I am interested in how Earth’s smallest constituents, microbes, cycle nutrients in aquatic ecosystems. I earned my PhD from the Department of Earth System Science at Stanford University focused on microbial ecology. I used molecular and biogeochemical approaches to understand the abundance, distribution, and activity of nitrifying bacteria and archaea in San Francisco Bay. My research used DNA, RNA, nitrification rate, and water quality data to uncover and characterize recurring massive ammonia-oxidizing archaea blooms in South Bay. For my postdoctoral work, I will use metagenomics to study subsurface microbial ecology in a river floodplain in collaboration with the Floodplain Hydro-Biogeochemistry Scientific Focus Area managed by a team at the SLAC National Accelerator Laboratory.

Honors & Awards

  • McGee-Levorsen Research Grant, Stanford Earth (April 2019, August 2020)
  • Data Science Scholar, Stanford Data Science (01/2020-12/2021)
  • Amherst College Fellowship, Amherst College (2016, 2017, 2018)
  • Graduate Research Fellowship Program (GRFP), NSF (September 2016-2021)
  • Best Session Talk, Research Review Stanford Earth (April 2018)

Professional Education

  • Doctor of Philosophy, Stanford University, ESS-PHD (2022)
  • BA, Amherst College, Biology (2013)

Stanford Advisors

Current Research and Scholarly Interests

I am interested in the co-evolution of life and Earth, and am particularly interested in the ecology of Earth's smallest constituents: microbes. Along my path towards graduate school, I become particularly interested in marine bacteria and archaea and how they impact global biogeochemical cycles. My graduate research focused on the ecology and activity of ammonia and nitrite-eating microbes in the highly nitrogen polluted San Francisco Bay estuary. I used DNA-based and biogeochemical techniques to study some of my favorite organisms, ammonia-oxidizing archaea, that use electrons from ammonia in their energy metabolism and produce nitrite in the process. For my postdoctoral research I am focusing on microbial communities in the subsurface of river floodplains.

All Publications

  • Genome-Resolved Metagenomic Insights into Massive Seasonal Ammonia-Oxidizing Archaea Blooms in San Francisco Bay. mSystems Rasmussen, A. N., Francis, C. A. 1800: e0127021


    Ammonia-oxidizing archaea (AOA) are key for the transformation of ammonia to oxidized forms of nitrogen in aquatic environments around the globe, including nutrient-rich coastal and estuarine waters such as San Francisco Bay (SFB). Using metagenomics and 16S rRNA gene amplicon libraries, we found that AOA are more abundant than ammonia-oxidizing bacteria (AOB) and nitrite-oxidizing bacteria (NOB), except in the freshwater stations in SFB. In South SFB, we observed recurrent AOA blooms of "Candidatus Nitrosomarinus catalina" SPOT01-like organisms, which account for over 20% of 16S rRNA gene amplicons in both surface and bottom waters and co-occur with weeks of high nitrite concentrations (>10muM) in the oxic water column. We observed pronounced nitrite peaks occurring in the autumn for 7 of the last 9years (2012 to 2020), suggesting that seasonal AOA blooms are common in South SFB. We recovered two high-quality AOA metagenome-assembled genomes (MAGs), including a Nitrosomarinus-like genome from the South SFB bloom and another Nitrosopumilus genome originating from Suisun Bay in North SFB. Both MAGs cluster with genomes from other estuarine/coastal sites. Analysis of Nitrosomarinus-like genomes show that they are streamlined, with low GC content and high coding density, and harbor urease genes. Our findings support the unique niche of Nitrosomarinus-like organisms which dominate coastal/estuarine waters and provide insights into recurring AOA blooms in SFB. IMPORTANCE Ammonia-oxidizing archaea (AOA) carry out key transformations of ammonia in estuarine systems such as San Francisco Bay (SFB)-the largest estuary on the west coast of North America-and play a significant role in both local and global nitrogen cycling. Using metagenomics and 16S rRNA gene amplicon libraries, we document a massive, recurrent AOA bloom in South SFB that co-occurs with months of high nitrite concentrations in the oxic water column. Our study is the first to generate metagenome-assembled genomes (MAGs) from SFB, and through this process we recovered two high-quality AOA MAGs, one of which originated from bloom samples. These AOA MAGs yield new insight into the Nitrosopumilus and Nitrosomarinus-like lineages and their potential niches in coastal and estuarine systems. Nitrosomarinus-like AOA are abundant in coastal regions around the globe, and we highlight the common occurrence of urease genes, low GC content, and range of salinity tolerances within this lineage.

    View details for DOI 10.1128/msystems.01270-21

    View details for PubMedID 35076275

  • Genome-Resolved Metagenomic Insights into Massive Seasonal Ammonia-Oxidizing Archaea Blooms in San Francisco Bay MSYSTEMS Rasmussen, A. N., Francis, C. A. 2022; 7 (1)
  • In-depth Spatiotemporal Characterization of Planktonic Archaeal and Bacterial Communities in North and South San Francisco Bay. Microbial ecology Rasmussen, A. N., Damashek, J. n., Eloe-Fadrosh, E. A., Francis, C. A. 2020


    Despite being the largest estuary on the west coast of North America, no in-depth survey of microbial communities in San Francisco Bay (SFB) waters currently exists. In this study, we analyze bacterioplankton and archaeoplankton communities at several taxonomic levels and spatial extents (i.e., North versus South Bay) to reveal patterns in alpha and beta diversity. We assess communities using high-throughput sequencing of the 16S rRNA gene in 177 water column samples collected along a 150-km transect over a 2-year monthly time-series. In North Bay, the microbial community is strongly structured by spatial salinity changes while in South Bay seasonal variations dominate community dynamics. Along the steep salinity gradient in North Bay, we find that operational taxonomic units (OTUs; 97% identity) have higher site specificity than at coarser taxonomic levels and turnover ("species" replacement) is high, revealing a distinct brackish community (in oligo-, meso-, and polyhaline samples) from fresh and marine end-members. At coarser taxonomic levels (e.g., phylum, class), taxa are broadly distributed across salinity zones (i.e., present/abundant in a large number of samples) and brackish communities appear to be a mix of fresh and marine communities. We also observe variations in brackish communities between samples with similar salinities, likely related to differences in water residence times between North and South Bay. Throughout SFB, suspended particulate matter is positively correlated with richness and influences changes in beta diversity. Within several abundant groups, including the SAR11 clade (comprising up to 30% of reads in a sample), OTUs appear to be specialized to a specific salinity range. Some other organisms also showed pronounced seasonal abundance, including Synechococcus, Ca. Actinomarina, and Nitrosopumilus-like OTUs. Overall, this study represents the first in-depth spatiotemporal survey of SFB microbial communities and provides insight into how planktonic microorganisms have specialized to different niches along the salinity gradient.

    View details for DOI 10.1007/s00248-020-01621-7

    View details for PubMedID 33150499

  • Emergence of trait variability through the lens of nitrogen assimilation in Prochlorococcus ELIFE Berube, P. M., Rasmussen, A., Braakman, R., Stepanauskas, R., Chisholm, S. W. 2019; 8


    Intraspecific trait variability has important consequences for the function and stability of marine ecosystems. Here we examine variation in the ability to use nitrate across hundreds of Prochlorococcus genomes to better understand the modes of evolution influencing intraspecific allocation of ecologically important functions. Nitrate assimilation genes are absent in basal lineages but occur at an intermediate frequency that is randomly distributed within recently emerged clades. The distribution of nitrate assimilation genes within clades appears largely governed by vertical inheritance, gene loss, and homologous recombination. By mapping this process onto a model of Prochlorococcus' macroevolution, we propose that niche-constructing adaptive radiations and subsequent niche partitioning set the stage for loss of nitrate assimilation genes from basal lineages as they specialized to lower light levels. Retention of these genes in recently emerged lineages has likely been facilitated by selection as they sequentially partitioned into niches where nitrate assimilation conferred a fitness benefit.

    View details for DOI 10.7554/eLife.41043

    View details for Web of Science ID 000458353700001

    View details for PubMedID 30706847

    View details for PubMedCentralID PMC6370341