Marta Estrada

ORCID: 0000-0001-5769-9498
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About
Contact & Profiles
Research Areas
  • Marine and coastal ecosystems
  • Marine Biology and Ecology Research
  • Microbial Community Ecology and Physiology
  • Aquatic Ecosystems and Phytoplankton Dynamics
  • Marine Toxins and Detection Methods
  • Oceanographic and Atmospheric Processes
  • Ocean Acidification Effects and Responses
  • Marine and fisheries research
  • Marine Bivalve and Aquaculture Studies
  • Isotope Analysis in Ecology
  • Diatoms and Algae Research
  • Historical and socio-economic studies of Spain and related regions
  • Protist diversity and phylogeny
  • Algal biology and biofuel production
  • Marine and environmental studies
  • Marine and coastal plant biology
  • Coastal and Marine Management
  • Geological and Geophysical Studies Worldwide
  • Archaeological and Historical Studies
  • Mediterranean and Iberian flora and fauna
  • Aquatic Invertebrate Ecology and Behavior
  • Marine Ecology and Invasive Species
  • Methane Hydrates and Related Phenomena
  • Arctic and Antarctic ice dynamics
  • Coral and Marine Ecosystems Studies

Institut Català de Ciències del Clima
2013-2023

Institut de Ciències del Mar
2014-2023

Consejo Superior de Investigaciones Científicas
2010-2022

Institut d'Estudis Catalans
2021

Instituto Español de Oceanografía
2001-2019

King Abdullah University of Science and Technology
2015

Council of Science Editors
2011

Centro Mediterráneo de Investigaciones Marinas y Ambientale
2002-2008

Pemex (Mexico)
2007

National Research Council
2003-2006

Despite the high abundance of Archaea in global ocean, their metabolism and biogeochemical roles remain largely unresolved. We investigated population dynamics metabolic activity Thaumarchaeota polar environments, where these microorganisms are particularly abundant exhibit seasonal growth. were more deep Arctic Antarctic waters grew throughout winter at surface deeper halocline waters. However, situ single-cell measurements revealed a low this group uptake both leucine bicarbonate (<5%...

10.1073/pnas.1201914109 article EN Proceedings of the National Academy of Sciences 2012-10-01

Abstract The role of the ocean as a sink for CO 2 is partially dependent on downward transport phytoplankton cells packaged within fast-sinking particles. However, whether such mechanisms deliver fresh organic carbon down to deep bathypelagic sea and this mechanism prevalent across requires confirmation. Here we report ubiquitous presence healthy photosynthetic cells, dominated by diatoms, 4,000 m in dark ocean. Decay experiments with surface suggested that large proportion (18%) observed,...

10.1038/ncomms8608 article EN cc-by Nature Communications 2015-07-09

Primary production by marine phytoplankton is one of the largest fluxes carbon on our planet. In past few decades, considerable progress has been made in estimating global primary at high spatial and temporal scales combining situ measurements with remote-sensing observations biomass. One major challenges this approach lies assignment appropriate model parameters that define photosynthetic response to light field. present study, a database photosynthesis versus irradiance (P-I) 20-year...

10.3390/rs12050826 article EN cc-by Remote Sensing 2020-03-03

A well-developed deep chlorophyll maximum (DCM) is a prominent feature of the Northwestern Mediterranean during large part year.Data from 7 oceanographic surveys carried out across Catalano-Balearic Sea, between 1982 and 1987, have been used to analyze shortterm (within cruises) seasonal+interannual (between variation several parameters (such as surface DCM concentration, integrated chlorophyll, DCM, nitracline nitrite depths).S~gnificant positlve correlations (p < 0.01) were found depths...

10.3354/meps092289 article EN Marine Ecology Progress Series 1993-01-01

10.1016/0169-5347(96)81132-3 article IT Trends in Ecology & Evolution 1996-07-01

Abstract Global patterns of planktonic diversity are mainly determined by the dispersal propagules with ocean currents. However, role that abundance and body size play in determining spatial remains unclear. Here we analyse community structure - β-diversity for several nektonic organisms from prokaryotes to small mesopelagic fishes collected during Malaspina 2010 Expedition. was compared surface transit times derived a global circulation model, revealing significant negative relationship is...

10.1038/s41467-017-02535-8 article EN cc-by Nature Communications 2018-01-04

Climate warming affects the development and distribution of sea ice, but at present evidence polar ecosystem feedbacks on climate through changes in atmosphere is sparse. By means synergistic atmospheric oceanic measurements Southern Ocean near Antarctica, we that microbiota ice ice-influenced ocean are a previously unknown significant source organic nitrogen, including low molecular weight alkyl-amines. Given keystone role nitrogen compounds aerosol formation, growth neutralization, our...

10.1038/s41598-017-06188-x article EN cc-by Scientific Reports 2017-07-14

We examine the large-scale distribution patterns of nano- and microphytoplankton collected from 145 oceanic stations, at 3 m depth, 20% light level depth subsurface chlorophyll maximum, during Malaspina-2010 Expedition (December 2010-July 2011), which covered 15 biogeographical provinces across Atlantic, Indian Pacific oceans, between 35°N 40°S. In general, water column was stratified, surface layers were nutrient-poor microplankton (hereafter phytoplankton, for simplicity, although it...

10.1371/journal.pone.0151699 article EN cc-by PLoS ONE 2016-03-16
Zhibo Shao Yangchun Xu Hua Wang Weicheng Luo Lice Wang and 92 more Yuhong Huang Nona S. R. Agawin Ayaz Ahmed Mar Benavides Mikkel Bentzon‐Tilia Ilana Berman‐Frank Hugo Berthelot Isabelle C. Biegala Mariana B. Bif Antonio Bode Sophie Bonnet Deborah A. Bronk Mark V. Brown Lisa Campbell Douglas G. Capone Edward J. Carpenter Nicolas Cassar Bonnie X. Chang Dreux Chappell Yuh-ling Lee Chen Matthew J. Church Francisco M. Cornejo‐Castillo Amália Maria Sacilotto Detoni Scott C. Doney Cécile Dupouy Marta Estrada Camila Fernández Bieito Fernández Castro Debany Fonseca-Batista Rachel A. Foster Ken Furuya Nicole Garcia Kanji Goto Jesús Gago Mary R. Gradoville M. Robert Hamersley Britt A. Henke Cora Hörstmann Amal Jayakumar Zhibing Jiang Shuh‐Ji Kao David M. Karl Leila Kittu Angela N. Knapp Sanjeev Kumar Julie LaRoche Hongbin Liu Jiaxing Liu Caroline Lory Carolin Löscher Emilio Marañón Lauren F. Messer Matthew M. Mills Wiebke Mohr Pia H. Moisander Claire Mahaffey Robert M. Moore Beatriz Mouriño‐Carballido Margaret R. Mulholland Shin‐Ichiro Nakaoka Joseph A. Needoba Eric J. Raes Eyal Rahav Teodoro Ramı́rez C. Christiansen Lasse Riemann Virginie Riou Julie Robidart V. V. S. S. Sarma Takuya Sato Himanshu Saxena Corday Selden Justin R. Seymour Dalin Shi Takuhei Shiozaki Arvind Singh Rachel E. Sipler Jun Sun Koji Suzuki Kazutaka Takahashi Yehui Tan Weiyi Tang Jean‐Éric Tremblay Kendra A. Turk‐Kubo Zuozhu Wen Angelicque White Samuel T. Wilson Takashi Yoshida Jonathan P. Zehr Run Zhang Yao Zhang Ya‐Wei Luo

Abstract. Marine diazotrophs convert dinitrogen (N2) gas into bioavailable nitrogen (N), supporting life in the global ocean. In 2012, first version of oceanic diazotroph database (version 1) was published. Here, we present an updated 2), significantly increasing number situ diazotrophic measurements from 13 565 to 55 286. Data points for N2 fixation rates, cell abundance, and nifH gene copy abundance have increased by 184 %, 86 809 respectively. Version 2 includes two new data sheets...

10.5194/essd-15-3673-2023 article EN cc-by Earth system science data 2023-08-15

10.1016/s0967-0653(98)82183-2 article EN Oceanographic literature review 1998-03-01

Abstract. Coccolithophores are calcifying marine phytoplankton of the class Prymnesiophyceae. They considered to play an import role in global carbon cycle through production and export organic calcite. We have compiled observations coccolithophore abundance from several existing databases as well individual contributions published unpublished datasets. make conservative estimates biomass using standardised conversion methods provide uncertainty associated with these values. The...

10.5194/essd-5-259-2013 article EN cc-by Earth system science data 2013-07-12

We carried out monthly photosynthesis-irradiance (P-E) experiments with the 14C-method for 12 years (2003–2014) to determine photosynthetic parameters and primary production of surface phytoplankton in Blanes Bay Microbial Observatory, a coastal sampling station NW Mediterranean Sea. Our goal was obtain seasonal trends establish basis detecting future changes this oligotrophic area. The maximal rate PBmax ranged 30-fold (0.5-15 mg C Chl a–1 h–1), averaged 3.7 h–1 (±0.25 SE) highest August...

10.3989/scimar.04480.06e article EN cc-by Scientia Marina 2016-09-30

The oligotrophic subtropical gyres are the largest biome on Earth, where picoplankton constitute dominant autotrophs. trend for autotrophic to increase with sea temperature has led predictions that picophytoplankton abundance will warming. Here we conducted a global survey in open subtropical-tropical ocean resolve functional relationships between and oceanic properties (water temperature, chlorophyll concentration, nutrient concentrations, underwater visible ultraviolet B radiation). We...

10.3389/fmars.2018.00506 article EN cc-by Frontiers in Marine Science 2019-01-15

Deep ocean microbial communities rely on the organic carbon produced in sunlit ocean, yet it remains unknown whether surface processes determine assembly and function of bathypelagic prokaryotes to a larger extent than deep-sea physicochemical conditions. Here, we explored variations phytoplankton assemblages across Atlantic, Pacific Indian stations can explain structural changes (ca. 4,000 m) free-living particle-attached prokaryotic (characterized through 16S rRNA gene sequencing), as well...

10.1111/mec.15454 article EN Molecular Ecology 2020-04-23

Sea spray aerosol (SSA) formation plays a major role in the climate system. The Antarctic Peninsula (AP) is affected by greatest warming occurring Southern Ocean; changes cryospheric and biological processes are being observed. Whilst there some evidence that organic material produced ice algae and/or phytoplankton high Arctic contributes to SSA, less known about (sympagic) regions. To gain insight into influence of biology biogeochemistry on atmospheric aerosol, we report simultaneous...

10.3389/fmars.2022.827061 article EN cc-by Frontiers in Marine Science 2022-06-16

MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout JournalEditorsTheme Sections 259:303-309 (2003) - doi:10.3354/meps259303 Relative grazing impact of microzooplankton and mesozooplankton on a bloom toxic dinoflagellate Alexandrium minutum Albert Calbet*, Dolors Vaqué, Jordi Felipe, Magda Vila, Maria Montserrat Sala, Miquel Alcaraz, Marta Estrada Institut de Ciències del Mar CMIMA...

10.3354/meps259303 article EN Marine Ecology Progress Series 2003-01-01

The diversity of prokaryotic and eukaryotic phytoplankton was studied along a gradient salinity in the solar salterns Bras del Port Santa Pola (Alacant, Spain) using different community descriptors. Chlorophyll a, HPLC pigment composition, flow cytometrically-determined picoplankton concentration, taxonomic composition (based on optical microscopy) genetic fingerprint patterns 16S (cyanobacteria- chloroplast-specific primers) 18S rRNA genes were determined for samples from ponds with...

10.1016/j.femsec.2004.04.002 article EN FEMS Microbiology Ecology 2004-04-21

MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout JournalEditorsTheme Sections 212:53-67 (2001) - doi:10.3354/meps212053 Short-term variability of photosynthetic parameters and particulate dissolved primary production in Alboran Sea (SW Mediterranean) Xosé Anxelu G. Morán*, Marta Estrada Departament de Biologia Marina i Oceanografia, Institut Ciències del Mar, CSIC, Pg. Joan Borbó, s/n,...

10.3354/meps212053 article EN Marine Ecology Progress Series 2001-01-01
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