Jessica Carilli

ORCID: 0000-0003-1946-7551
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About
Contact & Profiles
Research Areas
  • Coral and Marine Ecosystems Studies
  • Marine and fisheries research
  • Marine and coastal plant biology
  • Marine animal studies overview
  • Oceanographic and Atmospheric Processes
  • Coastal and Marine Dynamics
  • Geology and Paleoclimatology Research
  • Ichthyology and Marine Biology
  • Geochemistry and Geologic Mapping
  • Marine Biology and Ecology Research
  • Microplastics and Plastic Pollution
  • Climate variability and models
  • Isotope Analysis in Ecology
  • Environmental Conservation and Management
  • Coastal and Marine Management
  • Heavy metals in environment
  • Maritime and Coastal Archaeology
  • Tropical and Extratropical Cyclones Research
  • Maritime Navigation and Safety
  • Calcium Carbonate Crystallization and Inhibition
  • Radioactivity and Radon Measurements
  • Marine and Offshore Engineering Studies
  • Materials Engineering and Processing
  • Radioactive contamination and transfer
  • Methemoglobinemia and Tumor Lysis Syndrome

Naval Information Warfare Center Pacific
2020-2024

ETH Zurich
2024

Naval Research Laboratory Information Technology Division
2023

Scripps Institution of Oceanography
2007-2022

University of California, San Diego
2008-2021

University of Massachusetts Boston
2014-2019

Australian Nuclear Science and Technology Organisation
2012-2019

Arthur Rylah Institute for Environmental Research
2012-2014

Coral bleaching, during which corals lose their symbiotic dinoflagellates, typically corresponds with periods of intense heat stress, and appears to be increasing in frequency geographic extent as the climate warms. A fundamental question coral reef ecology is whether chronic local stress reduces resistance resilience from episodic such or alternatively promotes acclimatization, potentially resilience. Here we show that following a major bleaching event, Montastraea faveolata growth rates at...

10.1371/journal.pone.0006324 article EN cc-by PLoS ONE 2009-07-21

Coral bleaching is the breakdown of symbiosis between coral animal hosts and their dinoflagellate algae symbionts in response to environmental stress. On large spatial scales, heat stress most common factor causing bleaching, which predicted increase frequency severity as climate warms. There evidence that temperature threshold at occurs varies with local conditions background conditions. We investigated influence past variability on susceptibility using natural gradient peak Gilbert...

10.1371/journal.pone.0034418 article EN cc-by PLoS ONE 2012-03-30

Microplastics (less than 5 mm) are a recognized threat to aquatic food webs because they ingested at multiple trophic levels and may bioaccumulate. In urban coastal environments, high densities of microplastics disrupt nutritional intake. However, behavioural dynamics consequences microparticle ingestion still poorly understood. As filter or suspension feeders, benthic marine invertebrates vulnerable microplastic ingestion. We explored by the temperate coral Astrangia poculata . detected an...

10.1098/rspb.2019.0726 article EN Proceedings of the Royal Society B Biological Sciences 2019-06-26

Abstract Previous studies have estimated that coastal cliffs exist on about 80% of the global shoreline, but not been validated a scale. This study uses two approaches to capture information worldwide existence and erosion cliffs: detailed literature survey imagery search, GIS‐based mapping analysis. The review show in 93% combined recognized independent states non‐independent regions (total 213 geographic units). Additionally, cliff retreat rates quantified at least one location within 33%...

10.1002/esp.4574 article EN cc-by-nc-nd Earth Surface Processes and Landforms 2018-12-28

Abstract Coral bleaching, during which corals lose their symbiotic dinoflagellates, appears to be increasing in frequency and geographic extent, is typically associated with abnormally high water temperatures solar irradiance. A key question coral reef ecology whether local stressors reduce the thermal tolerance threshold, leading increased bleaching incidence. Using tree‐ring techniques, we produced master chronologies of growth rates dominant builder, massive Montastraea faveolata corals,...

10.1111/j.1365-2486.2009.02043.x article EN Global Change Biology 2009-07-31

Anthropogenic

10.1016/j.epsl.2012.10.004 article EN cc-by-nc-nd Earth and Planetary Science Letters 2012-11-08

The Congo Basin is home to the world’s largest tropical peatland complex storing 29 PgC across 16.7 million ha, which poses a major unconstrained source of global wetland CH4. Key controls over their spatio-temporal variability remain unclear, limiting our ability assess responses future environmental change. Here, we present first time series in situ measurements from four intensive locations covering peat, seasonally flooded and terra firma forest ecosystems. Measurements were...

10.5194/egusphere-egu25-5933 preprint EN 2025-03-14

Abstract Frequent occurrences of coral bleaching and associated mortality over recent decades have raised concerns about the survival reefs in a warming planet. The El Niño-influenced central Gilbert Islands Republic Kiribati, which experience years with prolonged heat stress more frequently than 99% world’s reefs, may serve as natural model for community response to frequent stress. Here we use nine survey data (2004–2012) suite remote sensing variables from sites along gradients climate...

10.1038/s41598-019-40150-3 article EN cc-by Scientific Reports 2019-03-05

Abstract Equatorial Pacific ocean‐atmosphere interactions affect climate globally, and a key component of the coupled system is Walker Circulation, which driven by sea surface temperature (SST) gradients across equatorial Pacific. There conflicting evidence as to whether SST gradient Circulation have strengthened or weakened over late twentieth century. We present new records salinity (SSS) spanning 1959–2010 based on paired measurements Sr/Ca δ 18 O in massive Porites coral from Butaritari...

10.1002/2014pa002683 article EN Paleoceanography 2014-10-01

Coral reefs thrive and provide maximal ecosystem services when they support a multi-level trophic structure grow in favorable water quality conditions that include high light levels, rapid flow, low nutrient levels. Poor other anthropogenic stressors have caused coral mortality recent decades, leading to downgrading the loss of biological complexity on many reefs. Solutions reverse causes remain elusive, part because efforts restore are often attempted same diminished first place. Arks,...

10.3791/64778 article EN Journal of Visualized Experiments 2023-01-06

Abstract Per‐ and polyfluoroalkyl substances (PFAS) are a large group of synthetic compounds that have emerged as chemicals concern in drinking water groundwater. Typically, such waters treated to remove PFAS by passing the through bed sorbent material (e.g., activated carbon anion exchange resins [AIX]). However, efficacy these sorbents varies depending on types concentrations PFAS, addition quality conditions organic matter content conductivity (ionic strength). The choice effectively...

10.1002/rem.21747 article EN Remediation Journal 2023-01-29

MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout JournalEditorsTheme Sections 456:87-99 (2012) - DOI: https://doi.org/10.3354/meps09684 Benthic foraminiferal assemblages from Kiritimati (Christmas) Island indicate human-mediated nutrification has occurred over scale of decades Jessica Carilli1,*, Sheila Walsh2,3 1Institute for Environmental Research, Australian Nuclear Science and...

10.3354/meps09684 article EN Marine Ecology Progress Series 2012-06-07

Abstract Global surface temperatures during the twentieth century are characterized by multidecadal periods of accelerated or reduced warming, which thought to be driven Pacific decadal variability, specifically changes in trade‐wind strength. However, relationship between strength and global warming remains poorly constrained due scarcity instrumental wind observations. Previous work has shown that corals growing at Tarawa Atoll (1.3°N, 173°E) incorporate dissolved Mn flushed from lagoon...

10.1029/2020gc009398 article EN publisher-specific-oa Geochemistry Geophysics Geosystems 2021-01-18

Within boulder forming corals, fixation of dissolved inorganic carbon is performed by symbiotic dinoflagellates within the coral tissue and, to a lesser extent, endolithic algae skeleton. Endolithic produce distinctive green bands in skeleton, and their origin may be related periods bleaching due complete loss dinoflagellate symbionts or "paling" which symbiont populations are patchily reduced tissue. Stable isotopes were analyzed skeletons across known event 12 blooms determine whether...

10.1007/s00338-010-0667-5 article EN cc-by-nc Coral Reefs 2010-08-14

Abstract Coral bleaching caused by heat stress (warm water) will arguably be the greatest driver of coral reef loss in coming decades. Understanding how corals have adapted to distinct oceanographic regimes on multiple scales can provide insight into future tolerance and persistence, information critical directed intervention or targeted protections. The northern Line Islands span a gradient across latitudes, with seawater becoming warmer, fresher, more oligotrophic, saturated aragonite away...

10.1002/lno.10670 article EN Limnology and Oceanography 2017-10-05

Improved understanding of marine terrace development and morphology can provide better estimates historical sea levels tectonic uplift rates. Using a numerical model, this study explored the relative influence environmental controls on late Pleistocene widths San Clemente Island (SCI) in Santa Cruz region (SCZ) southern central California, respectively. The model was calibrated/validated based SCI SCZ observations using digital elevation models (DEMs), modeled nearshore wave climate, as well...

10.1016/j.geomorph.2021.107986 article EN cc-by-nc-nd Geomorphology 2021-10-15

GENERAL COMMENTARY article Front. Mar. Sci., 12 March 2019Sec. Coral Reef Research Volume 6 - 2019 | https://doi.org/10.3389/fmars.2019.00086

10.3389/fmars.2019.00086 article EN cc-by Frontiers in Marine Science 2019-03-12
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