1
|
Anderson RP, Mughal S, Wedlake GO. Proterozoic microfossils continue to provide new insights into the rise of complex eukaryotic life. ROYAL SOCIETY OPEN SCIENCE 2024; 11:240154. [PMID: 39170929 PMCID: PMC11336685 DOI: 10.1098/rsos.240154] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/26/2024] [Revised: 07/11/2024] [Accepted: 07/12/2024] [Indexed: 08/23/2024]
Abstract
Eukaryotes have evolved to dominate the biosphere today, accounting for most documented living species and the vast majority of the Earth's biomass. Consequently, understanding how these biologically complex organisms initially diversified in the Proterozoic Eon over 539 million years ago is a foundational question in evolutionary biology. Over the last 70 years, palaeontologists have sought to document the rise of eukaryotes with fossil evidence. However, the delicate and microscopic nature of their sub-cellular features affords early eukaryotes diminished preservation potential. Chemical biomarker signatures of eukaryotes and the genetics of living eukaryotes have emerged as complementary tools for reconstructing eukaryote ancestry. In this review, we argue that exceptionally preserved Proterozoic microfossils are critical to interpreting these complementary tools, providing crucial calibrations to molecular clocks and testing hypotheses of palaeoecology. We highlight recent research on their preservation and biomolecular composition that offers new ways to enhance their utility.
Collapse
Affiliation(s)
- Ross P. Anderson
- Museum of Natural History, University of Oxford, OxfordOX1 3PW, UK
- All Souls College, University of Oxford, OxfordOX1 4AL, UK
| | - Sanaa Mughal
- Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AlbertaT6G 2E3, Canada
| | - George O. Wedlake
- Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, UK
| |
Collapse
|
2
|
Yu Y, Li YP, Ren K, Hao X, Fru EC, Rønn R, Rivera WL, Becker K, Feng R, Yang J, Rensing C. A brief history of metal recruitment in protozoan predation. Trends Microbiol 2024; 32:465-476. [PMID: 38103995 DOI: 10.1016/j.tim.2023.11.008] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/08/2023] [Revised: 11/20/2023] [Accepted: 11/23/2023] [Indexed: 12/19/2023]
Abstract
Metals and metalloids are used as weapons for predatory feeding by unicellular eukaryotes on prokaryotes. This review emphasizes the role of metal(loid) bioavailability over the course of Earth's history, coupled with eukaryogenesis and the evolution of the mitochondrion to trace the emergence and use of the metal(loid) prey-killing phagosome as a feeding strategy. Members of the genera Acanthamoeba and Dictyostelium use metals such as zinc (Zn) and copper (Cu), and possibly metalloids, to kill their bacterial prey after phagocytosis. We provide a potential timeline on when these capacities first evolved and how they correlate with perceived changes in metal(loid) bioavailability through Earth's history. The origin of phagotrophic eukaryotes must have postdated the Great Oxidation Event (GOE) in agreement with redox-dependent modification of metal(loid) bioavailability for phagotrophic poisoning. However, this predatory mechanism is predicted to have evolved much later - closer to the origin of the multicellular metazoans and the evolutionary development of the immune systems.
Collapse
Affiliation(s)
- Yanshuang Yu
- Institute of Environmental Microbiology, College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China
| | - Yuan-Ping Li
- Institute of Environmental Microbiology, College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China
| | - Kexin Ren
- Aquatic EcoHealth Group, Fujian Key Laboratory of Watershed Ecology, Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
| | - Xiuli Hao
- Hubei Key Laboratory of Soil Environment and Pollution Remediation, Huazhong Agricultural University, Wuhan 430070, China
| | - Ernest Chi Fru
- Centre for Geobiology and Geochemistry, School of Earth and Ocean Sciences, Cardiff University, CF10 3AT Cardiff, UK
| | - Regin Rønn
- Department of Biology, University of Copenhagen, Copenhagen, Denmark
| | - Windell L Rivera
- Pathogen-Host-Environment Interactions Research Laboratory, Institute of Biology, College of Science, University of the Philippines Diliman, Quezon City 1101, Philippines
| | - Karsten Becker
- Friedrich Loeffler-Institute for Medical Microbiology, University Medicine Greifswald, D-17489 Greifswald, Germany
| | - Renwei Feng
- Institute of Environmental Microbiology, College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China
| | - Jun Yang
- Aquatic EcoHealth Group, Fujian Key Laboratory of Watershed Ecology, Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China.
| | - Christopher Rensing
- Institute of Environmental Microbiology, College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China.
| |
Collapse
|
3
|
Bowles AMC, Williamson CJ, Williams TA, Donoghue PCJ. Cryogenian Origins of Multicellularity in Archaeplastida. Genome Biol Evol 2024; 16:evae026. [PMID: 38333966 PMCID: PMC10883732 DOI: 10.1093/gbe/evae026] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/04/2023] [Revised: 01/30/2024] [Accepted: 02/03/2024] [Indexed: 02/10/2024] Open
Abstract
Earth was impacted by global glaciations during the Cryogenian (720 to 635 million years ago; Ma), events invoked to explain both the origins of multicellularity in Archaeplastida and radiation of the first land plants. However, the temporal relationship between these environmental and biological events is poorly established, due to a paucity of molecular and fossil data, precluding resolution of the phylogeny and timescale of archaeplastid evolution. We infer a time-calibrated phylogeny of early archaeplastid evolution based on a revised molecular dataset and reappraisal of the fossil record. Phylogenetic topology testing resolves deep archaeplastid relationships, identifying two clades of Viridiplantae and placing Bryopsidales as sister to the Chlorophyceae. Our molecular clock analysis infers an origin of Archaeplastida in the late-Paleoproterozoic to early-Mesoproterozoic (1712 to 1387 Ma). Ancestral state reconstruction of cytomorphological traits on this time-calibrated tree reveals many of the independent origins of multicellularity span the Cryogenian, consistent with the Cryogenian multicellularity hypothesis. Multicellular rhodophytes emerged 902 to 655 Ma while crown-Anydrophyta (Zygnematophyceae and Embryophyta) originated 796 to 671 Ma, broadly compatible with the Cryogenian plant terrestrialization hypothesis. Our analyses resolve the timetree of Archaeplastida with age estimates for ancestral multicellular archaeplastids coinciding with the Cryogenian, compatible with hypotheses that propose a role of Snowball Earth in plant evolution.
Collapse
Affiliation(s)
- Alexander M C Bowles
- School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, UK
- Bristol Palaeobiology Group, School of Biological Sciences and School of Earth Sciences, Life Sciences Building, University of Bristol, Bristol BS8 1TQ, UK
| | | | - Tom A Williams
- Bristol Palaeobiology Group, School of Biological Sciences and School of Earth Sciences, Life Sciences Building, University of Bristol, Bristol BS8 1TQ, UK
| | - Philip C J Donoghue
- Bristol Palaeobiology Group, School of Biological Sciences and School of Earth Sciences, Life Sciences Building, University of Bristol, Bristol BS8 1TQ, UK
| |
Collapse
|
4
|
Mills DB, Simister RL, Sehein TR, Hallam SJ, Sperling EA, Crowe SA. Constraining the oxygen requirements for modern microbial eukaryote diversity. Proc Natl Acad Sci U S A 2024; 121:e2303754120. [PMID: 38165897 PMCID: PMC10786294 DOI: 10.1073/pnas.2303754120] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/06/2023] [Accepted: 11/07/2023] [Indexed: 01/04/2024] Open
Abstract
Eukaryotes originated prior to the establishment of modern marine oxygen (O2) levels. According to the body fossil and lipid biomarker records, modern (crown) microbial eukaryote lineages began diversifying in the ocean no later than ~800 Ma. While it has long been predicted that increasing atmospheric O2 levels facilitated the early diversification of microbial eukaryotes, the O2 levels needed to permit this diversification remain unconstrained. Using time-resolved geochemical parameter and gene sequence information from a model marine oxygen minimum zone spanning a range of dissolved O2 levels and redox states, we show that microbial eukaryote taxonomic richness and phylogenetic diversity remain the same until O2 declines to around 2 to 3% of present atmospheric levels, below which these diversity metrics become significantly reduced. Our observations suggest that increasing O2 would have only directly promoted early crown-eukaryote diversity if atmospheric O2 was below 2 to 3% of modern levels when crown-eukaryotes originated and then later met or surpassed this range as crown-eukaryotes diversified. If atmospheric O2 was already consistently at or above 2 to 3% of modern levels by the time that crown-eukaryotes originated, then the subsequent diversification of modern microbial eukaryotes was not directly driven by atmospheric oxygenation.
Collapse
Affiliation(s)
- Daniel B. Mills
- Department of Earth and Environmental Sciences, Paleontology and Geobiology, Ludwig-Maximilians-Universität München, 80333Munich, Germany
- Department of Earth and Planetary Sciences, Stanford University, Stanford, CA94305
- The Penn State Extraterrestrial Intelligence Center, The Pennsylvania State University, University Park, PA16802
| | - Rachel L. Simister
- Department of Microbiology and Immunology, University of British Columbia, Vancouver, BCV6T 1Z4, Canada
| | - Taylor R. Sehein
- Department of Biological Sciences, Smith College, Northampton, MA01063
| | - Steven J. Hallam
- Department of Microbiology and Immunology, University of British Columbia, Vancouver, BCV6T 1Z4, Canada
- Genome Science and Technology Program, University of British Columbia, Vancouver, BCV6T 1Z4, Canada
- Graduate Program in Bioinformatics, University of British Columbia, Vancouver, BCV6T 1Z4, Canada
- Life Sciences Institute, University of British Columbia, Vancouver, BCV6T 1Z3, Canada
- Bradshaw Research Initiative for Minerals and Mining, University of British Columbia, Vancouver, BCV6T 1Z4, Canada
- Ecosystem Services, Commercialization Platforms and Entrepreneurship (ECOSCOPE) Training Program, University of British Columbia, Vancouver, BCV6T 1Z3, Canada
| | - Erik A. Sperling
- Department of Earth and Planetary Sciences, Stanford University, Stanford, CA94305
| | - Sean A. Crowe
- Department of Microbiology and Immunology, University of British Columbia, Vancouver, BCV6T 1Z4, Canada
- Department of Earth, Ocean, and Atmospheric Sciences, University of British Columbia, Vancouver, BCV6T 1Z4, Canada
| |
Collapse
|
5
|
Crockford PW, Bar On YM, Ward LM, Milo R, Halevy I. The geologic history of primary productivity. Curr Biol 2023; 33:4741-4750.e5. [PMID: 37827153 DOI: 10.1016/j.cub.2023.09.040] [Citation(s) in RCA: 4] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/28/2023] [Revised: 09/11/2023] [Accepted: 09/18/2023] [Indexed: 10/14/2023]
Abstract
The rate of primary productivity is a keystone variable in driving biogeochemical cycles today and has been throughout Earth's past.1 For example, it plays a critical role in determining nutrient stoichiometry in the oceans,2 the amount of global biomass,3 and the composition of Earth's atmosphere.4 Modern estimates suggest that terrestrial and marine realms contribute near-equal amounts to global gross primary productivity (GPP).5 However, this productivity balance has shifted significantly in both recent times6 and through deep time.7,8 Combining the marine and terrestrial components, modern GPP fixes ≈250 billion tonnes of carbon per year (Gt C year-1).5,9,10,11 A grand challenge in the study of the history of life on Earth has been to constrain the trajectory that connects present-day productivity to the origin of life. Here, we address this gap by piecing together estimates of primary productivity from the origin of life to the present day. We estimate that ∼1011-1012 Gt C has cumulatively been fixed through GPP (≈100 times greater than Earth's entire carbon stock). We further estimate that 1039-1040 cells have occupied the Earth to date, that more autotrophs than heterotrophs have ever existed, and that cyanobacteria likely account for a larger proportion than any other group in terms of the number of cells. We discuss implications for evolutionary trajectories and highlight the early Proterozoic, which encompasses the Great Oxidation Event (GOE), as the time where most uncertainty exists regarding the quantitative census presented here.
Collapse
Affiliation(s)
- Peter W Crockford
- Department of Earth Sciences, Carleton University, Ottawa, ON K1S 5B6, Canada; Department of Earth and Planetary Sciences, Weizmann Institute of Science, 7610001 Rehovot, Israel; Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
| | - Yinon M Bar On
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, 7610001 Rehovot, Israel; Division of Geological Sciences, California Institute of Technology, Pasadena, CA 91125, USA
| | - Luce M Ward
- Department of Geosciences, Smith College, Northampton, MA 01063, USA
| | - Ron Milo
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, 7610001 Rehovot, Israel
| | - Itay Halevy
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, 7610001 Rehovot, Israel
| |
Collapse
|
6
|
Abstract
The origin of modern eukaryotes is one of the key transitions in life's history, and also one of the least understood. Although the fossil record provides the most direct view of this process, interpreting the fossils of early eukaryotes and eukaryote-grade organisms is not straightforward. We present two end-member models for the evolution of modern (i.e., crown) eukaryotes-one in which modern eukaryotes evolved early, and another in which they evolved late-and interpret key fossils within these frameworks, including where they might fit in eukaryote phylogeny and what they may tell us about the evolution of eukaryotic cell biology and ecology. Each model has different implications for understanding the rise of complex life on Earth, including different roles of Earth surface oxygenation, and makes different predictions that future paleontological studies can test.
Collapse
Affiliation(s)
- Susannah M Porter
- Department of Earth Science, University of California at Santa Barbara, Santa Barbara, California, USA;
| | - Leigh Anne Riedman
- Department of Earth Science, University of California at Santa Barbara, Santa Barbara, California, USA;
- Earth Research Institute, University of California at Santa Barbara, Santa Barbara, California, USA;
| |
Collapse
|
7
|
Kang J, Gill B, Reid R, Zhang F, Xiao S. Nitrate limitation in early Neoproterozoic oceans delayed the ecological rise of eukaryotes. SCIENCE ADVANCES 2023; 9:eade9647. [PMID: 36947611 PMCID: PMC10032604 DOI: 10.1126/sciadv.ade9647] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 09/19/2022] [Accepted: 02/17/2023] [Indexed: 06/18/2023]
Abstract
The early Neoproterozoic Era witnessed the initial ecological rise of eukaryotes at ca. 800 Ma. To assess whether nitrate availability played an important role in this evolutionary event, we measured nitrogen isotope compositions (δ15N) of marine carbonates from the early Tonian (ca. 1000 Ma to ca. 800 Ma) Huaibei Group in North China. The data reported here fill a critical gap in the δ15N record and indicate nitrate limitation in early Neoproterozoic oceans. A compilation of Proterozoic sedimentary δ15N data reveals a stepwise increase in δ15N values at ~800 Ma. Box model simulations indicate that this stepwise increase likely represents a ~50% increase in marine nitrate availability. Limited nitrate availability in early Neoproterozoic oceans may have delayed the ecological rise of eukaryotes until ~800 Ma when increased nitrate supply, together with other environmental and ecological factors, may have contributed to the transition from prokaryote-dominant to eukaryote-dominant marine ecosystems.
Collapse
Affiliation(s)
- Junyao Kang
- Department of Geosciences, Virginia Tech, Blacksburg, VA, USA
- Global Change Center, Virginia Tech, Blacksburg, VA, USA
| | - Benjamin Gill
- Department of Geosciences, Virginia Tech, Blacksburg, VA, USA
- Global Change Center, Virginia Tech, Blacksburg, VA, USA
| | - Rachel Reid
- Department of Geosciences, Virginia Tech, Blacksburg, VA, USA
- Global Change Center, Virginia Tech, Blacksburg, VA, USA
| | - Feifei Zhang
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Shuhai Xiao
- Department of Geosciences, Virginia Tech, Blacksburg, VA, USA
- Global Change Center, Virginia Tech, Blacksburg, VA, USA
| |
Collapse
|