@article{fdi:010049220,
  title = {{T}he sea-level conundrum: case studies from palaeo-archives},
  author = {{S}iddall, {M}. and {A}be-{O}uchi, {A}. and {A}ndersen, {M}. and {A}ntonioli, {F}. and {B}amber, {J}. and {B}ard, {E}. and {C}lark, {J}. and {C}lark, {P}. and {D}eschamps, {P}ierre and {D}utton, {A}. and {E}lliot, {M}. and {G}allup, {C}. and {G}omez, {N}. and {G}regory, {J}. and {H}uybers, {P}. and {K}awarnura, {K}. and {K}elly, {M}. and {L}ambeck, {K}. and {L}owell, {T}. and {M}ilrovica, {J}. and {O}tto-{B}liesner, {B}. and {R}ichards, {D}. and {S}tanford, {J}. and {S}tirling, {C}. and {S}tocker, {T}. and {T}homas, {A}. and {T}hompson, {B}. and {T}ornqvist, {T}. and {R}iveiros, {N}. {V}. and {W}aelbroeck, {C}. and {Y}okoyama, {Y}. and {Y}u, {S}. {Y}.},
  editor = {},
  language = {{ENG}},
  abstract = {{U}ncertainties in sea-level projections for the 21st century have focused ice sheet modelling efforts to include the processes that are thought to be contributing to the recently observed rapid changes at ice sheet margins. {T}his effort is still in its infancy, however, leaving us unable to make reliable predictions of ice sheet responses to a warming climate if such glacier accelerations were to increase in size and frequency. {T}he geological record, however, has long identified examples of nonlinear ice sheet response to climate forcing ({S}hackleton {NJ}, {O}pdyke {ND}. 1973. {O}xygen isotope and paleomagnetic stratigraphy of equatorial {P}acific core {V}28-239, late {P}liocene to latest {P}leistocene. {G}eological {S}ociety of {A}merica {M}emoirs 145: 449-464; {F}airbanks {RG}. 1989. {A} 17,000 year glacio-eustatic sea level record: influence of glacial melting rates on the {Y}ounger {D}ryas event and deep ocean circulation. {N}ature 342: 637-642; {B}ard {E}, {H}amelin {B}, {A}rnold {M}, {M}ontaggioni {L}, {C}abioch {G}, {F}aure {G}, {R}ougerie {F}. 1996. {S}ea level record from {T}ahiti corals and the timing of deglacial meltwater discharge. {N}ature 382: 241-244), thus suggesting an alternative strategy for constraining the rate and magnitude of sea-level change that we might expect by the end of this century.},
  keywords = {sea level ; climate change ; ice sheets},
  booktitle = {},
  journal = {{J}ournal of {Q}uaternary {S}cience},
  volume = {25},
  numero = {1},
  pages = {19--25},
  ISSN = {0267-8179},
  year = {2010},
  DOI = {10.1002/jqs.1270},
  URL = {https://www.documentation.ird.fr/hor/fdi:010049220},
}