<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing with OASIS Tables v3.0 20080202//EN" "journalpub-oasis3.dtd">
<article xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:oasis="http://docs.oasis-open.org/ns/oasis-exchange/table" dtd-version="3.0"><?xmltex \bartext{Workshop Reports}?>
  <front>
    <journal-meta>
<journal-id journal-id-type="publisher">SD</journal-id>
<journal-title-group>
<journal-title>Scientific Drilling</journal-title>
<abbrev-journal-title abbrev-type="publisher">SD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Sci. Dril.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1816-3459</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>

    <article-meta>
      <article-id pub-id-type="doi">10.5194/sd-20-59-2015</article-id><title-group><article-title>Advancing subsurface biosphere and paleoclimate research: ECORD–ICDP–DCO–J-DESC–MagellanPlus Workshop Series Program Report</article-title>
      </title-group><?xmltex \runningtitle{Advancing subsurface biosphere and paleoclimate research}?><?xmltex \runningauthor{H.~J.~Mills et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Mills</surname><given-names>H. J.</given-names></name>
          <email>geobiolab@gmail.com</email>
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>de Leeuw</surname><given-names>J.</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Hinrichs</surname><given-names>K.-U.</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff4">
          <name><surname>Inagaki</surname><given-names>F.</given-names></name>
          
        <ext-link>https://orcid.org/0000-0003-2887-6525</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff5">
          <name><surname>Kallmeyer</surname><given-names>J.</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-6440-1140</ext-link></contrib>
        <aff id="aff1"><label>1</label><institution>Division of Natural Sciences, University of Houston Clear Lake, Houston, TX, USA</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>NIOZ Royal Netherlands Institute for Sea Research, the Netherlands</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany</institution>
        </aff>
        <aff id="aff4"><label>4</label><institution>Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Kochi, Japan</institution>
        </aff>
        <aff id="aff5"><label>5</label><institution>GFZ German Research Centre for Geosciences, Potsdam, Germany</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">H. J. Mills (geobiolab@gmail.com)</corresp></author-notes><pub-date><day>17</day><month>December</month><year>2015</year></pub-date>
      
      <volume>20</volume>
      <issue>20</issue>
      <fpage>59</fpage><lpage>65</lpage>
      <history>
        <date date-type="received"><day>2</day><month>March</month><year>2015</year></date>
           <date date-type="rev-recd"><day>20</day><month>May</month><year>2015</year></date>
           <date date-type="accepted"><day>26</day><month>May</month><year>2015</year></date>
      </history>
      <permissions>
<license license-type="open-access">
<license-p>This work is licensed under a Creative Commons Attribution 3.0 Unported License. To view a copy of this license, visit <ext-link ext-link-type="uri" xlink:href="http://creativecommons.org/licenses/by/3.0/">http://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions><self-uri xlink:href="https://sd.copernicus.org/articles/20/59/2015/sd-20-59-2015.html">This article is available from https://sd.copernicus.org/articles/20/59/2015/sd-20-59-2015.html</self-uri>
<self-uri xlink:href="https://sd.copernicus.org/articles/20/59/2015/sd-20-59-2015.pdf">The full text article is available as a PDF file from https://sd.copernicus.org/articles/20/59/2015/sd-20-59-2015.pdf</self-uri>


      <abstract>
    <p>The proper pre-drilling preparation, on-site acquisition and post-drilling
preservation of high-quality subsurface samples are crucial to ensure
significant progress in the scientifically and societally important areas of
subsurface biosphere and paleoclimate research. Two of the four research
themes of IODP and ICDP and one of the four research areas of the Deep Carbon
Observatory (DCO) focus on the subsurface biosphere. Increasing understanding
of paleoclimate is a central goal of IODP and incorporated within the scope
of the IMPRESS program, the successor of the IMAGES program. Therefore, the
goal of our IODP–ICDP–DCO–J-DESC–MagellanPlus-sponsored workshop was to
help advance deep biosphere and paleoclimate research by identifying needed
improvements in scientific drilling planning and available technology, sample
collection and initial analysis, and long-term storage of subsurface samples
and data. Success in these areas will (a) avoid biological and other
contamination during drilling, sampling, storage and shipboard/shore-based
experiments; (b) build a repository and database of high-quality subsurface
samples for microbiological and paleoclimate research available for the
scientific community world-wide over the next decades; and (c) standardize,
as much as possible, microbiological and paleoclimate drilling, sampling and
storage workflows to allow results and data to be comparable across both
space and time. A result of this workshop is the development and suggested
implementation of new advanced methods and technologies to collect
high-quality samples and data for the deep biosphere and paleoclimate
scientific communities to optimize expected substantial progress in these
fields. The members of this workshop will enhance communication within the
scientific drilling community by crafting a handbook focused on pre-drilling,
drilling and post-drilling operations.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <title>Scientific rationale</title>
      <p>For nearly two decades, a multidisciplinary, international effort has been
conducted to describe the living subsurface biosphere. Although most research
was conducted in the marine systems with the support of the International
Ocean Discovery Program (IODP) and its predecessors (DSDP, ODP), exploration
of the terrestrial subsurface biosphere through the International Continental
Scientific Drilling Program (ICDP) has substantially increased in recent
years. Microbial communities have been characterized in numerous sediment
types representing a multitude of geologic ages, geochemical conditions, and
geophysical constraints (IODP – Parkes et al., 2005; Schippers et al., 2005;
Morono et al., 2011; Mills et al., 2012a; ICDP – Heim, 2011; Colwell and
D'Hondt, 2013; Lau et al., 2014). As IODP embarks on a new decade, the time
is right to coalesce the strengths and address the weaknesses from previous
studies to re-develop and implement a plan to improve and standardize
subsurface biosphere exploration. Due to the more individual or small group
nature of drilling projects within ICDP, the European Consortium for Ocean
Research Drilling (ECORD) and the Deep Carbon Observatory (DCO), the need for
standardized biological sampling, processing and analysis becomes even more
important.</p>
      <p>The demand for biological samples has and will continue to increase as a
result of the larger commitment to biology in the DCO and the new science
plans of both IODP (2011) and ICDP (2014). The biological scientific goals
within these groups focus on (a) the origin, composition and global
significance of subsurface communities, (b) the scarcity of nutrients and
energy and the limits of life in the subsurface, (c) the impact of
environmental change on subsurface ecosystems and biodiversity and (d) the
impact of subsurface communities on paleo-environmental and paleoclimate
proxies, minerals and hydrocarbon reservoirs. Without the ability to compare
results of multiple expeditions and access to properly acquired samples,
these goals cannot be achieved. The biosphere community is aware of this
challenge and understands the need for standardizing sample collection
procedures, initial analysis protocols and long-term storage techniques
(Orcutt et al., 2013; Kieft et al., 2015). We recognize that education of the
broader drilling community is also required as many efforts related to
biological sampling and characterization are seen as disruptive to normal
core flow and description.</p>
      <p>A unique challenge for the deep biosphere community has been fully
communicating our requirements and resources to the drilling community.
Biologists understand the need for collaborative data sets that characterize
the chemical, physical and geological parameters of the sample. In many ways
the drilling community views the biologist as a sink for drilling data; we
use the data others produce but contribute little information in return to
overall sample analysis. However, biologists can be a valuable source of
subsurface data when consulted during core description and preservation
efforts. By including biologically relevant chemical, physical and geological
parameters within standard data sets, biologists can determine active
microbial processes that may have altered or continue to alter parameters
measured by other groups. The presence of active biological processes within
retrieved samples can also have detrimental effects on legacy cores (Mills et
al., 2012b). It is time for other disciplines to engage with biologists and
biogeochemists in discussions about the effects of a living biosphere on the
subsurface environment. For example, the application of proxies in
paleoclimatology has become crucially important to reconstruct
paleo-environmental settings and paleoclimate change. Since these proxies are
based on organic compounds (biomarkers) and abundances and/or speciation of
inorganic constituents, including stable isotope compositions, we must
understand how these geochemical entities are affected by the microbial
communities within the subsurface biosphere.</p>
      <p>To further advance biosphere exploration in the scientific drilling
community, a multidisciplinary team, including a molecular biologist, an
ecologist, geochemists, and geologists, from nine countries assembled in
Seoul, South Korea. The group represented leaders in the field of subsurface
biosphere exploration in both the marine and terrestrial systems and
possessed knowledge of prior similar workshops and initiatives to standardize
subsurface biosphere techniques. The motivation for this workshop emerged
during presentations and discussions at the Chikyu<inline-formula><mml:math display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>10 meeting (Tokyo,
21–23 April 2013) and represents a successful extension from that meeting.
Initial plans for this workshop exclusively focused on IODP-related research,
but during the ICDP Science Conference in Potsdam, Germany (11–14 November
2013), it became clear that subsurface biosphere exploration faces the same
challenges in both the marine and terrestrial realm. Therefore, the conveners
broadened the workshop to cover additional programs including ICDP, DCO, and
IMPRESS. Together these groups, and new ones to follow, have the potential to
make a significant impact in subsurface biosphere research, the fastest
developing field within the drilling community. Results from this workshop
will be crucial in the development of the procedures required to accomplish
the goals set forth in the new science plans and promoted through new
initiatives.</p>
      <p>One of our main goals in organizing this workshop was to advance the efforts
of previous workshops. The 7th IODP Scientific Technology Panel that met on
28–30 July 2008 in Edmonton, Canada, expressed the need to standardize the
biological sampling process and improve mechanisms for completing biological
research within IODP. While procedural and policy changes have been implemented as a
result of this 2008 meeting, several key challenges remained insufficiently
addressed, including standard sub-sampling techniques for frozen samples,
time- and redox-sensitive measurements, and submission of microbiology data
and samples. ICDP first addressed subsurface biosphere research at their 2005
Science conference (Horsfield et al., 2007). In Potsdam 2009, an
international workshop on the integration of deep biosphere research into
ICDP listed potential drilling targets as well as technical and logistical
prerequisites (Mangelsdorf and Kallmeyer, 2010). The growing strengths of DCO and IMPRESS provide additional
momentum to subsurface biosphere exploration while presenting new and diverse
challenges that must also be considered. Incorporating individuals present at
these and other past meetings as well as those active within these different
research communities was viewed as vital to the success of our workshop. In
addition, individuals knowledgeable of new techniques and technologies were
invited to address needs realized since the conclusion of the previous
meetings. An open format for the workshop provided time for these groups to
address past, present and future needs of the growing subsurface biosphere
community.</p>
</sec>
<sec id="Ch1.S2">
  <title>The workshop</title>
      <p>The Advancing Subsurface Biosphere and Paleoclimate Research workshop took
place in Seoul, South Korea, on 21–23 August 2014, directly before the
International Society for Microbial Ecology (ISME) meeting, also in Seoul.
Twenty-eight junior and senior scientists with experience in the
geomicrobiological and biogeochemical components of the IODP, ICDP, DCO and
IMPRESS (the successor of IMAGES) programs representative of the global
community of subsurface microbiology, participated in this workshop and, for
the first time, were able to speak with one solid voice. The idea for this
workshop was developed during the Chikyu<inline-formula><mml:math display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>10 workshop in April 2013, but had
roots in many workshops, meetings and discussions over the last several
years. Since the Chikyu<inline-formula><mml:math display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>10 workshop, the idea to have a community
discussion on standard protocols for microbiological drilling, sample
handling and long-term sample storage developed rapidly with the interest and
support of ICDP and DCO. Timing was important for these discussions since
IODP, ICDP and DCO are at the beginning of new 10- and 5-year science plans
with large geomicrobiological and paleoclimate components.</p>
      <p>The overall aim of our workshop was to develop shared sampling and long-term
storage strategies partly based on already existing white and scientific
papers and to implement these strategies through standardized protocols for
all drilling platforms, i.e., “traditional drilling” with the JOIDES
Resolution, Chikyu and MSP/ICDP platforms. A decision was made during the
workshop planning to expand the goal for standardization to much less
expensive seabed drilling and long piston core operations from additional
research vessels.</p>
      <p>Initial workshop discussions were dedicated to providing background
information on the current state of deep life research and proxy-based
paleoclimatology within long-term scientific plans for IODP, ICDP, DCO and
IMPRESS. In addition, presentations on subsurface microbiology and
proxy-based paleoclimatology highlighted the benefits of conducting
geomicrobiological and paleoclimate research by acquiring high-quality
microbiological samples, even when the expedition may focus on other
scientific disciplines. At the end of day 1 and the start of day 2, most
participants gave short 10–15 min talks describing their specific research
activities. Presentations emphasized their needs and experience with key
aspects of pre-drilling, drilling, onboard sample handling, in-repository
sample handling and long-term storage. Topics included sample frequency,
contamination checks, core flow, geochemical measurements, cell enumeration,
sample archives, data submission, staffing needs, education and
collaborations with other scientific disciplines. Discussions that followed
the presentations identified an apparent communication gap between the
scientific drilling community and deep biosphere researchers that is
inhibiting the progress of the entire community. The lack of communication
was said to affect each stage of exploration from the pre-drilling planning
stages through the drilling process to the post-drilling analysis.
Misconceptions included the technical requirements for biological sampling,
the frequency and targets for biological research, and sample preservation
and storage. These issues are discussed below.</p>
</sec>
<sec id="Ch1.S3">
  <title>Enhance communications and expectations</title>
      <p>Workshop participants suggested a three-level approach to improve the
communication and expectation of biological research for upcoming drilling
operations to help develop and implement a feasible set of standardized
protocols for microbiological drilling, sample handling and long-term
storage. Where possible, we took into account the diversity of drilling
operations, i.e., “traditional” drilling, seabed drilling and long piston
coring. While the expectations listed below are more specific to IODP, a
similar level-based structure with program-specific expectation should be
discussed and determined with these expectations acting as the catalyst for
future discussion. The levels suggested are as follows.</p>
<sec id="Ch1.S3.SS1">
  <title>Level 1: expeditions with few to no geomicrobiological
components</title>
      <p>Expectation: a technician trained in microbiology sampling will be on board.
There will be low-frequency core sampling with no onboard contamination
checks. Proposals listing this level for biology will not receive support
from the biosphere community to improve rank when evaluated by the IODP
proposal evaluation panel. Support will be provided to determine ways to
enhance the biological components within the drilling plan and to demonstrate
how these enhancements will help increase the scientific output of the
expedition.</p>
</sec>
<sec id="Ch1.S3.SS2">
  <title>Level 2: expeditions with a modest geomicrobiological component</title>
      <p>Expectation: at least one of the sailing scientists will be a microbiologist.
A technician trained in microbiology sampling will also be on board. There
will be more frequent core sampling with onboard contamination checks
completed and limited supporting geochemistry compared to a Level 1
expedition. Proposals listed at this level will receive some support from the
biosphere community to improve rank when evaluated by the IODP proposal
evaluation panel. Support will be provided to determine ways to further
enhance the biological components within the drilling plan and to demonstrate
how these enhancements will help increase the scientific output of the
expedition.</p>
</sec>
<sec id="Ch1.S3.SS3">
  <title>Level 3: expeditions with a significant or predominant
geomicrobiological component</title>
      <p>Expectation: two sailing scientists should be microbiologists. A technician
trained in microbiology sampling will also be on board. There will be
frequent core sampling with full onboard contamination checks, onboard cell
counting, extended geochemical analysis and onboard CAS freezing facilities.
For information on CAS freezing, please see Morono et al. (2015). Proposals
listed at this level will receive full support from the biosphere community
to improve rank when evaluated by the IODP proposal evaluation panel.
Expedition advertisements and promotion within the biosphere community will
ensure adequate pre-expedition planning, and onshore and offshore research,
and post-expedition data and sample preservation will be made possible.</p>
      <p>These levels are meant to promote proper communication of scientific
expectations and requirements between expedition leaders and participants, an
area that is currently plagued with misconceptions from both sides. Early
communication during the proposal-writing phase will help guide sample
requests and operational expectations of the chief scientists, biologists and
drilling operators. The level approach was further refined through three
subgroups organized based on an expedition planning and operation timeline.
The groups were focused on predrilling and drilling,
onboard sample
processing and post-cruise legacy samples and data. Greater detail for these
levels will be provided in the handbook being written by workshop
participants. Details describing the handbook are provided below in Sect. 5.</p>
</sec>
</sec>
<sec id="Ch1.S4">
  <title>Legal requirements for microbiological sampling within the
economic exclusive zone (EEZ) through scientific drilling</title>
      <p>During the workshop, we discussed possible legal requirement issues for
microbiological samples regarding the Nagoya Protocol on Access and
Benefit-Sharing (ABS, <uri>http://www.cbd.int/abs/</uri>). Briefly, the Nagoya
Protocol on Access to Genetic Resources and the Fair and Equitable sharing of
Benefits Arising from their Utilization to the Convention on Biological
Diversity (CBD) is an international agreement at the government level, which
aims at sharing the benefits arising from the utilization of genetic
resources in a fair and equitable way. The Nagoya Protocol, created for
greater legal certainty and transparency for both providers and users of
genetic resources, was enacted on 12 October 2014, with the support of 57
countries. The Nagoya Protocol specified obligations to support compliance
with the domestic legislation or regulatory requirements of the contracting
party providing genetic resources, and contractual obligations reflected in
mutually agreed terms. The contracting parties of the Nagoya Protocol are to
take measures to ensure genetic resources utilized within their jurisdiction
have been accessed in accordance with prior informed consent (PIC), and that
mutually agreed terms (MAT) have been established, as required by another
contracting party.</p>
      <p>The United Nations Convention on the Law of the Sea (UNCLOS) establishes a
plan of sovereignty over parts of the seas. The resources of the seas within
state jurisdiction covered by UNCLOS are then accessed and shared according
to the procedure established by the CBD and the Nagoya Protocol. The
interaction of UNCLOS and the CBD means that the access regime of the CBD
extends to all genetic resources (both terrestrial and marine) within the
coastal state's jurisdiction. In this regard, the legal regulation is highly
relevant to the deep biosphere-related sampling through IODP and other
academic activities in the economic exclusive zone (EEZ). For example, during
an IODP drilling project in the EEZ of a certain country, the samples used
for biology are considered genetic resources belonging to that country, and
should be taken following the regulations of the domestic law through the PIC
and MAT. The complicacy of the Nagoya Protocol is that not all the party
countries have already established the regulations and systems. Moreover,
implementation of the Nagoya Protol in national legal systems has led to very
diverse regulations that are different in each country. This might make
microbiological sampling with IODP difficult when the drilling sites are
located within the EEZ of a nation. ICDP drilling operations are affected as
well.</p>
      <p>Given the situation, the workshop participants recognized that it is
important to share the knowledge among the IODP community and discuss
possible issues that should be addressed properly before the drilling
expedition at the IODP implementation organization level. Other
organizations will have similar difficulties with the Nagoya Protocol and
should also establish a working protocol to remain in compliance while not
interfering with the biological exploration of the subsurface.</p>
</sec>
<sec id="Ch1.S5">
  <title>DEEP BIO Handbook</title>
      <p>By the end of the workshop, a full handbook for microbiological and
proxy-based paleoclimate drilling operations was determined to be both
necessary and possible. The Deep Earth Exploration for Paleoclimate and
Biosphere Investigation and Observation (DEEP BIO) Handbook is meant to
promote proper communication of scientific expectations and requirements
between expedition leaders and participants, an area that is currently
plagued with misconceptions from both sides. As a result of discussions
during the workshop, participants and selected experts were asked to assist
in the writing of the handbook's four main sections: (1) Pre-drilling
preparations and planning; (2) On-site operations; (3) Post-drilling
processing and storage; and (4) Future Development (Table 1). Opportunities
for community involvement in the writing process are discussed below.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><caption><p>Sections and topics to be included in the DEEP BIO Handbook.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="2">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:thead>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Handbook section</oasis:entry>  
         <oasis:entry colname="col2">Initial topics for discussion</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Pre-drilling preparations and planning</oasis:entry>  
         <oasis:entry colname="col2">Proposal writing involvement</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Sample request writing and expectation</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Procedure/methods/protocol preparations</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">On-site operations</oasis:entry>  
         <oasis:entry colname="col2">Contamination check technology and application</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Personnel needs</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Efficient and sterile sampling procedure</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">On-site analysis in support of biological objectives</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Post-drilling processing and storage</oasis:entry>  
         <oasis:entry colname="col2">Storage requirements to maximize sample viability</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Repository requests and sample availability</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Future development</oasis:entry>  
         <oasis:entry colname="col2">Technologies for drilling, sampling and storage</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">On-site technique developments</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Advances in data management</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <p>Workshop participants, organized in breakout groups, identified multiple key
points within each handbook section to help describe the needs of the
biosphere community and where the biosphere community should be more
proactive and involved. The early stages of proposal writing and planning
were seen as a key time point for increased input from the biosphere
community. Early activity in the proposal writing process will promote the
inclusion of specific biological objectives within the main science plan and
help alleviate misconceptions about the operational demand of biological
sampling. Thus, sample requests, as well as drilling procedures, methods and
protocols, should be discussed among all proponents in order to include a
biological perspective of the overall goals of the drilling project. To
accomplish biological inclusion in the proposal writing stage, monitoring of
submitted proposals, involvement on planning committees and communication
within the biosphere community are required.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1"><caption><p>Standardization of cell counting techniques. The
determination of cell abundance is a basic measurement common to most
subsurface microbial community descriptions. An automated flow cytometer
system can be used to determine cell abundances with high reproducibility
and at a high sample rate (Morono et al., 2008). This method can be used
repeatedly at multiple drill sites to reduce human errors and provide better
connectivity between projects. (Figure is being used with permission from
Yuki Morono; Morono et al., 2013.)</p></caption>
        <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://sd.copernicus.org/articles/20/59/2015/sd-20-59-2015-f01.pdf"/>

      </fig>

      <p>The section describing on-site operations will focus on personnel needs,
quality assurance and quality control protocols including the use of
contamination checks, standardizing sampling procedures and requirements to
increase efficiency and reduce core disruption, and on-site analysis
protocols to maximize post-drilling research potential. Discussions were
stimulated by recent work by Lloyd et al. (2013) that illustrated how
different molecular methods used in multiple laboratories produced
inconsistent results and thus suggested standardizing protocols to help link
data sets. A standardized, high-throughput cell counting method, presented by
Yuki Morono (Fig. 1), will be included in the handbook as one of the
recommendations for on-site analysis (Morono et al., 2013). Additional
methods will be considered with the understanding that the handbook should be
updated as technologies advance.</p>
      <p>Post-drilling preservation of both samples and data will be detailed in the
third section. This will include recommendations as to how these resources
can be made more accessible to a broader community. Additional mechanisms
for sample storage and data archiving will be examined. Shifts in the
metabolically active microbial community structure have been previously
observed in cores under standard IODP storage conditions, suggesting
alterations of the physical and chemical characteristics (Mills et al.,
2012b). The advanced preservation techniques and cryo-sampling procedures
currently being used in the Kochi Core Repository DeepBIOS program led by
Nan Xiao will described. Recommendations will be made to expand this
program.</p>
      <p>In the Future Development section, drilling technologies such as gel coring
and large diameter side-wall coring will be highlighted to increase
community discussion on sampling needs. This section will be used to help
build new initiatives and discussions. It is our goal that new innovations
will help advance biosphere exploration beyond the current challenges with
the understanding that more challenges will be realized. Techniques and
technologies in this section may be moved to other sections as they become
more widely used.</p>
      <p>The handbook will be initially tested during IODP expedition planning,
drilling and post-expedition operations to determine feasibility and then
used to train technicians and scientists. Protocols and procedures specific
to different ocean and terrestrial drilling platforms, as well as within the
repositories, will be included. Community involvement is welcome during the
writing of this handbook. If you would like to contribute and be involved,
please contact Heath Mills at geobiolab@gmail.com. The handbook will be
designed to accommodate regular updates so that it may continue to guide
subsurface exploration in the future.</p>
      <p>The workshop successfully brought together an energetic and knowledgeable
group that worked efficiently toward our goal of improving subsurface
biosphere exploration. The key focal point discussed for moving forward was
improving communication within the drilling community to improve overall
understanding of the requirements and expectations for biosphere exploration.
Deliverables from this workshop include an EOS newsletter article (Mills et
al., 2014), this paper and a handbook to be written by workshop participants
with community input.</p>
</sec>

      
      </body>
    <back><ack><title>Acknowledgements</title><p>We thank ECORD, ICDP, DCO, J-DESC and MagellanPlus for providing financial
support to the workshop. We also thank N. Xiao for presenting the issue of
microbiological sampling within the economic exclusive zone through
scientific drilling. In addition, we would like to acknowledge the logistical
support and overall assistance provided by J.-H. Lee.<?xmltex \hack{\newline}?><?xmltex \hack{\newline}?> Edited by: T. Wiersberg<?xmltex \hack{\newline}?> Reviewed by:
B. Horsfield and one anonymous referee</p></ack><ref-list>
    <title>References</title>

      <ref id="bib1.bib1"><label>1</label><mixed-citation>Colwell, F. S. and D'Hondt, S.: Nature and Exteme of the Deep
Biosphere, in: Carbon in Earth. Mineralogical Society of America and
Geochemical Society, Reviews in Mineralogy and Geochemistry, edited by:
Hazen, R. H., Jones, A. P., and Baross, J. A., 75, 547–566,
<ext-link xlink:href="http://dx.doi.org/10.2138/rmg.2013.75.17" ext-link-type="DOI">10.2138/rmg.2013.75.17</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib2"><label>2</label><mixed-citation>
Heim, C.: Terrestrial deep biosphere, in: Encyclopedia of geobiology,
edited by: Reitner, J. and Thiel, V., Dordrecht, The Netherlands, Springer
ScienceCBusiness Media B.V., 871–876, 2011.</mixed-citation></ref>
      <ref id="bib1.bib3"><label>3</label><mixed-citation>
Horsfield, B., Kieft, T., Amann, H., Franks, S., Kallmeyer, S., Mangelsdorf,
K., Parkes, J., Wagner, W., Wilkes, H., and Zink, K.-G.: The GeoBiosphere,
edited by: Harms, U., Koeberl, C., and Zoback, M. D., Continental Scientific
Drilling: A Decade of Progress and Challenges for the Future,
Berlin-Heidelberg (Springer), 163–211, 2007.</mixed-citation></ref>
      <ref id="bib1.bib4"><label>4</label><mixed-citation>
ICDP: Unraveling the complexities of planet earth: science plan for
2014–2019, edited by: Horsfield, B., Knebel, C., Ludden, J., and Hyndman,
R, International Continental Scientific Drilling Program, Potsdam, Germany, 2014.</mixed-citation></ref>
      <ref id="bib1.bib5"><label>5</label><mixed-citation>
IODP: Science plan for 2013–2023: Illuminating earth's past, present
and future, Integrated Ocean Drilling Program Management International,
Washington DC, 2011.</mixed-citation></ref>
      <ref id="bib1.bib6"><label>6</label><mixed-citation>Kieft, T. L., Onstott, T. C., Ahonen, L., Aloisi, V., Colwell, F. S., Engelen, B.,
Fendrihan, S., Gaidos, E., Harms, U., Head, I., Kallmeyer, J., Kiel Reese, B.,
Lin, L.-H., Long, P. E., Moser, D. P., Mills, H., Sar, P., Schulze-Makuch, D.,
Stan-Lotter, H., Wagner, D., Wang, P.-L., Westall, F., and Wilkins, M. J.:
Workshop to develop deep-life continental scientific drilling projects, Sci. Dril., 19, 43–53, <ext-link xlink:href="http://dx.doi.org/10.5194/sd-19-43-2015" ext-link-type="DOI">10.5194/sd-19-43-2015</ext-link>,
2015.</mixed-citation></ref>
      <ref id="bib1.bib7"><label>7</label><mixed-citation>Lau, M. C. Y., Cameron, C., Magnabosco, C., Brown, C. T., Schilkey, F., Grim,
S., Hendrickson, S., Pullin, M., Sherwood Lollar, B., van Heerden, E., Kieft, T.
L., and Onstott, T. C.: Phylogeny and phylogeography of functional
genes shared among seven terrestrial subsurface metagenomes reveal N-cycling
and microbial evolutionary relationships, Front. Microbiol., 5, 531,
<ext-link xlink:href="http://dx.doi.org/10.3389/fmicb.2014.00531" ext-link-type="DOI">10.3389/fmicb.2014.00531</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib8"><label>8</label><mixed-citation>
Lloyd, K. G., May, M. K., Kevorkian, R. T., and Steen, A. D.: Meta-analysis
of quantification methods shows that archaea and bacteria have similar
abundances in the subseafloor, Appl. Environ. Microbiol., 79, 7790–7799, 2013.</mixed-citation></ref>
      <ref id="bib1.bib9"><label>9</label><mixed-citation>Mangelsdorf, K. and Kallmeyer, J.: Integration of Deep Biosphere Research into
the International Continental Scientific Drilling Program, Sci. Dril.,
10, 46–55, <ext-link xlink:href="http://dx.doi.org/10.5194/sd-10-46-2010" ext-link-type="DOI">10.5194/sd-10-46-2010</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib10"><label>10</label><mixed-citation>Mills, H. J., Reese, B. K., Shepard, A. K., Riedinger, N., Murano, Y., and
Inagaki, F.: Characterization of the metabolically active bacterial
populations in subseafloor Nankai Trough sediments above, within and below
the sulfate-methane transition zone, Front. Microbiol., 3, 113, <ext-link xlink:href="http://dx.doi.org/10.3389/fmicb.2012.00113" ext-link-type="DOI">10.3389/fmicb.2012.00113</ext-link>, 2012a.</mixed-citation></ref>
      <ref id="bib1.bib11"><label>11</label><mixed-citation>Mills, H. J., Reese, B. K., and St. Peter, C.: Characterization
of microbial population shifts during sample storage, Front. Microbiol.,
3, 49, <ext-link xlink:href="http://dx.doi.org/10.3389/fmicb.2012.00049" ext-link-type="DOI">10.3389/fmicb.2012.00049</ext-link>, 2012b.</mixed-citation></ref>
      <ref id="bib1.bib12"><label>12</label><mixed-citation>
Mills, H. J., de Leeuw, J., Kinrichs, K. U., Inagaki, F., and Kallmeyer, J.:
Advancing Sub-Surface Biosphere and Paleoclimate Research MagellanPlus
Workshop – 21–23 August 2014, Seoul (South Korea), ECORD Newsletter, 23, p. 21, 2014.</mixed-citation></ref>
      <ref id="bib1.bib13"><label>13</label><mixed-citation>
Morono, Y., Terada, T., Masui, N., and Inagaki, F.: Improved and automated cell
count system for rapid enumeration of microbial cells in the deep subsurface,
Geochem. Cosmochim. Ac., 72, A651–A651, 2008.</mixed-citation></ref>
      <ref id="bib1.bib14"><label>14</label><mixed-citation>
Morono, Y., Terada, T., Nishizawa, M., Ito, M., Hillion, F., Takahata, N.,
Sano, Y., and Inagaki, F.: Carbon and nitrogen assimilation in deep
subseafloor microbial cells, P. Natl. Acad. Sci. USA, 108, 18295–18300, 2011.</mixed-citation></ref>
      <ref id="bib1.bib15"><label>15</label><mixed-citation>Morono, Y., Terada, T., Kallmeyer, J., and Inagaki, F.: An improved cell
separation technique for marine subsurface sediments: applications for
high-throughput analysis using flow cytometry and cell sorting, Environ.
Microbiol., 15, 2841–2849, <ext-link xlink:href="http://dx.doi.org/10.1111/1462-2920.12153" ext-link-type="DOI">10.1111/1462-2920.12153</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib16"><label>16</label><mixed-citation>Morono, Y., Terada, T., Yamamoto, Y., Xiao, N., Hirose, T., Sugeno, M.,
Ohwada, N., and Inagaki, F.: Intact preservation of environmental samples by
freezing under an alternating magnetic field, Environ. Microbio. Rep.,
7, 243–251, <ext-link xlink:href="http://dx.doi.org/10.1111/1758-2229.12238" ext-link-type="DOI">10.1111/1758-2229.12238</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib17"><label>17</label><mixed-citation>Orcutt, B. N., LaRowe, D. E., Biddle, J. E., Colwell, F. S., Glazer, B. T.,
Reese, B. K., Kirkpatrick, J. B., Lapham, L. L., Mills, H. J., Sylvan, J. B., Wankel, S.
D., and Wheat, C. G.: Microbial activity in the marine deep biosphere:
progress and prospects, Front. Microbiol., 4, 1–14, <ext-link xlink:href="http://dx.doi.org/10.3389/fmicb.2013.00189" ext-link-type="DOI">10.3389/fmicb.2013.00189</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib18"><label>18</label><mixed-citation>Parkes, R. J., Webster, G., Cragg, B. A., Weightman, A. J., Newberry, C. J.,
Ferdelman, T. G., Kallmeyer, J., Jørgensen, B. B., Aiello, I. W., and Fry, J. C.:
Deep sub-seafloor prokaryotes stimulated at interfaces over geologic time,
Nature, 436, 390–394, 2005.
 </mixed-citation></ref><?xmltex \hack{\newpage}?>
      <ref id="bib1.bib19"><label>19</label><mixed-citation>
Schippers, A., Neretin, L. N., Kallmeyer, J., Ferdelman, T. G., Cragg, B. A.,
Parkes, R. J., and Jørgensen, B. B.: Prokaryotic cells of the deep
sub-seafloor biosphere identified as living bacteria, Nature, 433, 861–864,
2005.</mixed-citation></ref>

  </ref-list><app-group content-type="float"><app><title/>

    </app></app-group></back>
    <!--<article-title-html>Advancing subsurface biosphere and paleoclimate research: ECORD–ICDP–DCO–J-DESC–MagellanPlus Workshop Series Program Report</article-title-html>
<abstract-html><h6 xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg">Abstract. </h6><p xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" class="p">The proper pre-drilling preparation, on-site acquisition and post-drilling
preservation of high-quality subsurface samples are crucial to ensure
significant progress in the scientifically and societally important areas of
subsurface biosphere and paleoclimate research. Two of the four research
themes of IODP and ICDP and one of the four research areas of the Deep Carbon
Observatory (DCO) focus on the subsurface biosphere. Increasing understanding
of paleoclimate is a central goal of IODP and incorporated within the scope
of the IMPRESS program, the successor of the IMAGES program. Therefore, the
goal of our IODP–ICDP–DCO–J-DESC–MagellanPlus-sponsored workshop was to
help advance deep biosphere and paleoclimate research by identifying needed
improvements in scientific drilling planning and available technology, sample
collection and initial analysis, and long-term storage of subsurface samples
and data. Success in these areas will (a) avoid biological and other
contamination during drilling, sampling, storage and shipboard/shore-based
experiments; (b) build a repository and database of high-quality subsurface
samples for microbiological and paleoclimate research available for the
scientific community world-wide over the next decades; and (c) standardize,
as much as possible, microbiological and paleoclimate drilling, sampling and
storage workflows to allow results and data to be comparable across both
space and time. A result of this workshop is the development and suggested
implementation of new advanced methods and technologies to collect
high-quality samples and data for the deep biosphere and paleoclimate
scientific communities to optimize expected substantial progress in these
fields. The members of this workshop will enhance communication within the
scientific drilling community by crafting a handbook focused on pre-drilling,
drilling and post-drilling operations.</p></abstract-html>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
Colwell, F. S. and D'Hondt, S.: Nature and Exteme of the Deep
Biosphere, in: Carbon in Earth. Mineralogical Society of America and
Geochemical Society, Reviews in Mineralogy and Geochemistry, edited by:
Hazen, R. H., Jones, A. P., and Baross, J. A., 75, 547–566,
<a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.2138/rmg.2013.75.17" title="" class="ref">10.2138/rmg.2013.75.17</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
Heim, C.: Terrestrial deep biosphere, in: Encyclopedia of geobiology,
edited by: Reitner, J. and Thiel, V., Dordrecht, The Netherlands, Springer
ScienceCBusiness Media B.V., 871–876, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib3"><label>3</label><mixed-citation>
Horsfield, B., Kieft, T., Amann, H., Franks, S., Kallmeyer, S., Mangelsdorf,
K., Parkes, J., Wagner, W., Wilkes, H., and Zink, K.-G.: The GeoBiosphere,
edited by: Harms, U., Koeberl, C., and Zoback, M. D., Continental Scientific
Drilling: A Decade of Progress and Challenges for the Future,
Berlin-Heidelberg (Springer), 163–211, 2007.
</mixed-citation></ref-html>
<ref-html id="bib1.bib4"><label>4</label><mixed-citation>
ICDP: Unraveling the complexities of planet earth: science plan for
2014–2019, edited by: Horsfield, B., Knebel, C., Ludden, J., and Hyndman,
R, International Continental Scientific Drilling Program, Potsdam, Germany, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib5"><label>5</label><mixed-citation>
IODP: Science plan for 2013–2023: Illuminating earth's past, present
and future, Integrated Ocean Drilling Program Management International,
Washington DC, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib6"><label>6</label><mixed-citation>
Kieft, T. L., Onstott, T. C., Ahonen, L., Aloisi, V., Colwell, F. S., Engelen, B.,
Fendrihan, S., Gaidos, E., Harms, U., Head, I., Kallmeyer, J., Kiel Reese, B.,
Lin, L.-H., Long, P. E., Moser, D. P., Mills, H., Sar, P., Schulze-Makuch, D.,
Stan-Lotter, H., Wagner, D., Wang, P.-L., Westall, F., and Wilkins, M. J.:
Workshop to develop deep-life continental scientific drilling projects, Sci. Dril., 19, 43–53, <a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.5194/sd-19-43-2015" title="" class="ref">10.5194/sd-19-43-2015</a>,
2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib7"><label>7</label><mixed-citation>
Lau, M. C. Y., Cameron, C., Magnabosco, C., Brown, C. T., Schilkey, F., Grim,
S., Hendrickson, S., Pullin, M., Sherwood Lollar, B., van Heerden, E., Kieft, T.
L., and Onstott, T. C.: Phylogeny and phylogeography of functional
genes shared among seven terrestrial subsurface metagenomes reveal N-cycling
and microbial evolutionary relationships, Front. Microbiol., 5, 531,
<a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.3389/fmicb.2014.00531" title="" class="ref">10.3389/fmicb.2014.00531</a>, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib8"><label>8</label><mixed-citation>
Lloyd, K. G., May, M. K., Kevorkian, R. T., and Steen, A. D.: Meta-analysis
of quantification methods shows that archaea and bacteria have similar
abundances in the subseafloor, Appl. Environ. Microbiol., 79, 7790–7799, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib9"><label>9</label><mixed-citation>
Mangelsdorf, K. and Kallmeyer, J.: Integration of Deep Biosphere Research into
the International Continental Scientific Drilling Program, Sci. Dril.,
10, 46–55, <a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.5194/sd-10-46-2010" title="" class="ref">10.5194/sd-10-46-2010</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib10"><label>10</label><mixed-citation>
Mills, H. J., Reese, B. K., Shepard, A. K., Riedinger, N., Murano, Y., and
Inagaki, F.: Characterization of the metabolically active bacterial
populations in subseafloor Nankai Trough sediments above, within and below
the sulfate-methane transition zone, Front. Microbiol., 3, 113, <a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.3389/fmicb.2012.00113" title="" class="ref">10.3389/fmicb.2012.00113</a>, 2012a.
</mixed-citation></ref-html>
<ref-html id="bib1.bib11"><label>11</label><mixed-citation>
Mills, H. J., Reese, B. K., and St. Peter, C.: Characterization
of microbial population shifts during sample storage, Front. Microbiol.,
3, 49, <a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.3389/fmicb.2012.00049" title="" class="ref">10.3389/fmicb.2012.00049</a>, 2012b.
</mixed-citation></ref-html>
<ref-html id="bib1.bib12"><label>12</label><mixed-citation>
Mills, H. J., de Leeuw, J., Kinrichs, K. U., Inagaki, F., and Kallmeyer, J.:
Advancing Sub-Surface Biosphere and Paleoclimate Research MagellanPlus
Workshop – 21–23 August 2014, Seoul (South Korea), ECORD Newsletter, 23, p. 21, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib13"><label>13</label><mixed-citation>
Morono, Y., Terada, T., Masui, N., and Inagaki, F.: Improved and automated cell
count system for rapid enumeration of microbial cells in the deep subsurface,
Geochem. Cosmochim. Ac., 72, A651–A651, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib14"><label>14</label><mixed-citation>
Morono, Y., Terada, T., Nishizawa, M., Ito, M., Hillion, F., Takahata, N.,
Sano, Y., and Inagaki, F.: Carbon and nitrogen assimilation in deep
subseafloor microbial cells, P. Natl. Acad. Sci. USA, 108, 18295–18300, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib15"><label>15</label><mixed-citation>
Morono, Y., Terada, T., Kallmeyer, J., and Inagaki, F.: An improved cell
separation technique for marine subsurface sediments: applications for
high-throughput analysis using flow cytometry and cell sorting, Environ.
Microbiol., 15, 2841–2849, <a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.1111/1462-2920.12153" title="" class="ref">10.1111/1462-2920.12153</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib16"><label>16</label><mixed-citation>
Morono, Y., Terada, T., Yamamoto, Y., Xiao, N., Hirose, T., Sugeno, M.,
Ohwada, N., and Inagaki, F.: Intact preservation of environmental samples by
freezing under an alternating magnetic field, Environ. Microbio. Rep.,
7, 243–251, <a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.1111/1758-2229.12238" title="" class="ref">10.1111/1758-2229.12238</a>, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib17"><label>17</label><mixed-citation>
Orcutt, B. N., LaRowe, D. E., Biddle, J. E., Colwell, F. S., Glazer, B. T.,
Reese, B. K., Kirkpatrick, J. B., Lapham, L. L., Mills, H. J., Sylvan, J. B., Wankel, S.
D., and Wheat, C. G.: Microbial activity in the marine deep biosphere:
progress and prospects, Front. Microbiol., 4, 1–14, <a xmlns="http://www.w3.org/1999/xhtml" xmlns:m="http://www.w3.org/1998/Math/MathML" xmlns:svg="http://www.w3.org/2000/svg" href="http://dx.doi.org/10.3389/fmicb.2013.00189" title="" class="ref">10.3389/fmicb.2013.00189</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib18"><label>18</label><mixed-citation>
Parkes, R. J., Webster, G., Cragg, B. A., Weightman, A. J., Newberry, C. J.,
Ferdelman, T. G., Kallmeyer, J., Jørgensen, B. B., Aiello, I. W., and Fry, J. C.:
Deep sub-seafloor prokaryotes stimulated at interfaces over geologic time,
Nature, 436, 390–394, 2005.

</mixed-citation></ref-html>
<ref-html id="bib1.bib19"><label>19</label><mixed-citation>
Schippers, A., Neretin, L. N., Kallmeyer, J., Ferdelman, T. G., Cragg, B. A.,
Parkes, R. J., and Jørgensen, B. B.: Prokaryotic cells of the deep
sub-seafloor biosphere identified as living bacteria, Nature, 433, 861–864,
2005.
</mixed-citation></ref-html>--></article>
