# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Broadly sampled multigene trees of eukaryotes

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 2.0 which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The definitive version was published in BMC Evolutionary Biology 8 (2008): 14, doi:10.1186/1471-2148-8-14.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
Our understanding of the eukaryotic tree of life and the tremendous diversity of microbial eukaryotes is in flux as additional genes and diverse taxa are sampled for molecular analyses. Despite instability in many analyses, there is an increasing trend to classify eukaryotic diversity into six major supergroups: the 'Amoebozoa', 'Chromalveolata', 'Excavata', 'Opisthokonta', 'Plantae', and 'Rhizaria'. Previous molecular analyses have often suffered from either a broad taxon sampling using only single-gene data or have used multigene data with a limited sample of taxa. This study has two major aims: (1) to place taxa represented by 72 sequences, 61 of which have not been characterized previously, onto a well-sampled multigene genealogy, and (2) to evaluate the support for the six putative supergroups using two taxon-rich data sets and a variety of phylogenetic approaches.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
This project was made possible by a collaborative grant from the National Science Foundation Assembling the Tree of Life program (EF 04-31117) that was awarded to L.A.K., D.B., J.L., D.J.P., and to the ATCC

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Broadly sampled multigene trees of eukaryotes

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.contributor.author[].value
International Association of Aquatic and Marine Science Libraries and Information Centers

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Photographic identification guide to larvae at hydrothermal vents

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
The purpose of this guide is to assist researchers in the identification of larvae of benthic invertebrates at hydrothermal vents. Our work is based on plankton sampling at the East Pacific Rise 9-10°N vent field from 1991-2007, supplemented by benthic collections of juveniles. In addition to images and descriptions of the species, we included frequency data from large-volume plankton pump samples taken between 1998 and 2004 and time-series sediment trap samples from 2004-2005.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.identifier.citation[].value
Mills, S. W., Beaulieu, S. E., & Mullineaux, L. S. (2009). Photographic identification guide to larvae at hydrothermal vents. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/2996

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Photographic identification guide to larvae at hydrothermal vents

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Physeter macrocephalus Gulf of Mexico 6/16/2003 Animal a Depth Profile

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
Original Sampling Rate: 50 Hz, Sampling Rate of this file: 1Hz, Channels: 1, Resolution: .05 meters, Recording device: DTAG serial number 202, Filter: 4Hz

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
Location: Gulf of Mexico, Species: Physeter macrocephalus (Sperm Whale, Cachalot), Permit: Permit # 981-1707 issued to Peter L. Tyack, Water Depth: 973m

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.publisher[].value
The DTAG Project, Woods Hole Oceanographic Institution. Contact: dtag@whoi.edu

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Physeter macrocephalus Gulf of Mexico 6/16/2003 Animal a Depth Profile

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
The effect of sea level on glacial Indo-Pacific climate

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
Author Posting. © The Author(s), 2013.  This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution.  The definitive version was published in Nature Geoscience 6 (2013): 485–491, doi:10.1038/ngeo1823.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
The Indo-Pacific Warm Pool – the Earth’s largest body of warm water and main source of
heat and moisture to the global atmosphere – plays a prominent role in tropical and global
climate change. The physical mechanisms driving changes in the warm pool over glacial-interglacial timescales are largely unknown. Here we show that during the Last Glacial
Maximum (LGM) changes in global sea level influenced tropical climate by exposing the
Sunda Shelf and altering the Walker Circulation. Our result is based on a synthesis of marine and terrestrial proxies sensitive to hydroclimate and a multi-model ensemble of climate
simulations. The proxy data suggest drying throughout the warm pool, and wetter conditions in the western Indian and Pacific oceans. Only one model out of twelve simulates a
similar pattern of hydroclimate change, as measured by the Cohen’s   statistic. According to this model, weakened convection over the warm pool in response to exposure of the
Sunda Shelf drives the proxy-inferred hydrological changes. Our study demonstrates that
on glacial-interglacial timescales, ice sheets exert a first order influence on tropical climate
through changes in global sea level.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
Funding for this work was provided by NSF (grant AGS 1204011) and
the University of Hawaii.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
The effect of sea level on glacial Indo-Pacific climate

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
The Soviet maritime Arctic : proceedings of a workshop held May 10-13, 1987 by the Marine Policy Center of the Woods Hole Oceanographic Institution

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
This report is a summary of an international workshop on the Soviet
Maritime Arctic held May 10-13, 1987 by the Marine Policy Center of the Woods
Hole Oceanographic Institution. Twenty-eight scholars from Canada, Great
Britain, Norway and the United States participated. The workshop provided a
forum for Western scholars to examine and discuss Soviet domestic and
international policies regarding the Arctic Ocean. Interdisciplinary workshop
sessions addressed the following concerns: strategic, geographic, historical,
legal, scientific, technological, transportation, geopolitical and resource
development. This report includes an overview of the workshop, 15 abstracts
of contributed papers (8 with figures or tables), and an edited transcript of
the concluding discussion session. Appendices include the final program, a
list of participants and a list of discussion questions contributed by the
participants prior to the workshop. Several key findings of the workshop
include: more than 500 years of Russian involvement in the Arctic Ocean; USSR
operation of the world's largest polar fleet primarily for transportation and
resource development; Russian nationalism as a possible driving force in
Soviet activity in the Arctic; Soviet concerns for the Arctic representing an
amalgamation of interests (economic, security, environmental, resource,
others), none of which alone is predominant; probable Soviet participation in
international Arctic regimes based on past actions; and, Soviet legislative
enactments which indicate that the balance of interests embodied in the Law of
the Sea Convention are largely acceptable to the Soviet Union and that extreme
doctrinal views on the legal status of polar seas do not enjoy support in law
or State practice.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
Funding was provided by the John D. and Catherine T. MacArthur Foundation

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.identifier.citation[].value
Brigham, L. W., & Gately, E. M. (1988). The Soviet maritime Arctic: proceedings of a workshop held May 10-13, 1987 by the Marine Policy Center of the Woods Hole Oceanographic Institution. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/6927

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
The Soviet maritime Arctic : proceedings of a workshop held May 10-13, 1987 by the Marine Policy Center of the Woods Hole Oceanographic Institution

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Teamwork in the viscous oceanic microscale

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
© The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Kanso, E. A., Lopes, R. M., Strickler, J. R., Dabiri, J. O., & Costello, J. H.  Teamwork in the viscous oceanic microscale. Proceedings of the National Academy of Sciences of the United States of America, 118(29), (2021): e2018193118, https://doi.org/10.1073/pnas.2018193118.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
Nutrient acquisition is crucial for oceanic microbes, and competitive solutions to solve this challenge have evolved among a range of unicellular protists. However, solitary solutions are not the only approach found in natural populations. A diverse array of oceanic protists form temporary or even long-lasting attachments to other protists and marine aggregates. Do these planktonic consortia provide benefits to their members? Here, we use empirical and modeling approaches to evaluate whether the relationship between a large centric diatom, Coscinodiscus wailesii, and a ciliate epibiont, Pseudovorticella coscinodisci, provides nutrient flux benefits to the host diatom. We find that fluid flows generated by ciliary beating can increase nutrient flux to a diatom cell surface four to 10 times that of a still cell without ciliate epibionts. This cosmopolitan species of diatom does not form consortia in all environments but frequently joins such consortia in nutrient-depleted waters. Our results demonstrate that symbiotic consortia provide a cooperative alternative of comparable or greater magnitude to sinking for enhancement of nutrient acquisition in challenging environments.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
We are grateful to Y. Garcia for help with organism sampling and sorting. E.A.K. is funded by NSF-2100209, NSF RAISE IOS-2034043 and NIH R01 HL 153622-01A1. R.M.L. is a CNPq research fellow (grant # 310642/2017-5). J.H.C. and J.O.D. are funded by Grant NSF-2100705.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.identifier.citation[].value
Kanso, E. A., Lopes, R. M., Strickler, J. R., Dabiri, J. O., & Costello, J. H. (2021). Teamwork in the viscous oceanic microscale. Proceedings of the National Academy of Sciences of the United States of America, 118(29), e2018193118.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Teamwork in the viscous oceanic microscale

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Evaluating Southern Ocean biological production in two ocean biogeochemical models on daily to seasonal timescales using satellite chlorophyll and O2 / Ar observations

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeosciences 12 (2015): 681-695, doi:10.5194/bg-12-681-2015.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
We assess the ability of ocean biogeochemical models to represent seasonal structures in biomass and net community production (NCP) in the Southern Ocean. Two models are compared to observations on daily to seasonal timescales in four different sections of the region. We use daily satellite fields of chlorophyll (Chl) as a proxy for biomass and in situ observations of O2 and Ar supersaturation (ΔO2 / Ar) to estimate NCP. ΔO2 / Ar is converted to the flux of biologically generated O2 from sea to air (O2 bioflux). All data are aggregated to a climatological year with a daily resolution. To account for potential regional differences within the Southern Ocean, we conduct separate analyses of sections south of South Africa, around the Drake Passage, south of Australia, and south of New Zealand.

We find that the models simulate the upper range of Chl concentrations well, underestimate spring levels significantly, and show differences in skill between early and late parts of the growing season. While there is a great deal of scatter in the bioflux observations in general, the four sectors each have distinct patterns that the models pick up. Neither model exhibits a significant distinction between the Australian and New Zealand sectors and between the Drake Passage and African sectors. South of 60° S, the models fail to predict the observed extent of biological O2 undersaturation. We suggest that this shortcoming may be due either to problems with the ecosystem dynamics or problems with the vertical transport of oxygen.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
This work was supported in part by funding
from the National Aeronautic and Space Administration (NASA
NNX08AF12G) and the National Science Foundation (NSF
OPP-0823101).

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.publisher[].value
Copernicus Publications on behalf of the European Geosciences Union

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Evaluating Southern Ocean biological production in two ocean biogeochemical models on daily to seasonal timescales using satellite chlorophyll and O2 / Ar observations

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Reconstitution of amoeboid motility in vitro identifies a motor-independent mechanism for cell body retraction

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
Author Posting. © The Author(s), 2011.  This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution.  The definitive version was published in Current Biology 21 (2011): 1727-1731, doi:10.1016/j.cub.2011.08.047.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
Crawling movement in eukaryotic cells requires coordination of leading edge protrusion
with cell body retraction [1-3]. Protrusion is driven by actin polymerization along the
leading edge [4]. The mechanism of retraction is less clear; myosin contractility may be
involved in some cells [5] but is not essential in others [6-9]. In Ascaris sperm, protrusion
and retraction are powered by the major sperm protein (MSP) motility system instead of
the conventional actin apparatus [10-11]. These cells lack motor proteins [12] and so are
well-suited to explore motor-independent mechanisms of retraction. We reconstituted
protrusion and retraction simultaneously in MSP filament meshworks, called fibers, that
assemble behind plasma membrane-derived vesicles. Retraction is triggered by
depolymerization of complete filaments in the rear of the fiber [13]. The surviving
filaments reorganize to maintain their packing density. By packing fewer filaments into a
smaller volume the depolymerizing network shrinks and thereby generates sufficient
force to move an attached load. Thus, this work provides direct evidence for motorindependent
retraction in the reconstituted MSP motility system of nematode sperm. This
mechanism could also apply to actin-based cells and may explain reports of cells that
crawl even when their myosin activity is compromised.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
This work was supported by the National Institutes of Health
(R37-GM29994). N.N. was supported by an NIH grant (R01-EB002583) to Rudolf
Oldenbourg.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Reconstitution of amoeboid motility in vitro identifies a motor-independent mechanism for cell body retraction

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Satellite data processing system (SDPS) users manual V1.0

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
SDPS is a menu driven interactive program designed to facilitate the display and
output of image and line-based data sets common to telemetry, modeling and
remote sensing. This program can be used to display up to four separate raster
images and overlay line-based data such as coastlines, ship tracks and velocity
vectors. The program uses multiple windows to communicate information with
the user. At any given time, the program may have up to four image display
windows as well as auxiliary windows containing information about each image
displayed. SDPS is not a commercial program. It does not contain complete
type checking or error diagnostics which may allow the program to crash. Known
anomalies will be mentioned in the appropriate section as notes or cautions.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
Funding was provided by the Office of Naval Research
under contract Number N00014-86-K-0751; and by the National Aeronautic
and Space Administration under contract No. 957652.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.identifier.citation[].value
Caruso, M. J., & Dunn, C. (1989). Satellite data processing system (SDPS) users manual V1.0. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/6415

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Satellite data processing system (SDPS) users manual V1.0

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Comparing glacial and Holocene opal fluxes in the Pacific sector of the Southern Ocean

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
Author Posting. © American Geophysical Union, 2009.  This article is posted here by permission of American Geophysical Union for personal use, not for redistribution.  The definitive version was published in Paleoceanography 24 (2009): PA2214, doi:10.1029/2008PA001693.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
The silicic acid leakage hypothesis (SALH) predicts that during glacial periods excess silicic acid was transported from the Southern Ocean to lower latitudes, which favored diatom production over coccolithophorid production and caused a drawdown of atmospheric CO2. Downcore records of 230Th-normalized opal (biogenic silica) fluxes from 31 cores in the Pacific sector of the Southern Ocean were used to compare diatom productivity during the last glacial period to that of the Holocene and to examine the evidence for increased glacial Si export to the tropics. Average glacial opal fluxes south of the modern Antarctic Polar Front (APF) were less than during the Holocene, while average glacial opal fluxes north of the APF were greater than during the Holocene. However, the magnitude of the increase north of the APF was not enough to offset decreased fluxes to the south, resulting in a decrease in opal burial in the Pacific sector of the Southern Ocean during the last glacial period, equivalent to approximately 15 Gt opal ka−1. This is consistent with the work of Chase et al. (2003a), and satisfies the primary requirement of the SALH, assuming that the upwelled supply of Si was approximately equivalent during the Holocene and the glacial period. However, previous results from the equatorial oceans are inconsistent with the other predictions of the SALH, namely that either the Corg:CaCO3 ratio or the rate of opal burial should have increased during glacial periods. We compare the magnitudes of changes in the Southern Ocean and the tropics and suggest that Si escaping the glacial Southern Ocean must have had an alternate destination, possibly the continental margins. There is currently insufficient data to test this hypothesis, but the existence of this sink and its potential impact on glacial pCO2 remain interesting topics for future study.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
Funding for this research was provided in
part by the U.S. NSF (grant OPP02-30268). We thank the core repository at
LDEO and the Antarctic Research Facility at FSU for providing samples.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Comparing glacial and Holocene opal fluxes in the Pacific sector of the Southern Ocean

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Distribution of crustal melt bodies at the hot spot-influenced section of the Galapagos Spreading Centre from seismic reflection images

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters, 46(9), (2019):4664-4673, doi:10.1029/2019GL082201.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
Accretion of the lower crust at mid‐ocean ridges is a debated topic, with modern seismic observations pointing to a complex magmatic system that includes an axial multisill system of middle‐ and lower‐crustal melt lenses and near‐ and off‐axis melt bodies. Here we revisit the hot spot‐influenced section of the western Galápagos Spreading Centre and reprocess multichannel seismic reflection data using a wide‐angle seismic tomography model. Our new images show that the magma reservoir in the lower crust at this ridge section is intruded with partially molten melt lenses. The images also show evidence for off‐axis melt lenses, magmatic‐hydrothermal interactions and Moho reflections in this region. We conclude that the similarities between the axial crustal structure of this hot spot‐influenced mid‐ocean ridge and the multisill magmatic structure imaged at the East Pacific Rise indicate that these features are common along the global mid‐ocean ridge system where seafloor spreading is dominated by magmatic accretion.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
Seismic data used in this study are available at https://doi.org/10.1594/IEDA/314480 (Detrick & Sinton, 2014). Data processing was conducted with Emerson‐Paradigm Software package Echos licensed to Woods Hole Oceanographic Institution under Paradigm Academic Software Program. B. B. is funded by the Graduate School of the National Oceanography Centre Southampton UK. We thank two anonymous reviewers for their constructive and insightful comments that helped us in improving the manuscript and A. S. Soule for fruitful discussions.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.identifier.citation[].value
Boddupalli, B., & Canales, J. P. (2019). Distribution of crustal melt bodies at the hot spot-influenced section of the Galapagos Spreading Centre from seismic reflection images. Geophysical Research Letters, 46(9), 4664-4673.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Distribution of crustal melt bodies at the hot spot-influenced section of the Galapagos Spreading Centre from seismic reflection images

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.name
Identity of epibiotic bacteria on symbiontid euglenozoans in O2-depleted marine sediments : evidence for symbiont and host co-evolution

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description[].value
Author Posting. © The Author(s), 2010.  This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution.  The definitive version was published in The ISME Journal 5 (2011): 231–243, doi:10.1038/ismej.2010.121.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.abstract[].value
A distinct subgroup of euglenozoans, referred to as the “Symbiontida,” has been described from
oxygen-depleted and sulfidic marine environments. By definition, all members of this group
carry epibionts that are intimately associated with underlying mitochondrion-derived organelles
beneath the surface of the hosts. We have used molecular phylogenetic and ultrastructural
evidence to identify the rod-shaped epibionts of two members of this group, Calkinsia aureus
and Bihospites bacati, hand-picked from sediments from two separate oxygen-depleted, sulfidic
environments. We identify their epibionts as closely related sulfur or sulfide oxidizing members
of the Epsilon proteobacteria. The Epsilon proteobacteria generally play a significant role in
deep-sea habitats as primary colonizers, primary producers, and/or in symbiotic associations. The
epibionts likely fulfill a role in detoxifying the immediate surrounding environment for these two
different hosts. The nearly identical rod-shaped epibionts on these two symbiontid hosts provides
evidence for a co-evolutionary history between these two sets of partners. This hypothesis is
supported by congruent tree topologies inferred from 18S and 16S rDNA from the hosts and
bacterial epibionts, respectively. The eukaryotic hosts likely serve as a motile substrate that
delivers the epibionts to the ideal locations with respect to the oxic/anoxic interface whereby
their growth rates can be maximized, perhaps also allowing the host to cultivate a food source.
Because symbiontid isolates and additional SSU rDNA gene sequences from this clade have now
been recovered from many locations worldwide, the Symbiontida are likely more widespread
and diverse than presently known.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.description.sponsorship[].value
This
research was supported by a grant from NSF (MCB-0604084) to VE and JMB and by grants
from the Tula Foundation (Centre for Microbial Diversity and Evolution) and the National
Science and Engineering Research Council of Canada (NSERC 283091-09) to BSL.

# _embedded.searchResult._embedded.objects[]._embedded.indexableObject.metadata.dc.title[].value
Identity of epibiotic bacteria on symbiontid euglenozoans in O2-depleted marine sediments : evidence for symbiont and host co-evolution