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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/918318.rdf" xlink:actuate="onRequest">Benthic seawater temperature at 10m depth in Moorea, French Polynesia from 2005 to 2021</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Edmunds, P. J., Burgess, S., Maritorena, S. (2024) Benthic seawater temperature at 10m depth in Moorea, French Polynesia from 2005 to 2021. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-01-23 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.918318.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Methods and Sampling: &amp;lt;p&amp;gt;The ecological methods are described in detail in Edmunds et al. (2024, doi:10.1007/s00442-024-05517-y), and are briefly summarized below.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The study utilized the time series of the Moorea Coral Reef LTER, as they relate to coral community dynamics on the north shore fore reef. Annual measurements of coral cover, the density of coral settlers, and the density of small corals were used together with records of the environmental conditions to which they were exposed. Analyses focused on 2008–2021, which captured the final years of the last population outbreak of the crown of thorns (COTs) sea star, the coral population recovery that took place between 2010 and 2019, and coral mortality attributed to bleaching in 2019. Biological data came from two sites (LTER1 and LTER2) that are ~ 3 km apart, with environmental data from the same or similar sites (temperature), one of the two sites (flow at LTER1), or from 4.5 km resolution remote sensing data (Chlorophyll a).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Temperature was recorded with bottom-mounted sensors (Seabird SBE39, ± 0.002°C) at 10-m depth, with one sensor at each of LTER2 and 300 m west of LTER1 (named LTER0). &amp;amp;nbsp;Data were obtained&amp;amp;nbsp;from MCR data file knb-lter-mcr.1035.14 accessed 11 March 2022, from 10 m depth (doi: 10.6073/pasta/b8b3c1a927b7639459a244ff2ceef4e2). Sensors recorded at 0.0008 Hz, and values were averaged by day. This dataset only includes data from LTER0 and LTER2 and were used to characterize sites LTER1 and LTER2. In this file, “Site” column in this dataset refers to the site to which the data were applied in the statistical analysis (LTER1 or LTER2) and “the Data_Source” column shows which combination of sensors (at LTER0 or LTER2) was used to source the data.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Methodology excerpt from originating source data&amp;amp;nbsp;knb-lter-mcr.1035.14:&amp;lt;br /&amp;gt;
“A continuous time series of benthic water temperature is measured with bottom-mounted thermistors at six sites around the shores of Moorea, on the fringing reef, backreef, and forereef. The forereef temperature is recorded with SBE 39s at 10, 20, 30 and 40 m, starting between 2005 to 2007, except FOR00 starting in 2010. These are ongoing except the 40 m deployments were discontinued after August 2019. The backreef SBE 39s are mounted on plates at 1 m depth at LTER 1 and at 2 m depth at the other five sites. Onset HOBOs are deployed on the fringing reef at one shallow 1 m depth and one deeper depth varying by site as follows: 6 m at LTER 1, 4 m at LTER 2, 7 m at LTER 3, 6 m at LTER 4, 3 m at LTER 5 and 4 m at LTER 6. Those depths do not vary. The mounting plate is fixed to the reef. These depths are not measured by the thermistors and should be considered categorical. Temperature data are processed and resampled to a 20 minute time step. This material is based upon work supported by the U.S. National Science Foundation under Grant No. OCE 16-37396 (and earlier awards) as well as a generous gift from the Gordon and Betty Moore Foundation. Research was completed under permits issued by the French Polynesian Government (Délégation à la Recherche) and the Haut-commissariat de la République en Polynésie Francaise (DTRT) (Protocole d'Accueil 2005-2022). This work represents a contribution of the Moorea Coral Reef (MCR) LTER Site.”&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
* See &amp;quot;Related Datasets&amp;quot; section for access to related dataset pages which include dataset-specific methodology.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/918266.rdf" xlink:title="OCE-2224354" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2224354 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2224354</gmx:Anchor>
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&lt;p&gt;Coral reefs provide important benefits to society, from food to exceptional biodiversity to shoreline protection and recreation, but they are threatened by natural perturbations and human activities, including those causing global-scale changes. These pressures increasingly are causing coral reefs to undergo large, often abrupt, ecological changes where corals are being replaced by seaweeds or other undesirable organisms. Historically, the major agent of disturbance to coral reefs has been powerful storms, but in recent decades, episodes of mass coral bleaching from marine heat waves have become more frequent and severe as the temperature of ocean surface waters continues to rise. Coral reefs are further stressed by local human activities that cause nutrient pollution and deplete herbivorous fishes that control growth of seaweeds. Studying how coral reefs respond to these two types of disturbance under different levels of nutrient pollution and fishing provides essential information on what affects the ability of coral reefs to buffer environmental change and disturbances without collapsing to a persistent, degraded condition. The fundamental goals of the Moorea Coral Reef Long Term Ecological Research program (MCR LTER) are to understand how and why coral reefs change over time, to assess the consequences of these changes, and to contribute scientific knowledge needed to sustain coral reef ecosystems and the important societal services they provide. This research improves understanding and management of coral reefs, which benefits all groups concerned with the welfare of this ecologically, economically and culturally important ecosystem. In addition to academic communities, scientific findings are communicated to interested individuals, non-governmental organizations, island communities and governmental entities. These findings also are integrated into K-12, undergraduate, graduate and public education activities through a multi-pronged program that includes inquiry-based curricula, interactive and media-based public education programs, and internet-based resources. MCR?s research, training, education and outreach efforts all emphasize broadening participation in STEM fields and strengthening STEM literacy.&lt;/p&gt;
&lt;p&gt;New research activities build on MCR LTER?s powerful foundation of long-term observations and broad ecological understanding of oceanic coral reefs to address the following core issues: How is the changing disturbance regime (recurrent heat waves in addition to cyclonic storms) altering the resilience of coral reefs, and what are the ecological consequences of altered resilience? Research activities are organized around a unifying framework that explicitly addresses how reef communities are affected by the nature and history of coral-killing disturbances, and how those responses to disturbance are influenced by the pattern of local human stressors. New studies answer three focal questions: (1) How do different disturbance types, which either remove (storms) or retain (heat waves) dead coral skeletons, affect community dynamics, abrupt changes in ecological state, and resilience? (2) How do local stressors interact with new disturbance regimes to create spatial heterogeneity in community dynamics, ecosystem processes, and spatial resilience? And (3) What attributes of coral and coral reef communities influence their capacity to remain resilient under current and future environmental conditions? These questions provide an unparalleled opportunity to test hypotheses and advance theory regarding ecological resilience and the causes and consequences of abrupt ecological change, which is broadly relevant across aquatic and terrestrial ecosystems.&lt;/p&gt;
&lt;p&gt;This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;From &lt;a href=&quot;http://www.lternet.edu/sites/mcr/&quot;&gt;http://www.lternet.edu/sites/mcr/&lt;/a&gt; and &lt;a href=&quot;http://mcr.lternet.edu/&quot;&gt;http://mcr.lternet.edu/&lt;/a&gt;&lt;/strong&gt;:&lt;br /&gt;
The Moorea Coral Reef LTER site encompasses the coral reef complex that surrounds the island of Moorea, French Polynesia (17°30'S, 149°50'W). Moorea is a small, triangular volcanic island 20 km west of Tahiti in the Society Islands of French Polynesia. An offshore barrier reef forms a system of shallow (mean depth ~ 5-7 m), narrow (~0.8-1.5 km wide) lagoons around the 60 km perimeter of Moorea. All major coral reef types (e.g., fringing reef, lagoon patch reefs, back reef, barrier reef and fore reef) are present and accessible by small boat.&lt;/p&gt;
&lt;p&gt;The MCR LTER was established in 2004 by the US National Science Foundation (NSF) and is a partnership between the University of California Santa Barbara and California State University, Northridge. MCR researchers include marine scientists from the UC Santa Barbara, CSU Northridge, UC Davis, UC Santa Cruz, UC San Diego, CSU San Marcos, Duke University and the University of Hawaii. Field operations are conducted from the UC Berkeley Richard B. Gump South Pacific Research Station on the island of Moorea, French Polynesia.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;MCR LTER Data:&lt;/strong&gt; The Moorea Coral Reef (MCR) LTER data are managed by and available directly from the MCR project data site URL shown above.  The datasets listed below were collected at or near the MCR LTER sampling locations, and funded by NSF OCE as ancillary projects related to the MCR LTER core research themes.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;This project is supported by continuing grants with slight name variations:&lt;/strong&gt;&lt;/p&gt;
&lt;ul&gt;
&lt;li&gt;LTER: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR II - Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR IIB: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR III: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR IV: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
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	Units: unitless
	Description: &lt;p&gt;Year of measurement&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/918505.rdf
	Name: Month
	Units: unitless
	Description: &lt;p&gt;Month of measurement (1 = January, 2 = February, etc)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/918506.rdf
	Name: Day
	Units: unitless
	Description: &lt;p&gt;Day of month&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/918507.rdf
	Name: Temperature
	Units: degrees Celsius (degC)
	Description: &lt;p&gt;Seawater temperature record&lt;/p&gt; 
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&amp;lt;p&amp;gt;The study utilized the time series of the Moorea Coral Reef LTER, as they relate to coral community dynamics on the north shore fore reef. Annual measurements of coral cover, the density of coral settlers, and the density of small corals were used together with records of the environmental conditions to which they were exposed. Analyses focused on 2008–2021, which captured the final years of the last population outbreak of the crown of thorns (COTs) sea star, the coral population recovery that took place between 2010 and 2019, and coral mortality attributed to bleaching in 2019. Biological data came from two sites (LTER1 and LTER2) that are ~ 3 km apart, with environmental data from the same or similar sites (temperature), one of the two sites (flow at LTER1), or from 4.5 km resolution remote sensing data (Chlorophyll a).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Temperature was recorded with bottom-mounted sensors (Seabird SBE39, ± 0.002°C) at 10-m depth, with one sensor at each of LTER2 and 300 m west of LTER1 (named LTER0). &amp;amp;nbsp;Data were obtained&amp;amp;nbsp;from MCR data file knb-lter-mcr.1035.14 accessed 11 March 2022, from 10 m depth (doi: 10.6073/pasta/b8b3c1a927b7639459a244ff2ceef4e2). Sensors recorded at 0.0008 Hz, and values were averaged by day. This dataset only includes data from LTER0 and LTER2 and were used to characterize sites LTER1 and LTER2. In this file, “Site” column in this dataset refers to the site to which the data were applied in the statistical analysis (LTER1 or LTER2) and “the Data_Source” column shows which combination of sensors (at LTER0 or LTER2) was used to source the data.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Methodology excerpt from originating source data&amp;amp;nbsp;knb-lter-mcr.1035.14:&amp;lt;br /&amp;gt;
“A continuous time series of benthic water temperature is measured with bottom-mounted thermistors at six sites around the shores of Moorea, on the fringing reef, backreef, and forereef. The forereef temperature is recorded with SBE 39s at 10, 20, 30 and 40 m, starting between 2005 to 2007, except FOR00 starting in 2010. These are ongoing except the 40 m deployments were discontinued after August 2019. The backreef SBE 39s are mounted on plates at 1 m depth at LTER 1 and at 2 m depth at the other five sites. Onset HOBOs are deployed on the fringing reef at one shallow 1 m depth and one deeper depth varying by site as follows: 6 m at LTER 1, 4 m at LTER 2, 7 m at LTER 3, 6 m at LTER 4, 3 m at LTER 5 and 4 m at LTER 6. Those depths do not vary. The mounting plate is fixed to the reef. These depths are not measured by the thermistors and should be considered categorical. Temperature data are processed and resampled to a 20 minute time step. This material is based upon work supported by the U.S. National Science Foundation under Grant No. OCE 16-37396 (and earlier awards) as well as a generous gift from the Gordon and Betty Moore Foundation. Research was completed under permits issued by the French Polynesian Government (Délégation à la Recherche) and the Haut-commissariat de la République en Polynésie Francaise (DTRT) (Protocole d'Accueil 2005-2022). This work represents a contribution of the Moorea Coral Reef (MCR) LTER Site.”&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
* See &amp;quot;Related Datasets&amp;quot; section for access to related dataset pages which include dataset-specific methodology.&amp;lt;/p&amp;gt;</gco:CharacterString>
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** Missing data values are displayed differently based on the file format you download.  They are blank in csv files, &amp;quot;NaN&amp;quot; in MatLab files, etc.
* Column names adjusted to conform to BCO-DMO naming conventions designed to support broad re-use by a variety of research tools and scripting languages. [Only numbers, letters, and underscores.  Can not start with a number]

* Date column added from year month day columns

* Rows for years with Month 2 Day 29 in years that there were only 28 days in Feb were removed from this dataset.  There was no temperature value for these rows (was missing data identifier).
* dataset references to results publication Edmunds et al 2023 changed to 2024 since that was the year assoicated with the DOI after final publication. Edmunds et al. (2024, doi:10.1007/s00442-024-05517-y)</gco:CharacterString>
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