Sabiia Seb
PortuguêsEspañolEnglish
Embrapa
        Busca avançada

Botão Atualizar


Botão Atualizar

Ordenar por: 

RelevânciaAutorTítuloAnoImprime registros no formato resumido
Registros recuperados: 12
Primeira ... 1 ... Última
Imagem não selecionada

Imprime registro no formato completo
Mg/Ca ratios in the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in the northern North Atlantic/Nordic Seas ArchiMer
Meland, My; Jansen, E; Elderfield, H; Dokken, Tm; Olsen, A; Bellerby, Rgj.
In core top samples in the Nordic Seas, Mg/Ca ratios of N. pachyderma ( sin.) are generally consistent with previous high-latitude calibration data but do not reflect the modern calcification temperature gradient from 2 degrees C in the northwest to 8 degrees C in the southeast. This is because Mg/Ca ratios in foraminiferal shells from the central Nordic Seas are similar to 0.4 mmol/mol higher than expected from calibrations of Nurnberg ( 1995) and Elderfield and Ganssen ( 2000). The enhanced Mg/Ca ratios are observed in an area with low sedimentation rates (< similar to 5 cm/kyr). Possible factors that may cause this include bioturbation, Holocene variability in old core tops, dissolution, pore water chemistry, occurrence of volcanic ash, and other...
Tipo: Text Palavras-chave: Planktonic foraminifera; N. pachyderma (sin.); Mg/Ca; Paleothermometry; Paleoceanography; Nordic Seas.
Ano: 2006 URL: https://archimer.ifremer.fr/doc/00234/34559/33319.pdf
Imagem não selecionada

Imprime registro no formato completo
Mg/Ca ratios of two Globigerinoides ruber (white) morphotypes: Implications for reconstructing past tropical/ subtropical surface water conditions ArchiMer
Steinke, S; Chiu, Hy; Yu, Ps; Shen, Cc; Lowemark, L; Mii, Hs; Chen, Mt.
Tests of the planktonic foraminifer Globigerinoides ruber ( white; d'Orbigny) have become a standard tool for reconstructing past oceanic environments. Paleoceanographers often utilize the Mg/Ca ratios of the foraminiferal tests for reconstructing low-latitude ocean glacial-interglacial changes in sea surface temperatures (SST). We report herein a comparison of Mg/Ca measurements on sample pairs (n = 20) of two G. ruber (white) morphotypes (G. ruber sensu stricto (s. s.) and G. ruber sensu lato ( s. l.)) from surface and downcore samples of the western Pacific and Indian Oceans. G. ruber s. s. refers to specimens with spherical chambers sitting symmetrically over previous sutures with a wide, high arched aperture, whereas G. ruber s. l. refers to a more...
Tipo: Text Palavras-chave: Planktonic foraminifera; Globigerinoides ruber (white); Morphotypes; Mg/Ca; Stable isotopes; Sea surface temperature.
Ano: 2005 URL: https://archimer.ifremer.fr/doc/00230/34081/32520.pdf
Imagem não selecionada

Imprime registro no formato completo
Orbital variations in planktonic foraminifera assemblages from the Ionian Sea during the Middle Pleistocene Transition ArchiMer
Incarbona, Alessandro; Dinares-turell, Jaume; Di Stefano, Enrico; Ippolito, Giuseppe; Pelosi, Nicola; Sprovieri, Rodolfo.
The Middle Pleistocene Transition (1.2-0.7 Ma) is the most recent re-organization of the global climate system which includes variations in the frequency and amplitude of glacial/interglacial cycles, increased ice sheet volume, sea surface temperature cooling and a significant drop in the CO2 atmospheric levels. Here we present high-resolution planktonic foraminifera data (mean sampling resolution of about 780 years) from core LC10 recovered in the Ionian Sea (eastern Mediterranean), between 1.2 and 0.9 Ma. Selected taxa, among them G. ruber, T. quinqueloba and G. bulloides, show significant periodicities that can be associated to orbital cycles, mainly precession and obliquity. The planktonic foraminifera based paleoclimatic curve exhibits a cooling...
Tipo: Text Palavras-chave: Middle Pleistocene Transition; Planktonic foraminifera; Ionian Sea; Orbital climate variability; Neogloboquadrina pachyderma sinistral coiling.
Ano: 2013 URL: https://archimer.ifremer.fr/doc/00181/29205/27581.pdf
Imagem não selecionada

Imprime registro no formato completo
Surface changes in the eastern Labrador Sea around the onset of the Little Ice Age ArchiMer
Moffa-sanchez, Paola; Hall, Ian R.; Barker, Stephen; Thornalley, David J. R.; Yashayaev, Igor.
Despite the relative climate stability of the present interglacial, it has been punctuated by several centennial-scale climatic oscillations; the latest of which are often colloquially referred to as the Medieval Climatic Anomaly (MCA) and the Little Ice Age (LIA). The most favored explanation for the cause of these anomalies is that they were triggered by variability in solar irradiance and/or volcanic activity and amplified by ocean-atmosphere-sea ice feedbacks. As such, changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC) are widely believed to have been involved in the amplification of such climatic oscillations. The Labrador Sea is a key area of deep water formation. The waters produced here contribute approximately one...
Tipo: Text Palavras-chave: Planktonic foraminifera; &#x03B4; 18O; Mg; Ca; Surface Labrador Sea; Last millennium.
Ano: 2014 URL: https://archimer.ifremer.fr/doc/00290/40167/39108.pdf
Imagem não selecionada

Imprime registro no formato completo
Rapid changes in meridional advection of Southern Ocean intermediate waters to the tropical Pacific during the last 30 kyr ArchiMer
Pena, L. D.; Goldstein, S. L.; Hemming, S. R.; Jones, K. M.; Calvo, E.; Pelejero, C.; Cacho, I..
The Southern Ocean is increasingly recognized as a key player in the general ocean thermohaline circulation and the global climate system during glacial interglacial transitions. In particular, the advection of Southern Ocean intermediate waters (SOIW), like Antarctic Intermediate Water and Sub-Antarctic Mode Water, to the Eastern Equatorial Pacific (EEP), through a so-called "oceanic tunnelling" mechanism, is an important means for rapid transfer of climatic signals (such as heat, fresh water, salt, and chemical species) from high-to-low latitudes. However, information on how intermediate water advection rates changed in the past, and particularly during deglaciations, is fragmentary. We present new results for Nd isotopes (epsilon(Nd)) in cleaned...
Tipo: Text Palavras-chave: Neodymium isotopes; Planktonic foraminifera; Intermediate water masses; Eastern Equatorial Pacific; Equatorial Undercurrent; Southern Ocean.
Ano: 2013 URL: https://archimer.ifremer.fr/doc/00264/37543/36928.pdf
Imagem não selecionada

Imprime registro no formato completo
Centennial-scale Holocene North Atlantic surface temperatures from Mg/Ca ratios in Globigerina bulloides ArchiMer
Farmer, Elizabeth J.; Chapman, Mark R.; Andrews, Julian E..
A high-resolution record of Mg/Ca ratios from the planktonic foraminifer Globigerina bulloides has been produced for IMAGES core MD99-2251 from the subpolar North Atlantic. The record extends from the Younger Dryas-Preboreal transition through the Holocene at similar to 70 year resolution, with a more detailed section at similar to 20 year resolution through the interval encompassing the major cooling episode 8200 years ago. Mg/Ca derived temperatures show significant variations through the Holocene, with surface temperatures ranging from similar to 8 to 13 degrees C. The onset of the Holocene is marked by an abrupt warming, with a further increase in early Holocene temperatures occurring prior to 9.5 ka. This is followed by a mid-Holocene period of cooler...
Tipo: Text Palavras-chave: Planktonic foraminifera; Mg/Ca; G. bulloides; North Atlantic; Holocene.
Ano: 2008 URL: https://archimer.ifremer.fr/doc/00236/34760/33396.pdf
Imagem não selecionada

Imprime registro no formato completo
Centennial-scale surface hydrology off Portugal during marine isotope stage 3: Insights from planktonic foraminiferal fauna variability ArchiMer
Vautravers, Maryline J.; Shackleton, Nicholas J..
The marine isotopic stage 3 (MIS3) at Ocean Drilling Program (ODP) Site 1060 (Gulf Stream) shows both sharp onset and end of interstadials, the existence of very short lived warm events during stadials, and points to differences in detail between the sea surface temperature (SST) record from the western North Atlantic and the atmospheric temperature record inferred from delta O-18 in Greenland ice. Investigating MIS3 and obtaining comparable data from other locations appears crucial. The eastern Atlantic provides well-documented records of climate changes. We have selected a core from off Portugal and use it to examine Dansgaard/Oeschger events (D/O) at centennial-scale resolution (139 years on average between two data points). We have obtained a faunal...
Tipo: Text Palavras-chave: SST; Planktonic foraminifera; Last glacial.
Ano: 2006 URL: https://archimer.ifremer.fr/doc/00234/34548/33352.pdf
Imagem não selecionada

Imprime registro no formato completo
Nomenclature for the Nameless: A Proposal for an Integrative Molecular Taxonomy of Cryptic Diversity Exemplified by Planktonic Foraminifera ArchiMer
Morard, Raphael; Escarguel, Gilles; Weiner, Agnes K. M.; Andre, Aurore; Douady, Christophe J.; Wade, Christopher M.; Darling, Kate F.; Ujiie, Yurika; Seears, Heidi A.; Quillevere, Frederic; De Garidel-thoron, Thibault; De Vargas, Colomban; Kucera, Michal.
Investigations of biodiversity, biogeography, and ecological processes rely on the identification of "species" as biologically significant, natural units of evolution. In this context, morphotaxonomy only provides an adequate level of resolution if reproductive isolation matches morphological divergence. In many groups of organisms, morphologically defined species often disguise considerable genetic diversity, which may be indicative of the existence of cryptic species. The diversity hidden by morphological species can be disentangled through genetic surveys, which also provide access to data on the ecological distribution of genetically circumscribed units. These units can be identified by unique DNA sequence motifs and allow studies of evolutionary and...
Tipo: Text Palavras-chave: Cryptic species; Genetic diversity; Planktonic foraminifera; Molecular nomenclature; MOTUs.
Ano: 2016 URL: https://archimer.ifremer.fr/doc/00383/49408/49900.pdf
Imagem não selecionada

Imprime registro no formato completo
Contribution of seasonal sub-Antarctic surface water variability to millennial-scale changes in atmospheric CO2 over the last deglaciation and Marine Isotope Stage 3 ArchiMer
Gottschalk, Julia; Skinner, Luke C.; Waelbroeck, Claire.
The Southern Ocean is thought to have played a key role in past atmospheric carbon dioxide (CO2,(atm)) changes. Three main factors are understood to control the Southern Ocean's influence on CO2,(atm), via their impact on surface ocean pCO(2) and therefore regional ocean-atmosphere CO2 fluxes: 1) the efficiency of air-sea gas exchange, which may be attenuated by seasonal- or annual sea-ice coverage or the development of a shallow pycnocline; 2) the supply of CO2-rich water masses from the subsurface and the deep ocean, which is associated with turbulent mixing and surface buoyancy- and/or wind forcing; and 3) biological carbon fixation, which depends on nutrient availability and is therefore influenced by dust deposition and/or upwelling. In order to...
Tipo: Text Palavras-chave: South Atlantic; Planktonic foraminifera; Stable oxygen and carbon isotopes; Atmospheric CO2; Last glacial period.
Ano: 2015 URL: https://archimer.ifremer.fr/doc/00297/40868/39920.pdf
Imagem não selecionada

Imprime registro no formato completo
Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ArchiMer
De Abreu, C; Abrantes, Ff; Shackleton, Nj; Tzedakis, Pc; Mcmanus, Jf; Oppo, Dw; Hall, Ma.
Similar orbital geometry and greenhouse gas concentrations during marine isotope stage 11 ( MIS 11) and the Holocene make stage 11 perhaps the best geological analogue period for the natural development of the present interglacial climate. Results of a detailed study of core MD01-2443 from the Iberian margin suggest that sea surface conditions during stage 11 were not significantly different from those observed during the elapsed portion of the Holocene. Peak interglacial conditions during stage 11 lasted nearly 18 kyr, indicating a Holocene unperturbed by human activity might last an additional 6-7 kyr. A comparison of sea surface temperatures ( SST) derived from planktonic foraminifera for all interglacial intervals of the last million years reveals that...
Tipo: Text Palavras-chave: Stage 11; Interglacials; Planktonic foraminifera; Stable isotopes; Western Iberian margin; Eastern North Atlantic.
Ano: 2005 URL: https://archimer.ifremer.fr/doc/00233/34407/32828.pdf
Imagem não selecionada

Imprime registro no formato completo
Mg/Ca-paleothermometry in the western Mediterranean Sea on planktonic foraminifer species Globigerina bulloides: Constraints and implications ArchiMer
Boussetta, Soumaya; Kallel, Nejib; Bassinot, Franck; Labeyrie, Laurent; Duplessy, Jean-claude; Caillon, Nicolas; Dewilde, Fabien; Rebaubier, Helene.
We generated a high-resolution SSTMg/Ca record for the surface-dwelling planktonic foraminifera Globigerina bulloides from the core MD99-2346 collected in the Gulf of Lion, and compared it to that obtained using modern analogue techniques applied to fossil foraminiferal assemblages (SSTMAT). The two temperature records display similar patterns during the last 28,000 years but the SSTMg/Ca estimates are several degrees warmer (similar to+4 degrees C) than SSTMAT. The temperature shift between SSTMg/Ca and SSTMAT remained relatively constant over time. This seems to exclude a bias on the Mg/Ca record associated with salinity or secondary Mg-rich calcite encrustation on the foraminiferal tests during early diagenesis. Therefore, anomalously high Mg/Ca...
Tipo: Text Palavras-chave: Mediterranean; Mg/Ca; Planktonic foraminifera; Sea surface Temperature; Salinity; Diagenesis; Vital effect.
Ano: 2012 URL: https://archimer.ifremer.fr/doc/00139/25047/23181.pdf
Imagem não selecionada

Imprime registro no formato completo
RECENT PLANKTONIC FORAMINIFERA FROM DEEP-SEA SEDIMENTS FROM THE EASTERN EQUATORIAL PACIFIC: PROXIES OF THE EQUATORIAL FRONT IN THE LATE QUATERNARY Boletín de Investigaciones
Martinez,Jose Ignacio; Bedoya,Geovanny.
Planktonic foraminifera recovered from 25 deep-sea sediment samples (core-tops) from the eastern Equatorial Pacific were analyzed for their geographic distribution and possible environmental controls. Samples collected deeper than the carbonate lysocline (~2800 m) show significant signs of dissolution, - when compared to sediment-trap samples -, resulting in the increase of the solution-resistant species Neogloboquadrina dutertrei, Neogloboquadrina pachyderma and Globorotalia cultrata and the reduction of the solution-susceptible species Globigerinita glutinata, Globigerinoides ruber and Globigerinoides sacculifer. Three bioprovinces were recognized by cluster analysis: (1) bioprovince I that occurs on the Cocos Ridge where G. cultrata and N. pachyderma...
Tipo: Info:eu-repo/semantics/article Palavras-chave: Planktonic foraminifera; Eastern Equatorial Pacific; Panama Basin; Deep-sea sediments; Micropaleontology.
Ano: 2001 URL: http://www.scielo.org.co/scielo.php?script=sci_arttext&pid=S0122-97612001000100008
Registros recuperados: 12
Primeira ... 1 ... Última
 

Empresa Brasileira de Pesquisa Agropecuária - Embrapa
Todos os direitos reservados, conforme Lei n° 9.610
Política de Privacidade
Área restrita

Embrapa
Parque Estação Biológica - PqEB s/n°
Brasília, DF - Brasil - CEP 70770-901
Fone: (61) 3448-4433 - Fax: (61) 3448-4890 / 3448-4891 SAC: https://www.embrapa.br/fale-conosco

Valid HTML 4.01 Transitional