area: Sea level and climate changes

Cardeña

Dabrio

Goy

et al. 2008

Quaternary International

106

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Sea level and clima te changes archived in various coastal environments during the last part of the last glacial and present interglacial periods are investigated by interpolating available geomorphology, sedimentology, palaeontology and geochronology data. The coastal response to these changes depended on the environment and geographic location. Changes of sea level during the rising, transgressive phase are well recorded in the sedimentary filling of the estuaries, whereas during the phase of highstand they are best recorded in beach-barrier environments. The postglacial rise of sea level took place in two phases: a rapid rise until 6500 cal BP, and a second phase of near stability with minor oscillations of metric magnitude. Regarding climate changes, there is no record of changing temperatures in the coastal zones of southern Spain, although there is in precipitation and wind intensityjvelocity. After 7-5 cal ka BP, the general climatic trend towards aridity was punctuated by several short-lived (centennial) episodes of increased aridity that occurred with a millennial cycle, often coincident with Bond cool events and, in sorne cases, with decreases of sea surface temperatures. The absence of human in ter ventio n in vegetation composition until 2000 BP suggests that most environmental coastal shifts were climatically driven,

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Section: E-mail Address: Rncnzc65 @Rnncncsices (E Zazo)mentioning

confidence: 99%

Section: E-mail Address: Rncnzc65 @Rnncncsices (E Zazo)mentioning

confidence: 99%

Section: E-mail Address: Rncnzc65 @Rnncncsices (E Zazo)mentioning

confidence: 99%

See 1 more Smart Citation

The coastal archives of the last 15ka in the Atlantic–Mediterranean Spanish linkage area: Sea level and climate changes

Cardeña

Dabrio

Goy

et al. 2008

Quaternary International

106

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“…Furthermore, sea-level changes in far-field locations (those with a distal position from formerly glaciated areas), are of interest, as they provide the most robust constraints on the eustatic component of the sea-level signal (e.g. Nakada and Lambeck 1989;Fleming et al 1998;Lambeck 2002;Milne et al 2002;Peltier 2002) and can be employed to constrain the source geometry of major meltwater pulses (Clark et al 2002;Bassett et al 2005). The use of coral reconstructions (Fairbanks 1989;Chappell and Polach 1991;Bard et al 1996) has proved extremely useful for reconstructions prior to the Holocene but the large error ranges (±2.5m , Fairbanks 1989;±5m Blanchon 2005) limit their use for Holocene reconstructions where the error is often greater than the magnitude of the change being investigated.…”

Section: Introductionmentioning

confidence: 99%

Mangrove pollen of Indonesia and its suitability as a sea-level indicator

et al. 2007

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The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-pro t purposes provided that:• a full bibliographic reference is made to the original source• a link is made to the metadata record in Durham E-Theses• the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Mangrove Pollen of Indonesia and its Suitability as a Sea-Level IndicatorThe copyright of this thesis rests with the author or the university to which it was submitted. No quotation from it, or information derived from it may be published without the prior written consent of the author or university, and any information derived from it should be acknowledged. Simon Edward EngelhartThesis The copyright of this thesis rests with the author. No quotations from it should be published without his prior written consent and information derived from it should be acknowledged.11 AcknowledgemeBlts I would like to thank all those people who have helped in the production of this thesis.

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“…between 26,000 and 35,000 yr BP). To avoid the potential for meteoric alteration, the rate of subsidence in such locales would have to be extremely large, on the order 3 to 12 mm/yr (Lambeck et al, 2002;Siddall et al, 2003). No such reefs have yet been exploited for radiocarbon calibration purposes.…”

Section: Data Quality and Screeningmentioning

confidence: 99%

Comment on “Radiocarbon calibration curve spanning 0 to 50,000 years BP based on paired 230Th/234U/238U and 14C dates on pristine corals” by R.G. Fairbanks et al. (Quaternary Science Reviews 24 (2005) 1781–1796)☆☆doi of original article: 10.1016/j.quascirev.2005.04.007 and “Extending the radiocarbon calibration beyond 26,000 years before present using fossil corals” by T.-C. Chiu et al. (Quaternary Science Reviews 24 (2005) 1797–1808)☆☆☆☆doi of original article: 10.1016/j.quascirev.2005.04.002

Reimer

Baillie

McCormac

et al. 2006

Quaternary Science Reviews

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A recently published radiocarbon calibration curve extending to 50,000 cal BP ) is purportedly superior to that generated by the IntCal working group beyond the end of the tree-ring data at 12,400 cal BP ). This claim is based, in part, on different diagenetic screening criteria and pretreatment for coral samples Chiu et al. 2005) which do not stand up under careful scrutiny. Also at issue is the conversion of the coral-based calibration curve to an atmospheric curve where large inter-annual variability in the sea-surface age reservoir age has been observed in the southwest Pacific where one of two sets of corals used were sampled. In addition we comment on the seemingly ad hoc statistical methods utilized by Fairbanks et al. (2005) to construct their curve. We recognize the value of the Fairbanks et al. (2005) coral radiocarbon data set, but reassert the need for multiple, independently derived data to provide confirmation and validation to all radiocarbon calibration data. This is especially important before 26,000 cal BP when lower sea-levels of the last glacial maximum exposed most coral samples to alteration by fresh water

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Into and out of the Last Glacial Maximum: sea-level change during Oxygen Isotope Stages 3 and 2

Cited by 663 publications

References 55 publications

The coastal archives of the last 15ka in the Atlantic–Mediterranean Spanish linkage area: Sea level and climate changes

The coastal archives of the last 15ka in the Atlantic–Mediterranean Spanish linkage area: Sea level and climate changes

Mangrove pollen of Indonesia and its suitability as a sea-level indicator

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