@Article{EvangelistaGurSifRigBou:2014:SoTrAt,
author = "Evangelista, Heitor and Gurgel, Marcio and Sifeddine, Abdelfettah
and Rigozo, Nivaor Rodolfo and Boussafir, Mohammed",
affiliation = "LARAMG - Lab. de Radioecologia e Mudan{\c{c}}as
Globais/DBB/IBRAG/Uni. do Estado do Rio de Janeiro, Pavilh{\~a}o
Haroldo L. Cunha, Subsolo, Rua S{\~a}o Francisco Xavier, 524,
Maracan{\~a}Rio de Janeiro, RJ, Brazil and School of Arts,
Sciences and Humanities, University of S{\~a}o PauloS{\~a}o
Paulo, Brazil; Av. Arlindo Bettio, 1000S{\~a}o Paulo, SP, Brazil
and Departamento de Geoquimica, Universidade Federal Fluminense,
Departamento de Geoqu{\'{\i}}mica/IQ, Morro de Valongunho S/n, 5
AndarCentro, Niter{\'o}i, RJ, Brazil; IRD-LOCEAN (UMR 7159
IRD/CNRS/UPMC/MNHN)-Institut Pierre-Simon LaplaceBondy, France and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and IRD-LOCEAN
(UMR 7159 IRD/CNRS/UPMC/MNHN)-Institut Pierre-Simon LaplaceBondy,
France",
title = "South Tropical Atlantic anti-phase response to Holocene Bond
Events",
journal = "Palaeogeography, Palaeoclimatology, Palaeoecology",
year = "2014",
volume = "415",
pages = "21--27",
keywords = "alkenone, climate change, climate effect, hematite, Holocene, sea
surface temperature, sediment core, time series, Atlantic Ocean,
Atlantic Ocean (Tropical), Brazil, Caribbean Sea, Gulf of Caraico,
Rio de Janeiro [Brazil].",
abstract = "Records of the climatic impacts of the North Atlantic Bond cycles
over the subtropical Southern Hemisphere remain scarce, and their
mechanism is a topic of active discussion. We present here an
alkenone-based reconstructed sea surface temperature (SST) of a
sediment core retrieved from the Brazilian Southwestern Tropical
Atlantic (SWTA), Rio de Janeiro, together with a sediment SST
record from the Cariaco Basin. The sediment cores span the period
2,100 B.P. - 11,100 B.P. Morlet-wavelet analysis detected marked
periodic signals of ~. 0.8, ~. 1.7 and ~. 2.2. kyr, very similar
and with comparable phases to the hematite-stained-grain time
series from the Northern North Atlantic in which the cyclic
pattern was recognized as Bond cycles. Our result corroborates the
modeled surface ocean anti-phase thermal relation between the
North and the South Atlantic. We attribute this behavior to the
slowing of the Atlantic Meridional Overturning Circulation. The
relative SST warming at Rio de Janeiro and the relative cooling at
Cariaco were comparatively more pronounced during the early
Holocene (from 11 to 5 kyr B.P.) than in more recent time.",
doi = "10.1016/j.palaeo.2014.07.019",
url = "http://dx.doi.org/10.1016/j.palaeo.2014.07.019",
issn = "0031-0182",
label = "scopus 2015-01 EvangelistaGurSifRigBou:2014:SoTrAt",
language = "en",
targetfile = "1-s2.0-S0031018214003745-main.pdf",
urlaccessdate = "27 abr. 2024"
}