@article{fdi:010073053,
  title = {{O}n the long-lasting sequences of coral reef terraces from {SE} {S}ulawesi ({I}ndonesia) : distribution, formation, and global significance},
  author = {{P}edoja, {K}. and {H}usson, {L}. and {B}ezos, {A}. and {P}astier, {A}. {M}. and {I}mran, {A}. {M}. and {A}rias-{R}uiz, {C}. and {S}arr, {A}. {C}. and {E}lliot, {M}. and {P}ons-{B}ranchu, {E}. and {N}exer, {M}. and {R}egard, {V}. and {H}afidz, {A}. and {R}obert, {X}avier and {B}enoit, {L}. and {D}elcaillau, {B}. and {A}uthemayou, {C}. and {D}umoulin, {C}. and {C}hoblet, {G}.},
  editor = {},
  language = {{ENG}},
  abstract = {{M}any islands of the eastern {I}ndonesian {A}rchipelago exhibit {L}ate {C}enozoic sequences of coral reef terraces. {I}n {SE} {S}ulawesi, on the {T}ukang {B}esi and {B}uton archipelagos, we identified 23 islands bearing such sequences, {R}emote sensing imagery and field mapping combined to {U}/{T}h and {C}-14 dating enable to establish a chronologic framework of the reef terrace sequences from {W}angi-{W}angi, {B}uton as well as on the neighbouring, smaller islands of {U}lar, {S}iumpu and {K}adatua. {W}e identified the terraces from the last interglacial maximum ({MIS} 5e) at elevations lower than 20 m except on {W} {K}adatua where it is raised at 34 5 m. {S}uch elevations yield low to moderate {U}pper {P}leistocene uplift rates (<0.3 mm yr(-1)). {O}n {SE} {B}uton {I}sland, a sequence culminates at 650 m and includes at least 40 undated strandlines. {N}ext to this exceptional sequence, on the {S}ampolawa {P}eninsula, 18 strandlines culminate at 430 m. {D}ated samples at the base of this sequence (<40m) yield mean {M}iddle {P}leistocene uplift rates of 0.14 +/- 0.09 mm yr(-1). {E}xtrapolation of these uplift rates compared to the geological setting suggests that the sequences of the {S}ampolawa {P}eninsula provide a record of sea-level high-stands for the last 3.8 +/- 0.6 {M}a. {T}he sequences on {SE} {B}uton {I}sland therefore constitute the best preserved long-lasting geomorphic record of {P}lio{Q}uaternary sea-level stands worldwide.},
  keywords = {{I}nterglacial(s) ; {P}leistocene ; {U}-{T}h series ; {S}ulawesi ; {M}arine and coral ; reef terrace ; {INDONESIE} ; {CELEBES}},
  booktitle = {},
  journal = {{Q}uaternary {S}cience {R}eviews},
  volume = {188},
  numero = {},
  pages = {37--57},
  ISSN = {0277-3791},
  year = {2018},
  DOI = {10.1016/j.quascirev.2018.03.033},
  URL = {https://www.documentation.ird.fr/hor/fdi:010073053},
}