@article{fdi:010063594, title = {{S}outh {T}ropical {A}tlantic anti-phase response to {H}olocene bond events}, author = {{E}vangelista, {H}. and {G}urgel, {M}. and {S}ifeddine, {A}bdelfettah and {R}igozo, {N}. {R}. and {B}oussafir, {M}.}, editor = {}, language = {{ENG}}, abstract = {{R}ecords of the climatic impacts of the {N}orth {A}tlantic {B}ond cycles over the subtropical {S}outhern {H}emisphere remain scarce, and their mechanism is a topic of active discussion. {W}e present here an alkenone-based reconstructed sea surface temperature ({SST}) of a sediment core retrieved from the {B}razilian {S}outhwestern {T}ropical {A}tlantic ({SWTA}), {R}io de {J}aneiro, together with a sediment {SST} record from the {C}ariaco {B}asin. {T}he sediment cores span the period 2,100 {B}.{P}. - 11,100 {B}.{P}. {M}orlet-wavelet analysis detected marked periodic signals of similar to 0.8, similar to 1.7 and similar to 2.2 kyr, very similar and with comparable phases to the hematite-stained-grain time series from the {N}orthern {N}orth {A}tlantic in which the cyclic pattern was recognized as {B}ond cycles. {O}ur result corroborates the modeled surface ocean anti-phase thermal relation between the {N}orth and the {S}outh {A}tlantic. {W}e attribute this behavior to the slowing of the {A}tlantic {M}eridional {O}verturning {C}irculation. {T}he relative {SST} warming at {R}io de {J}aneiro and the relative cooling at {C}ariaco were comparatively more pronounced during the early {H}olocene (from {II} to 5 kyr {B}.{P}.) than in more recent time.}, keywords = {{B}ond cycles ; {A}tlantic overturning ; {S}outh {A}tlantic ; {H}olocene ; {A}lkenone ; {ATLANTIQUE} {SUD} ; {ZONE} {TROPICALE} ; {BRESIL}}, booktitle = {{C}ontinental and coastal marine records of centennial to millennial changes in {S}outh {A}merican climate since the last glacial maximum}, journal = {{P}alaeogeography {P}alaeoclimatology {P}alaeoecology}, volume = {415}, numero = {no sp{\'e}cial}, pages = {21--27}, ISSN = {0031-0182}, year = {2014}, DOI = {10.1016/j.palaeo.2014.07.019}, URL = {https://www.documentation.ird.fr/hor/fdi:010063594}, }