KEILA CRISTINA PEREIRA ANICETO

@ufam.edu.br

Post-graduate Program in Geosciences.
Institute of Exact Sciences - Federal University of Amazonas

KEILA CRISTINA PEREIRA ANICETO


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https://researchid.co/keilaniceto

EDUCATION

Degree in Chemistry from the Federal University of Amazonas (2004), a master's degree in Geosciences (Environmental Geology-Geochemistry) from the Federal University of Amazonas (2008) and doctorate in Geosciences (Environmental Geochemistry) from the Federal Fluminense University (2014) with internship in France. Post-doctoral student and collaborating professor of the Post-Graduate Program in Geosciences at the Federal University of Amazonas (2014- 2019).
10

Scopus Publications

166

Scholar Citations

7

Scholar h-index

7

Scholar i10-index

Scopus Publications

  • Hydrosedimentary Dynamics in the Confluence of the Beni and Mamoré Rivers
    Ednaldo Bras Severo, Rogerio Ribeiro Marinho, Jean-Michel Martinez, Naziano Pantoja Filizola, Henrique Llacer Roig, et al.
    Revista Brasileira De Geomorfologia, 2025
    This study analyzed hydrosedimentary dynamics at the confluence of the Beni and Mamoré rivers, the two main source rivers of the Madeira River, the largest tributary of the Amazon River. Thirteen field campaigns were conducted between March 2021 and April 2022 at four cross-sections, complemented by historical data from the HYBAM Observatory. The results showed clear contrasts between the tributary rivers: mean suspended sediment concentrations (SSC) were 639 mg.L⁻¹ in the Beni and 218 mg.L⁻¹ in the Mamoré, with specific yields of 2.07 and 0.34 ton.km⁻².yr⁻¹, respectively. The Madeira River exhibited intermediate SSC values (357–371 mg.L⁻¹). During high-water conditions, vertical SSC stratification was more pronounced in the Mamoré and Madeira rivers. The sediment budget indicated a 15% deficit downstream of the confluence, corresponding to the retention of approximately 40 million tons over a 220 km reach. Downstream of this confluence lies the Jirau Hydroelectric Power Plant reservoir, whose dam may influence the study reach. Together, the Beni and Mamoré rivers contribute about 291 million tons of suspended sediment annually to the Madeira River, confirming their strategic role in the Amazon sediment budget and providing a basis for sustainable management of this watershed’s resources.
  • Paleoenvironmental changes in a lower Rio Negro floodplain lake (Anavilhanas Archipelago, Brazil) during the past 4550 years
    Renato Campello Cordeiro, Caroline Rocha Maia, Luciane Silva Moreira, Bruno Turcq, Patricia Moreira-Turcq, et al.
    Holocene, 2025
    This study investigates Holocene climate variability and its influence on organic carbon accumulation patterns in the Anavilhanas Archipelago, Rio Negro, Brazilian Amazon. We analyzed a 404 cm sediment core from a floodplain lake to reconstruct paleoenvironmental changes and carbon storage dynamics over the last 4550 cal yr BP. The Middle to Late-Holocene transition (4550–4270 cal yr BP) was characterized by significant hydrological changes. Low chlorophyll derivative values during this period reflect elevated water levels and variable discharge regimes, consistent with a braided channel system exhibiting high hydrodynamic energy and unstable fluvial architecture. These conditions prevented the establishment of stable lentic environments, resulting in highly variable deposition of organic compounds. Between 4270 and 3865 cal yr BP, sedimentary and organic proxies showed pronounced variability, indicating shifts in precipitation patterns and fluvial geomorphology. Organic matter exhibited high C/N ratios and δ 13 C values, indicating a predominantly allochthonous origin, likely from vascular plant material with C4 signatures. Carbon accumulation rates peaked at 196 g m −2 yr −1 around 4050 cal yr BP. The period 3865–3200 cal yr BP marked the establishment of arboreal vegetation alongside increased lacustrine productivity with enhanced algal contributions, signaling a transition to more humid conditions. Maximum primary productivity occurred between 3200 and 2100 cal yr BP, coinciding with the development of the current levee-lake morphology, with carbon accumulation averaging 18 g m −2 yr −1 . From 2100 to 760 cal yr BP, sediment records indicate an intensified dryness compared to preceding and subsequent periods, with reduced carbon accumulation rate of only ~15 g m −2 yr −1 . The most recent 760 years, particularly the last two centuries, show significantly increased carbon fluxes (38.1 g m −2 yr −1 ) associated with wetter conditions. Our results demonstrate that Late-Holocene hydroclimatic variations, including increased humidity and seasonal variability, exerted fundamental control on sedimentary dynamics, lacustrine productivity, and carbon storage in the Rio Negro floodplain system.
  • Sentinel-2 MSI image time series reveal hydrological and geomorphological control of the sedimentation processes in an Amazonian hydropower dam
    Diego R. Alves e Santos, Jean-Michel Martinez, Diogo Olivetti, André Zumak, David Guimarães, et al.
    International Journal of Applied Earth Observation and Geoinformation, 2024
  • Development of lacustrine primary productivity in the Amazon Basin during the Holocene
    Juliano HF Soares, Luciane S Moreira, Bruno Turcq, Patricia Moreira-Turcq, Abdel Sifeddine, et al.
    Holocene, 2022
    The Amazon Basin is one of the most productive regions in the world and an important carbon sink. However, lake productivity has varied throughout the Holocene, as preserved in lacustrine sedimentary records. Concentrations of chlorophyll pigmented derivatives that are mainly derived from phytoplankton and macrophyte populations can be used to infer lake production levels. Here we use the chlorophyll derivatives concentrations analyzed by spectrophotometer in sediment cores from nine lakes distributed throughout the Brazilian Amazon Basin to document the continental-scale changes in lake production during the Holocene. Chlorophyll derivatives have varied with changes in precipitation rate throughout the last 10,000 years, similar to other climate records in tropical South America, including Ti concentration from the Cariaco Basin, δ13C from Lake Titicaca, and refractory black carbon in Nevado Illimani. Increasing precipitation is responsible for increasing the nutrient supply into the lake, which stimulates primary production. Our analysis was compared to climate-related parameters, suggesting an increasing trend of lake production rates during the wetter Late and Early Holocene, while lower production rates characterized the dry phase of the Middle Holocene. Therefore, the chlorophyll derivatives concentrations generally follow precipitation changes in the Amazon Basin during the Holocene.
  • Dust arriving in the Amazon basin over the past 7,500 years came from diverse sources
    Juliana Nogueira, Heitor Evangelista, Claudio de Morisson Valeriano, Abdelfettah Sifeddine, Carla Neto, et al.
    Communications Earth and Environment, 2021
    A large amount of dust from the Sahara reaches the Amazon Basin, as observed with satellite imagery. This dust is thought to carry micronutrients that could help fertilize the rainforest. However, considering different atmospheric transport conditions, different aridity levels in South America and Africa and active volcanism, it is not clear if the same pathways for dust have occurred throughout the Holocene. Here we present analyses of Sr-Nd isotopic ratios of a lacustrine sediment core from remote Lake Pata in the Amazon region that encompasses the past 7,500 years before present, and compare these ratios to dust signatures from a variety of sources. We find that dust reaching the western Amazon region during the study period had diverse origins, including the Andean region and northern and southern Africa. We suggest that the Sahara Desert was not the dominant source of dust throughout the vast Amazon basin over the past 7,500 years.
  • Climate and hydrologic controls on late Holocene sediment supply to an Amazon floodplain lake
    Luciane Silva Moreira, Patricia Moreira-Turcq, Renato Campello Cordeiro, Bruno Turcq, Keila Cristina Aniceto, et al.
    Journal of Paleolimnology, 2020
    Organic and inorganic geochemical analyses on sediments from Preto Lake, a central Amazon basin floodplain water body, were used to document hydrological changes of the Solimões River during the late Holocene. Between 3600 and 400 cal yr BP, Preto Lake received smectite-rich sediment from the Solimões River, with high concentrations of Al (~ 53 × 103 ppm) and Si (~ 210 × 103 ppm). The high detrital input suggests there was a direct connection between Preto Lake and the main river channel. High river inflow maintained lake stage and was responsible for the contribution to sediments of phytoplankton-derived organic matter. Low sediment organic carbon concentrations characterized this period (mean ~ 3.8 wt%), probably because of dilution by river-borne lithogenic matter. Although the river inputs remained high, abrupt increases in TOC content around 1800 and 1200 cal yr BP suggest brief increases in fluvial nutrient supply to Preto Lake. During the last 400 cal yr, substantial declines in smectite (mean 40%), Al (~ 29 × 103 ppm) and Si (138 × 103 ppm) suggest the establishment of a semi-isolated lake, with reduced river inflow. A large proportion of C3-plant-derived organic matter, supplied by runoff from the kaolinite-rich watershed, was observed during this period, and was accompanied by high autochthonous primary production, driven by development of an aquatic macrophyte community. This change in sediment organic matter source accounted for the greater TOC content (~ 20%) of sediments deposited during this period. Although Holocene climate change was an important control on fluvial sediment supply to upper and lower Amazon Basin floodplain lakes, sedimentation processes in Preto Lake can also be linked to changes in the river’s course. The transition to a semi-isolated lake could have been a consequence of lateral and vertical sediment accretion, which formed a natural levee that blocked fluvial input to Preto Lake.
  • Hydrological characterization of anavilhanas archipelago lake systems by remote sensing
    V. A. Silva, K. Aniceto, R. R. Marinho, N. Filizola
    Geociencias, 2020
    This study characterized the Anavilhanas Archipelago lake systems and evaluated the spatial variation of the water surface under conditions close to the interannual fluviometric averages for each period, using Landsat 08 images and Rio Negro fluviometric data. The seasonal variation observed for the entire archipelago was around 10%. For lake systems and “dead water” areas it was 17%. For 447 lakes identified, 46% are connected to the archipelago canals during the low water period and 54% are isolated during this period. Three domains were pointed to the Archipelago. In domain A (upstream) the river is relatively narrow and the islands and lakes are smaller. In domain B (center) the river is relatively wider and the islands and lakes are large. In domain C (downstream) the river is similar in width to domain A and the narrow, elongated and winding islands with elongated and open lakes. The C domain presented less seasonal variation and a larger number of connected lakes, which may be associated with the geomorphological characteristics and hydraulic conditions given by the influence of the Solimoes River hydraulic bus.
  • Dynamics of floodplain lakes in the Upper Amazon Basin during the late Holocene
    Isabel Quintana-Cobo, Patricia Moreira-Turcq, Renato C. Cordeiro, Keila Aniceto, Alain Crave, et al.
    Comptes Rendus Geoscience, 2018
    To better understand the impact of channel migration processes and climate change on the depositional dynamics of floodplain lakes of the upper Amazon Basin during the late Holocene, we collected three sediment cores from floodplain lakes of the Ucayali River and one from the Maranon River. The cores were dated with 14C, radiographed and described. Bulk density, grain size analysis and total organic carbon (TOC) were determined. The results show that sedimentation in Ucayali floodplain lakes was marked by variations during the late Holocene, with periods of intense hydrodynamic energy and abrupt accumulations, a gap in the record between about 2870 and 690 cal yr BP, and periods of more lacustrine conditions. These changes in sedimentation were associated with variations in the river's influence related to changes in its meandering course (2870 cal yr BP) and a period of severe flooding between 3550 and 3000 cal yr BP. Lake Lagarto on the Maranon River floodplain exhibits a different sedimentary environment of low hydrodynamics with palm trees and macrophytes. Apparently, the lake has not experienced intense migration processes during the last 600 cal yr BP (base of the core). Nevertheless, the river sediment flux to the lake was important from 600 to 500 cal yr BP, although it decreased thereafter until the present. This decrease in the mineral accumulation rate indicates a decrease in river discharge since 500 cal yr BP, which coincides with precipitation records from the central Andes. In the upper part of the three Ucayali floodplain cores, a 30- to 250-cm-thick layer of reworked sediments has been deposited since 1950 AD (post-bomb). In Lake Carmen, this layer is associated with invasion of the lake by the levee of a migrating meander of the Ucayali. In Lakes Hubos and La Moringa, however, the river is still far away and the deposition must be interpreted as the result of extreme flooding. The beginning of the Ucayali meander migration is dated back to 2000 AD, suggesting that these extreme floods could be very recent and linked to hydrologic extremes registered instrumentally in the Amazon Basin.
  • Holocene paleohydrology of Quistococha Lake (Peru) in the upper Amazon Basin: Influence on carbon accumulation
    Keila Aniceto, Patricia Moreira-Turcq, Renato C. Cordeiro, Pascal Fraizy, Isabel Quintana, et al.
    Palaeogeography Palaeoclimatology Palaeoecology, 2014
    In order to study the impact of hydrological changes of the Amazon River on sedimentation process and organic matter (OM) accumulation, in an Amazonian floodplain lake during the Holocene, three sediment cores were collected from Quistococha Lake, Peru. The cores were dated with 14C accelerator mass spectrometry (AMS), radiographed, and described. Bulk density, granulometry, loss on ignition (LOI), total organic carbon (TOC) and total nitrogen (TN) contents were measured, and stable isotopic composition of TOC (δ13C) and TN (δ15N) and carbon accumulation rates were determined. Two distinctive sedimentary depositional phases were identified based on the lithology, granulometry and the geochemical characteristics of sedimentary OM. Between about 6100 and 4900 cal years BP, the lake was under strong influence of the Amazon River. The river induced highest sedimentation rates (mean 0.5 cm yr− 1), a predominant deposition of relatively coarse particles (coarse silt), low LOI (1%), low contents of organic carbon (0.5%), low C/N ratios (~ 10), relatively low δ13C values (− 26.0‰), very laminated sediments and high carbon accumulation rates between 14 and 29 g C m− 2 yr− 1. A gap in the record between about 4900 and 2600 cal years BP corresponds to a sedimentation hiatus during the dry mid Holocene. This gap is probably due to an avulsion of the main stem that induced significant changes in the lacustrine sedimentation. After 2600 cal years BP, sedimentation resumed but now the lake was isolated far from the Amazon influence. The resumption of sedimentation corresponds to wetter conditions during the late Holocene and an increase in water levels. The lake was now characterized by very low sedimentation rates (0.02 cm yr− 1), fine organic-rich sediments with high LOI (between 20 and 80%), TOC (between 10 and 40% of TOC), high C/N ratio (20), and lower δ13C and δ15N indicating a predominant deposition of C3-plant derived OM. Carbon accumulation in this sedimentary depositional phase was about 8 g C m− 2 yr− 1. These results, combined with those of studies from other isolated lakes (Cordeiro et al., 1997, 2008; Turcq et al., 2002) and from other floodplain lakes (Moreira et al., 2012; Moreira et al., 2013), point out that floodplain lakes with strong influences from the Amazon River act as important carbon sinks in the Amazon Basin despite their low carbon concentrations.
  • Urban soils formed by the accumulation of waste in Manaus, Amazonas, Brazil
    Keila Cristina Pereira Aniceto, Adriana Maria Coimbra Horbe
    Acta Amazonica, 2012
    Este estudo apresenta dados sobre a mineralogia e a química de dois solos urbanos em Manaus (Horto Minicipal e Novo Israel) formados a partir da disposição e degradação de resíduo urbano em condições tropicais úmidas. Foi determinada a concentração de Pb, Cu, Ni, Zn, Mn, Fe, Cd e Cr, investigado o grau de contaminação desses elementos no solo e o potencial deles comprometerem a qualidade da água subterrânea. Foi medido o fracionamento geoquímico por lixiviação sequencial dos elementos, além de determinado o pH, teor de matéria orgânica e caracterizados os grupos funcionais dos ácidos húmicos e fúlvicos. Comparativamente esses solos urbanos refletem a composição mineralógica dos solos naturais da região embora a caulinita tenha menor grau de ordenamento cristalino. Contudo, o pH e o conteúdo de matéria orgânica são bem mais elevados. Em termos absolutos ambos os solos têm aproximadamente a mesma sequência de concentração dos elementos: no Horto Municipal Fe>Zn>Mn>Cu>Pb>Cr>Ni>Cd e em Novo Israel Fe>Zn>Cu>Mn>Pb>Cr>Ni>Cd. As maiores acumulações foram nas frações hidróxido de Fe amorfo e óxi-hidróxidos de Fe seguidas da matéria orgânica. Comparativamente, essas frações tiveram maior enriquecimento no Horto Municipal, provavelmente em consequência dos efeitos de envelhecimento dos resíduos, enquanto as mais biodisponíveis e a residual se acumularam mais em Novo Israel. Esse acúmulo nas fases mais móveis em Novo Israel é a causa da contaminação da água subterrânea e indica que o mesmo deve ocorrer no Horto Municipal.

RECENT SCHOLAR PUBLICATIONS

  • Hydrosedimentary Dynamics in the Confluence of the Beni and Mamoré Rivers
    EB Severo, RR Marinho, JM Martinez, NP Filizola, HL Roig, K Aniceto, ...
    Revista Brasileira de Geomorfologia 27 (1) , 2026
    2026
  • Rare Earth Elements as Emerging Contaminants in Negro River Sediments During an Extreme Drought Event (Central Amazon)
    GS Caldeira, PC Evangelistaa, MM Lage, FB Egreja Filho, ...
    Environmental Pollution, 127707 , 2026
    2026
    Citations: 1
  • Paleoenvironmental changes in a lower Rio Negro floodplain lake (Anavilhanas Archipelago, Brazil) during the past 4550 years
    RC Cordeiro, CR Maia, LS Moreira, B Turcq, P Moreira-Turcq, ...
    The Holocene 35 (9), 907-925 , 2025
    2025
    Citations: 3
  • Desenvolvendo um modelo de sensoriamento remoto para estimativa de sólidos em suspensão em águas turvas complexas: o caso do Rio Madeira
    D Olivetti, JM Martinez, D França, O Santos, A Zumak, K Aniceto, ...
    XVI ENES, Curitiba , 2024
    2024
    Citations: 1
  • Sentinel-2 MSI image time series reveal hydrological and geomorphological control of the sedimentation processes in an Amazonian hydropower dam
    DRA e Santos, JM Martinez, D Olivetti, A Zumak, D Guimarães, K Aniceto, ...
    International Journal of Applied Earth Observation and Geoinformation 128 … , 2024
    2024
    Citations: 12
  • Evolucion historica de la dinamica fluvial del Rio Ucayali (Peru)
    I Quintana-Cobo, K Aniceto, P Moreira-Turcq, RC Cordeiro, A Crave, ...
    Revista Geonorte 15 (52), 219-242 , 2024
    2024
    Citations: 1
  • The Si and Li isotope signatures of chemical weathering in tectonically quiescent, tropical areas
    D Guinoiseau, J Bouchez, JS Moquet, D Calmels, JM Martinez, K Aniceto, ...
    Thirty-third Annual Goldschmidt Conference, 19156 , 2023
    2023
  • Paleoenvironmental changes in a lower rio Negro Amazon floodplain lake (Anavilhanas archipelago) over the last 4500 Years
    RC Cordeiro, CR Maia, LS Moreira, B Turcq, P Moreira-Turcq, ...
    Available at SSRN 4605495 , 2023
    2023
    Citations: 1
  • Development of lacustrine primary productivity in the Amazon Basin during the Holocene
    JHF Soares, LS Moreira, B Turcq, P Moreira-Turcq, A Sifeddine, ...
    The Holocene 32 (7), 639-649 , 2022
    2022
    Citations: 3
  • Dust arriving in the Amazon basin over the past 7,500 years came from diverse sources
    J Nogueira, H Evangelista, CM Valeriano, A Sifeddine, C Neto, G Vaz, ...
    Communications Earth & Environment 2 (1), 5 , 2021
    2021
    Citations: 32
  • Climate and hydrologic controls on late Holocene sediment supply to an Amazon floodplain lake
    LS Moreira, P Moreira-Turcq, RC Cordeiro, B Turcq, KC Aniceto, ...
    Journal of Paleolimnology 64 (4), 389-403 , 2020
    2020
    Citations: 10
  • CARACTERIZAÇÃO HIDROLÓGICA DOS SISTEMAS LACUSTRES DO ARQUIPÉLAGO DE ANAVILHANAS COM BASE EM SENSORIAMENTO REMOTO: Hydrological characterization of Anavilhanas Archipelago Lake …
    VC Silva, KP Aniceto, RR Marinho, NP Filizola
    Geosciences= Geociências 39 (2), 411-424 , 2020
    2020
    Citations: 6
  • An Integrated Approach to Tracking Paleohydrological Changes Along the Amazon Basin
    LS Moreira, PF Moreira-Turcq, K Aniceto, RC Cordeiro, B Turcq
    AGU Fall Meeting Abstracts 2019, PP51F-1436 , 2019
    2019
  • Caracterização hidrogeoquímica e qualidade da água de poços tubulares em aldeias indígenas na região da Amazônia Central
    CAS Clebsch
    Dissertação, Manaus, Amazonas, Brasil: UNIVERSIDADE FEDERAL DO AMAZONAS , 2018
    2018
    Citations: 2
  • Dynamics of floodplain lakes in the Upper Amazon Basin during the late Holocene
    I Quintana-Cobo, P Moreira-Turcq, RC Cordeiro, K Aniceto, A Crave, ...
    Comptes Rendus Geoscience 350 (1-2), 55-64 , 2018
    2018
    Citations: 18
  • River mixing in the Amazon as a driver of concentration-discharge relationships
    JS Moquet, J Bouchez, J Carlo Espinoza, JM Martinez, JL Guyot, ...
    EGU General Assembly Conference Abstracts, 19644 , 2017
    2017
  • Holocene paleohydrology of Quistococha Lake (Peru) in the upper Amazon Basin: Influence on carbon accumulation
    K Aniceto, P Moreira-Turcq, RC Cordeiro, P Fraizy, I Quintana, B Turcq
    Palaeogeography, Palaeoclimatology, Palaeoecology 415, 165-174 , 2014
    2014
    Citations: 28
  • The complex and dynamic process of sedimentation in Amazonia floodplain lakes: the case of the Quistococha Lake, Peru
    K Aniceto, P Moreira-Turcq, K Macario
    Radiocarbon in the environment , 2014
    2014
  • Paleohidrologia do rio Amazonas influenciando a sedimentação do Lago Quistococha, Peru
    K Aniceto, P Moreira-Turcq, RC Cordeiro, P Fraizy, I Quintana, B Turcq
    International Conference on the Status and Future of the World’s Large Rivers , 2014
    2014
  • Impacto del cambio climático en la sedimentación y en la acumulación de carbono en los lagos de la Amazonía peruana
    P Moreira-Turcq, K Aniceto, I Quintana-Cobo, E Chavarri, P Fraizy, ...
    El Perú frente al Cambio Climático. Resultados de investigaciones franco … , 2014
    2014
    Citations: 2

MOST CITED SCHOLAR PUBLICATIONS

  • Dust arriving in the Amazon basin over the past 7,500 years came from diverse sources
    J Nogueira, H Evangelista, CM Valeriano, A Sifeddine, C Neto, G Vaz, ...
    Communications Earth & Environment 2 (1), 5 , 2021
    2021
    Citations: 32
  • Holocene paleohydrology of Quistococha Lake (Peru) in the upper Amazon Basin: Influence on carbon accumulation
    K Aniceto, P Moreira-Turcq, RC Cordeiro, P Fraizy, I Quintana, B Turcq
    Palaeogeography, Palaeoclimatology, Palaeoecology 415, 165-174 , 2014
    2014
    Citations: 28
  • Solos urbanos formados pelo acúmulo de resíduos em Manaus, Amazonas, Brasil
    KCP Aniceto, AMC Horbe
    Acta Amazonica 42 (1), 135-148 , 2012
    2012
    Citations: 26
  • Dynamics of floodplain lakes in the Upper Amazon Basin during the late Holocene
    I Quintana-Cobo, P Moreira-Turcq, RC Cordeiro, K Aniceto, A Crave, ...
    Comptes Rendus Geoscience 350 (1-2), 55-64 , 2018
    2018
    Citations: 18
  • Hydrological changes in West Amazonia over the past 6 Ka inferred from geochemical proxies in the sediment record of a floodplain lake
    K Aniceto, P Moreira-Turcq, RC Cordeiro, I Quintana, P Fraizy, B Turcq
    Procedia Earth and Planetary Science 10, 287-291 , 2014
    2014
    Citations: 16
  • Sentinel-2 MSI image time series reveal hydrological and geomorphological control of the sedimentation processes in an Amazonian hydropower dam
    DRA e Santos, JM Martinez, D Olivetti, A Zumak, D Guimarães, K Aniceto, ...
    International Journal of Applied Earth Observation and Geoinformation 128 … , 2024
    2024
    Citations: 12
  • Climate and hydrologic controls on late Holocene sediment supply to an Amazon floodplain lake
    LS Moreira, P Moreira-Turcq, RC Cordeiro, B Turcq, KC Aniceto, ...
    Journal of Paleolimnology 64 (4), 389-403 , 2020
    2020
    Citations: 10
  • CARACTERIZAÇÃO HIDROLÓGICA DOS SISTEMAS LACUSTRES DO ARQUIPÉLAGO DE ANAVILHANAS COM BASE EM SENSORIAMENTO REMOTO: Hydrological characterization of Anavilhanas Archipelago Lake …
    VC Silva, KP Aniceto, RR Marinho, NP Filizola
    Geosciences= Geociências 39 (2), 411-424 , 2020
    2020
    Citations: 6
  • Paleoenvironmental changes in a lower Rio Negro floodplain lake (Anavilhanas Archipelago, Brazil) during the past 4550 years
    RC Cordeiro, CR Maia, LS Moreira, B Turcq, P Moreira-Turcq, ...
    The Holocene 35 (9), 907-925 , 2025
    2025
    Citations: 3
  • Development of lacustrine primary productivity in the Amazon Basin during the Holocene
    JHF Soares, LS Moreira, B Turcq, P Moreira-Turcq, A Sifeddine, ...
    The Holocene 32 (7), 639-649 , 2022
    2022
    Citations: 3
  • Química e mineralogia da fração sólida do material acumulado nos antigos lixões de Novo Israel e Horto Municipal na área urbana de Manaus
    KCP Aniceto
    Universidade Federal do Amazonas , 2008
    2008
    Citations: 3
  • Caracterização hidrogeoquímica e qualidade da água de poços tubulares em aldeias indígenas na região da Amazônia Central
    CAS Clebsch
    Dissertação, Manaus, Amazonas, Brasil: UNIVERSIDADE FEDERAL DO AMAZONAS , 2018
    2018
    Citations: 2
  • Impacto del cambio climático en la sedimentación y en la acumulación de carbono en los lagos de la Amazonía peruana
    P Moreira-Turcq, K Aniceto, I Quintana-Cobo, E Chavarri, P Fraizy, ...
    El Perú frente al Cambio Climático. Resultados de investigaciones franco … , 2014
    2014
    Citations: 2
  • Rare Earth Elements as Emerging Contaminants in Negro River Sediments During an Extreme Drought Event (Central Amazon)
    GS Caldeira, PC Evangelistaa, MM Lage, FB Egreja Filho, ...
    Environmental Pollution, 127707 , 2026
    2026
    Citations: 1
  • Desenvolvendo um modelo de sensoriamento remoto para estimativa de sólidos em suspensão em águas turvas complexas: o caso do Rio Madeira
    D Olivetti, JM Martinez, D França, O Santos, A Zumak, K Aniceto, ...
    XVI ENES, Curitiba , 2024
    2024
    Citations: 1
  • Evolucion historica de la dinamica fluvial del Rio Ucayali (Peru)
    I Quintana-Cobo, K Aniceto, P Moreira-Turcq, RC Cordeiro, A Crave, ...
    Revista Geonorte 15 (52), 219-242 , 2024
    2024
    Citations: 1
  • Paleoenvironmental changes in a lower rio Negro Amazon floodplain lake (Anavilhanas archipelago) over the last 4500 Years
    RC Cordeiro, CR Maia, LS Moreira, B Turcq, P Moreira-Turcq, ...
    Available at SSRN 4605495 , 2023
    2023
    Citations: 1
  • Urban soils formed by the accumulation of waste in Manaus, Amazonas, Brazil
    KCP Aniceto, AMC Horbe
    Acta Amazonica 42, 135-148 , 2012
    2012
    Citations: 1
  • Hydrosedimentary Dynamics in the Confluence of the Beni and Mamoré Rivers
    EB Severo, RR Marinho, JM Martinez, NP Filizola, HL Roig, K Aniceto, ...
    Revista Brasileira de Geomorfologia 27 (1) , 2026
    2026
  • The Si and Li isotope signatures of chemical weathering in tectonically quiescent, tropical areas
    D Guinoiseau, J Bouchez, JS Moquet, D Calmels, JM Martinez, K Aniceto, ...
    Thirty-third Annual Goldschmidt Conference, 19156 , 2023
    2023