Francisco Chavez de la O

Prof. Dr. Francisco Chavez de la O


Research Focus & Metrics

Academic Career Length

36Years (1991-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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5 January 2018 in Science
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Journal Article
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DBDenise Breitburg
Denise Breitburg
LLLisa A. Levin
Lisa A. Levin
AOAndreas Oschlies
Andreas Oschlies
MGMarilaure Grégoire
Marilaure Grégoire
FOFrancisco Chavez de la O
Francisco Chavez de la O
JZJing Zhang
Jing Zhang
Beneath the waves, oxygen disappears: As plastic waste pollutes the oceans and fish stocks decline, unseen below the surface another problem grows: deoxygenation. Breitburg et al. review the evidence for the downward trajectory of oxygen levels in increasing areas of the open ocean and coastal waters. Rising nutrient loads coupled with climate change—each resulting from human activities—are changing ocean biogeochemistry and increasing oxygen consumption. This results in destabilization of sediments and fundamental shifts in the availability of key nutrients. In the short term, some compensatory effects may result in improvements in local fisheries, such as in cases where stocks are squeezed between the surface and elevated oxygen minimum zones. In the longer term, these conditions are unsustainable and may result in ecosystem collapses, which ultimately will cause societal and economic harm. Science , this issue p. eaam7240

10 January 2003 in Science
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Journal Article
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FOFrancisco Chavez de la O
Francisco Chavez de la O
JRJohn Ryan
John Ryan
SLSalvador E Lluch-Cota
Salvador E Lluch-Cota
MCMiguel Ñiquen C.
Miguel Ñiquen C.
In the Pacific Ocean, air and ocean temperatures, atmospheric carbon dioxide, landings of anchovies and sardines, and the productivity of coastal and open ocean ecosystems have varied over periods of about 50 years. In the mid-1970s, the Pacific changed from a cool “anchovy regime” to a warm “sardine regime.” A shift back to an anchovy regime occurred in the middle to late 1990s. These large-scale, naturally occurring variations must be taken into account when considering human-induced climate change and the management of ocean living resources.

10 December 1999 in Science
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Journal Article
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FOFrancisco Chavez de la O
Francisco Chavez de la O
PSP. G. Strutton
P. G. Strutton
GFG. E. Friederich
G. E. Friederich
RFR. A. Feely
R. A. Feely
GFG. C. Feldman
G. C. Feldman
MMM. J. McPhaden
M. J. McPhaden
During the 1997–98 El Niño, the equatorial Pacific Ocean retained 0.7 × 10 15 grams of carbon that normally would have been lost to the atmosphere as carbon dioxide. The surface ocean became impoverished in plant nutrients, and chlorophyll concentrations were the lowest on record. A dramatic recovery occurred in mid-1998, the system became highly productive, analogous to coastal environments, and carbon dioxide flux out of the ocean was again high. The spatial extent of the phytoplankton bloom that followed recovery from El Niño was the largest ever observed for the equatorial Pacific. These chemical and ecological perturbations were linked to changes in the upwelling of nutrient-enriched waters. The description and explanation of these dynamic changes would not have been possible without an observing system that combines biological, chemical, and physical sensors on moorings with remote sensing of chlorophyll.

15 January 2011 in Annual Review of Marine Science
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Journal Article
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FOFrancisco Chavez de la O
Francisco Chavez de la O
MMMonique Messié
Monique Messié
JPJ. Timothy Pennington
J. Timothy Pennington
Marine photosynthetic plankton are responsible for approximately 50 petagrams (1015) of carbon per year of net primary production, an amount equivalent to that on land. This primary production supports essentially all life in the oceans and profoundly affects global biogeochemical cycles and climate. This review discusses the general distribution of primary production in the sea, the processes that regulate this distribution, and how marine primary production is sensitive to climate variability and change. Statistical modes of ocean variability and their characteristic interannual to multi-decadal timescales over the last century are described. Recent in situ and satellite time-series of primary production can be clearly linked to interannual ocean variability. Global marine primary production appears to have increased over the past several decades in association with multi-decadal variations. A paleoclimate record extends discussion to the centennial scale, providing contrasting insights into how marine primary production might vary in the future.

1 April 1999 in Deep Sea Research Part I: Oceanographic Research Papers
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Journal Article
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MAMark A. Altabet
Mark A. Altabet
CPCynthia Pilskaln
Cynthia Pilskaln
RTRobert Thunell
Robert Thunell
CPCarol Pride
Carol Pride
DSDaniel Sigman
Daniel Sigman
RFRoger Francois
Roger Francois

14 January 2020 in Nature Communications
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Journal Article
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ADAnni Djurhuus
Anni Djurhuus
CCCollin J. Closek
Collin J. Closek
RKRyan P. Kelly
Ryan P. Kelly
KPKathleen J. Pitz
Kathleen J. Pitz
RMReiko P. Michisaki
Reiko P. Michisaki
MBMya Breitbart
Mya Breitbart
Environmental DNA (eDNA) analysis allows the simultaneous examination of organisms across multiple trophic levels and domains of life, providing critical information about the complex biotic interactions related to ecosystem change. Here we used multilocus amplicon sequencing of eDNA to survey biodiversity from an eighteen-month (2015–2016) time-series of seawater samples from Monterey Bay, California. The resulting dataset encompasses 663 taxonomic groups (at Family or higher taxonomic rank) ranging from microorganisms to mammals. We inferred changes in the composition of communities, revealing putative interactions among taxa and identifying correlations between these communities and environmental properties over time. Community network analysis provided evidence of expected predator-prey relationships, trophic linkages, and seasonal shifts across all domains of life. We conclude that eDNA-based analyses can provide detailed information about marine ecosystem dynamics and identify sensitive biological indicators that can suggest ecosystem changes and inform conservation strategies.