Deep Sea Coral

June 2017 – Oceana Deep sea Coral and Sponge 2017 Final Report


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Oceana Deepsea Coral and Sponge 2017 Final Report

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 1

June 5, 2017

Andrew R. Lauermann, Heidi M. Lovig, Yuko Yokozawa, Johnathan Centoni, Greta Goshorn

 

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 2

Marine Applied Research and Exploration
320 2nd Street, Suite 1C, Eureka, CA 95501 (707) 269-0800
www.maregroup.org

TABLE OF CONTENTS

 

INTRODUCTION 4

METHODS 5

DATA COLLECTION 5

ROV Equipment 5

ROV Sampling Operations 6

POST-PROCESSING 6

Substrate and Habitat 7

Finfish and Invertebrate Enumeration 7

RESULTS 9

SURVEY TOTALS 9

SUBSTRTATE AND HABITAT 11

Substrate 11

Habitat 11

FISH AND INVERTEBRATE TOTAL COUNTS 11

Fish 11

Invertebrates 11

FISH AND INVERTEBRATE DENSITY 16

Fish 16

Invertebrates 16

MAPS OF TRANSECTS 20

Southeast Santa Rosa Island 21

Footprint Deep Ridge 22

West Santa Barbara Island 23

West Santa Barbara Island 24

West Santa Barbara Island 25

South Santa Barbara Island 26

West Butterfly Bank 27

UNIDENTIFIED SPECIES LIST 28

Anemones 28

Boot Sponges 28

UI Lobed Sponge 29

Other Sponges Observed 30

UI Bubblegum Coral 31

REFERENCES 32

INTRODUCTION

From August 7th through 11th of 2016, four study locations were surveyed using a remotely operated vehicle (ROV) within the Sothern California Bight. The goal of this Oceana lead expedition was to collect high definition video and still imagery within unique deep-water sponge and coral habitats. Study areas and dive locations were based on bathymetry mapping data and/or data from NOAA’s Deep Sea Coral National Observation Database. The data collection protocols used for this project were similar  to those used inside the Channel Islands National Marine Sanctuary, Monterey Bay National Marine Sanctuary, Farallon Islands National Marine Sanctuary, Cordell Bank National Marine Sanctuary and at over 175 sites in and adjacent to California’s marine protected areas network.

During the 5-day expedition, deep-water ROV surveys were conducted near Santa Rosa Island, Footprint MPA, Santa Barbara Island and Butterfly Bank. During each  dive, ROV survey lines were broken into 15-minute transects at the discretion of Oceana scientists onboard. Each 15-minute transect and the corresponding positional data were subsequently post-processed in the lab by Marine Applied Research and Exploration (MARE) using standardized methods that were developed in partnership by the California Department of Fish and Wildlife and MARE. These methods have been used since 2003 to process over 2,000 km of ROV video.

The following report describes the data collection and post-processing methods used for the survey. Data summaries are provided which highlight post-processing results and a complete database of all data collected will be provided to Oceana.

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METHODS

DATA COLLECTIONJune 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 4

ROV Equipment

An observation class ROV, the Beagle, was used to complete benthic surveys of select Southern California Bight study locations. The ROV was equipped with a three-axis autopilot including a rate gyro- damped compass and altimeter.  Together, these allowed the pilot to maintain a constant heading (± 1 degree) and constant altitude (± 0.3 m) with minimal corrections. In addition, a forward speed control was used to help the pilot maintain a consistent forward velocity between 0.25 and 0.5 m/sec while on transect. A Tritech® 500 kHz ranging sonar, which measure distance across a

range of 0.1–10 m using a 6° conical transducer, was used as the primary method for measuring transect width from the forward facing HD video. The transducer  was pointed at the center of the camera’s viewing area and was used to calculate the distance to middle of screen, which was subsequently converted to width using the known properties of the cameras field of view. Readings from the sonar were averaged five times per second and recorded at a one-second interval with all other sensor data. Measurements of transect width using a ranging sonar are accurate to ± 0.1 m (Karpov et al. 2006). ROV Beagle was also equipped with parallel lasers set with a 10 cm  spread and positioned to be visible in the field of view of the primary forward camera. These lasers provided a scalable reference of size when reviewing video.

An ORE Offshore Trackpoint III® ultra-short baseline acoustic positioning system with ORE Offshore Motion Reference Unit (MRU) pitch and roll sensor was used to reference the ROV position relative to the ship’s Wide Area Augmentation System Global Positioning System (WAAS GPS). The ship’s heading was determined using a KVH magnetic compass. The Trackpoint III® positioning system calculated the XY position of the ROV relative to the ship at approximately two-second intervals. The ship-relative position was corrected to real world position and recorded in meters as X and Y using the World Geodetic System (WGS)1984 Universal Transverse Mercator (UTM) coordinate system using HYPACK® 2013 hydrographic survey and navigation software. Measurements of ROV heading, depth, altitude, water temperature, camera tilt and ranging sonar distance were averaged over a one-second period and recorded along with the position data.

The ROV was equipped with four cameras, including one forward facing high definition (HD) camera, two standard definition cameras and one HD still camera. The primary

data collection camera (HD video camera) and HD still camera were oriented obliquely forward. All video and still images were linked using UTC timecode recorded as a video overlay or using the camera’s built-in time stamp which was set to UTC time each day.

 

All data collected by the ROV, along with subsequent observations extracted during post-processing of the video, was linked in a Microsoft Access® database using GPS time. GPS time was used to provide a basis for relating position, field data and video observations (Veisze and Karpov 2002). Data management software was used to expand all data records to one second of Greenwich Mean Time (GMT) time code. During video post-processing, a Horita® Time Code Wedge (model number TCW50) was used in conjunction with a customized computer keyboard to record the audio time code in a Microsoft Access® database.

 

ROV Sampling OperationsJune 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 5

R/V Shearwater, a 22 m NOAA research vessel, was used to complete the 2016 survey. At each site, the ROV was piloted along 15-minute transect lines (determined during dive) and was flown off the vessel’s stern using a “live boat” technique that employed a 317.5 kg (700 lb) clump weight. Using this method, all but 50 m of the ROV umbilical was isolated from current-induced drag by coupling it with the clump weight cable and suspending the clump weight at least 10 m off the seafloor. The 45 m tether allowed the ROV pilot sufficient

maneuverability to maintain a constant speed (0.5 to 0.75 m/sec) and a straight course down the planned survey line, while on transect.

 

The ship remained within 35 m of the ROV position at all times. To achieve this, an acoustic tracking system was used to calculate the position of the ROV relative to the ship. ROV position was calculated every two seconds and recorded along with UTC timecode using navigational software. Additionally, the ROV pilot and ship captain utilized real-time video displays of the location of the ship and the ROV, in relation to the planned transect line. A consistent transect width, from the forward camera’s field of view, was achieved using sonar readings to sustain a consistent distance from the camera to the substrate (at the screen horizontal mid-point) between 1.5 and 3 m. In areas with low visibility, BlueView multibeam sonar was used to navigate hazardous terrain.

 

POST-PROCESSING

Following data collection, the ROV position data was processed to remove outliers and data anomalies caused by acoustic noise and vessel movement, which are inherent in these systems (Karpov et al. 2006). In addition, deviations from sampling protocols

such as pulls (ROV pulled by the ship), stops (ROV stops to let the ship catch up), or loss of target altitude caused by traveling over backsides of high relief structures, were identified in the data and not used in calculations of density for fish and invertebrate species.

 

Substrate and Habitat

For each study area, all video collected was reviewed for up to six different substrate types: rock, boulder, cobble, gravel, sand and mud (Green et al. 1999). Each substrate was recorded as discrete segments by entering the beginning and ending UTC timecode. Substrate annotation was completed in a multi-viewing approach, in which each substrate type was recorded independently, enabling us to capture the often overlapping segments of substrates (Figure 1). These overlapping substrate segments allowed identification of mixed substrate areas along the transect line.

 

After the video review process, the substrate data was combined to create three independent habitat types: hard, soft, and mixed habitats (Figure 1). Rock and boulder were categorized as hard substrate types, while cobble, gravel, sand, and mud were all considered to be unconsolidated substrates and categorized as soft. Hard habitat was defined as any combination of the hard substrates, soft habitat as any combination of soft substrates, and mixed habitat as any combination of hard and soft substrates.

 

Finfish and Invertebrate EnumerationJune 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 6

After completion of habitat and substrate review, video was processed to collect data for use in estimating finfish and macro-invertebrate distribution, relative abundance and density. During the review process, both  the forward and down video files were simultaneously reviewed, yielding a continuous and slightly overlapping view of what was present in front of and below the ROV. This approach effectively increased the resolution of the visual survey, by identifying animals that were difficult to recognize in the forward camera, but were clearly visible and identifiable in the down camera.

 

During multiple subsequent viewings, finfish and macro-invertebrates were classified to the lowest taxonomic level possible. Observations that could not be classified  to species level were identified to a taxonomic complex, or recorded as unidentified (UI). During video review, both the HD video and HD still imagery were used to aid in species identification. Each fish or invertebrate observation was entered into a Microsoft Access® database along with UTC timecode, taxonomic name/grouping, sex/developmental stage (when applicable), and count. Fish, were sized using the two sets of parallel lasers to estimate total length. Not all fish were sizeable due to their position within the field of view of the ROV.

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 7

Figure 1. (a) Basic ROV strip transect methodology used to collect video data along the sea floor, (b) overlapping base substrate layers produced during video processing and (c) habitat types (hard, mixed soft) derived from the overlapping base substrate layers after video processing is completed.

All clearly visible finfish and macro-invertebrates were enumerated from the video record. Invertebrate species that typically form large colonial mats or cover large areas and could not be counted individually were instead recorded as invertebrate layers (with discrete start and stop points and percent cover estimates for each segment). Invertebrate patch segments were coded for percent cover using four groupings: 1) less than 25% cover, 2) 25% to 50% cover, 3) 50% to 75% cover and 4) greater than 75% cover. Only data on individual invertebrate observations are presented in this report. Invertebrate patch data are provided as part of the final data submission for use in future analysis.

RESULTS

Due to technical difficulties with the ROV’s USBL tracking system, several ROV dives surveyed during the 2016 expedition do not have positional data. These dives include, dive #8 at East Butterfly Bank and dive #11 at South Santa Rosa Island. Because there was no base data to correlate video observations, dive #8 at East Butterfly Bank was not video post-processed. However, video collect on dive #11 at South Santa Rosa Island had already been processed when it was discovered that the positional files were corrupted. Therefore, fish and invertebrate observational data at South Santa Rosa Island will be included in the data package, but those observations are not presented in the results section of this report.

In addition, dive #6 at West Butterfly Bank was aborted before completing the transect; and no transects were defined during dive #10 at Footprint Ridge.

SURVEY TOTALS

Total number of fish and macro-invertebrates observed and sampling effort and are given in Table 1. Over 18,000 fish and macro-invertebrates were observed at depths ranging from 126 m to 379 m, and a total of 10.8 kilometers of seafloor was surveyed during the completion of 23 transects at all five study areas combined (Figure 2).

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Table 1. Total sampling effort at five Southern California study areas, showing total distance, area, fish and macro-invertebrate counts and depth range.

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 9

Figure 2. ROV dive locations for the five study areas video post-processed.

SUBSTARTATE AND HABITAT

Substrate

Substrate types observed on transects are not mutually exclusive and represent the proportion of the total surveyed transect distance that has a given substrate present (see methods for full description). Overall, mud, cobble and rock substrates were the most common (Table 2). Sand was only observed at Southeast Santa Rosa Island (the shallowest area surveyed).

Habitat

Habitat types derived from substrate data show that across all sites, soft and mixed habitats were the most common, combined accounting for between 81% – 100% of the habitat observed across all sites (Table 2). Hard habitats were the least common accounting for only 0% to 19 % of the available habitat across all sites.

Table 2. Percent substate and habitat types encountered at the five study areas.

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 10

FISH AND INVERTEBRATE TOTAL COUNTS
Fish
Rockfish were the most commonly observed fish accounting for 92.7% of the total fish count at all study areas combined (Table 3). Halfbanded rockfish were the most abundant rockfish species, accounting for nearly 40% of all of the fish observations. The next most abundant species were the following rockfish: YOY, Swordspine rockfish, Sebastomus rockfish, UI rockfish and Pygmy rockfish which combined accounted for another 44% of all fish observations. Cowcod, a currently listed overfished species, was observed, representing 0.3% of the total count. The most abundant non-rockfish grouping was the combfish complex, accounting for 2.4% of the fish observations.

Invertebrates
Four species/groupings of macro-invertebrates accounted for approximately 65% of the total invertebrate counts (Table 4). The most abundant species observed was the fragile pink urchin, which accounted for approximately 26% of the overall count; followed by the squat lobster, UI lobed sponge and white slipper sea cucumber which accounted for the remaining 39%.

Over 3,400 structure forming sponges from 11 species/groupings were observed, accounting for 26% of the total invertebrate observations. Corals were commonly observed and represented 9% of the observations (11 species/groupings). Gorgonians were the most commonly observed coral type, with 3 species/groupings representing the majority of the observations: gray, red swiftia and yellow gorgonians. Fifteen species/groupings of sea stars were also observed, but represented less than 5% of the total macro-invertebrate observations.

Table 3. Overall fish counts are presented in order from highest to lowest abundance.

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Table 4. Overall macro-invertebrate counts are presented in order from highest to lowest abundance.

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Table 4. Continued.

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 13

FISH AND INVERTEBRATE DENSITY

 

FishJune 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 14

At Southeast Santa Rosa Island, fish densities were higher than any other study area, with 53 fish/100 m2 (Table 5). Halfbanded rockfish represented the majority of the density, accounting for over 45 fish/100 m2. When Halfbanded rockfish are not included in the overall densities of each study area, West Santa Barbara Island has the highest overall density at almost 12 fish/100 m2. At West Butterfly Bank, the lowest overall fish density was observed with just over 2 fish per 100 m2.

 Halfbanded rockfish

After Halfbanded rockfish, the next most abundant species/groupings were YOY and swordspine rockfish at West Santa Barbara Island. Sebastomus rockfish, unidentified rockfish and small benthic fish were also common across all sites. Bank rockfish were observed at all sites except at Southeast Santa Rosa Island. Cowcod were only observed at South Santa Barbara Island.

The number of species observed at each study location varied greatly. June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 15Of the 46 species/groupings observed, 30 were observed at West Santa Barbara Island, the highest of all study areas. In contrast, the lowest number of fish species observed was at West Butterfly Bank, with only 11 species/groupings observed.

 

Invertebrates

Cowcod

 

The Footprint Deep Ridge study area had the highest overall macro-invertebrate density, with over 196 invertebrates/100 m2 (Table 6). At Footprint Deep Ridge, fragile pink urchin densities were the highest observed, with densities over 7 times higher than the next most abundant species/grouping, which was the squat lobster at West Butterfly Bank. West Santa Barbara Island had the most species/groupings of any study area surveyed with a total of 52 species/groupings (Table 6).

In contrast, Southeast Santa Rosa Island had the lowest number of invertebrate species/groupings observed and lowest total invertebrate density. At Southeast Santa Rosa Island, a total of 20 invertebrate species/groupings produced a total density of just over 8 invertebrates/100 m2. All other sites overall densities exceeded 33 invertebrates/100 m2.

Coral and sponge species were observed at all study areas, with some notable differences at each location. The gray gorgonian was only observed at West Santa

 

Barbara Island and Footprint Deep Ridge. Densities of the gray corals were almost 16 times June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 16higher at West Santa Barbara Island than at Footprint Deep Ridge. Black corals were found at both the Footprint Deep Ridge and Santa Barbara Island sites, though black corals were over four times denser at Footprint Deep Ridge.

 

Other corals observed included: an unidentified small orange gorgonian (UI orange gorgonian) at Footprint Deep Ridge and West Butterfly Bank, a yellow gorgonian observed at all locations except Footprint Deep Ridge, and the red swiftia gorgonian found at all study areas.

Gray gorgonian

 

 

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 17Structure forming sponges were observed at all study areas, with the highest density observed at West Butterfly Bank. At this site, three sponge types: the hairy boot sponge, UI laced sponge and UI lobed sponge accounted for over 38 sponges per 100m2. Trumpet sponges were unique to only West Butterfly Bank, while the UI large yellow sponge was only observed at West Santa Barbara Island.

UI hairy boot sponge

Sponge identification was based on morphology, which createdJune 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 18
a particular issue for one morphotype: the UI lobed sponge. UI lobed sponges were observed at all study areas, but the type of lobed sponge varied (see unidentified species list). Lobed sponges at West Butterfly Bank were almost entirely ‘Type 3’ lobed sponge, while at both Santa Barbara Island study areasthe lobed sponges were predominantly ‘Type 1’. At Southeast Santa Rosa Island, lobed sponges were entirely ‘Type 1’, while Footprint Deep Ridge was 50% ‘Type 1’ and 50% ‘Type 2’.

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MAPS OF TRANSECTS

 

Maps of ROV transects for all four study areas surveyed are shown in Figures 3 – 9. Each set of maps shows select invertebrates that were of species interest during the survey, and substrate types encountered along each transect.

 

Select invertebrates include: black corals, gorgonians (UI orange, red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

Southeast Santa Rosa Island

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 22

Figure 3. ROV transects at Southeast Santa Rosa Island showing select invertebrates (top) and substrates encountered (bottom). Invertebrate grouping include: black corals, gorgonians (UI orange,  red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

Footprint Deep Ridge

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 23

Figure 4. ROV transects at Footprint Deep Ridge Island showing select invertebrates (top) and substrates encountered (bottom). Invertebrate grouping include: black corals, gorgonians (UI orange,  red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

West Santa Barbara Island

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 24

Figure 5. ROV transects at West Santa Barbara Island showing select invertebrates (top) and substrates encountered (bottom). Invertebrate grouping include: black corals, gorgonians (UI orange, red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

 

West Santa Barbara Island

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 25

Figure 6. ROV transects at West Santa Barbara Island showing select invertebrates (top) and substrates encountered (bottom). Invertebrate grouping include: black corals, gorgonians (UI orange, red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

 

West Santa Barbara Island

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 26

Figure 7. ROV transects at West Santa Barbara Island showing select invertebrates (top) and substrates encountered (bottom). Invertebrate grouping include: black corals, gorgonians (UI orange, red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

 

South Santa Barbara Island

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 27

Figure 8. ROV transects at South Santa Barbara Island showing select invertebrates (top) and  substrates encountered (bottom). Invertebrate grouping include: black corals, gorgonians (UI orange,  red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 28

Figure 9. ROV transects at West Butterfly Bank showing select invertebrates (top) and substrates encountered (bottom). Invertebrate grouping include: black corals, gorgonians (UI orange, red, yellow, gray, red swiftia and unidentified gorgonians), other corals (bubblegum and mushroom corals), basket stars and sponges (laced, large yellow, boot, hairy boot, branched, lobed, vase and trumpet sponges).

UNIDENTIFIED SPECIES LIST

Anemones

The three Unidentified anemone species were observed:

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 29

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 30

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 31

UI anemone 1                                    UI anemone 2                             UI anemone 4

Boot Sponges

Two boot sponges were observed, one ‘hairy’ type and the more typically seen boot sponge:

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 32 June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 33

         UI hairy boot sponge                                                   UI boot sponge

 

UI Lobed Sponge

Three UI lobed sponges were observed. The visually estimated percent of UI lobed sponges for each type by location are given in Table 7.

Type 1: Forms a thicker, softer, more variable mat. It is variable color, and may have darker margins.

Type 2: Forms thin, rigid, sheet-like structures, and is off-white in color.

Type 3: Ossicles are large and clearly visible, and is bright white in color.

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Other Sponges Observed

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 36

UI Bubblegum Coral

Of the 24 UI bubblegum coral observed, only one large, highly branched individual was enumerated across all sites (upper right photo). All other bubblegum coral observed resembled the other three photos shown here.

June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 37

REFERENCES

Greene, H.G., M.M. Yoklavich, R.M. Starr, V.M. O’Connell, W.W. Wakefield, D.E. Sullivan, J.E. McRea Jr., and G.M. Cailliet. 1999. A classification scheme for deep seafloor habitats: Oceanologica Acta 22(6):663–678.

Karpov, K., A. Lauermann, M. Bergen, and M. Prall. 2006. Accuracy and Precision of Measurements of Transect Length and Width Made with a Remotely Operated Vehicle. Marine Technical Science Journal 40(3):79–85.

Veisze, P. and K. Karpov. 2002. Geopositioning a Remotely Operated Vehicle for Marine Species and Habitat Analysis. Pages 105–115 in Undersea with GIS. Dawn J. Wright, Editor. ESRI Press.

 

 

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June 2017 - Oceana Deep sea Coral and Sponge 2017 Final Report 38
2021-03-10T21:21:07-08:00June 1st, 2017|research|

June 2016 – Cruise Report for ‘Patterns in Deep-Sea Corals’ Expedition 2016: NOAA ship Shearwater SW-16-08

Cruise Report for ‘Patterns in Deep-Sea Corals’
Expedition 2016: NOAA ship Shearwater SW-16-08

June 2016 - Cruise Report for ‘Patterns in Deep-Sea Corals’ Expedition 2016: NOAA ship Shearwater SW-16-08 39
June 2016 - Cruise Report for ‘Patterns in Deep-Sea Corals’ Expedition 2016: NOAA ship Shearwater SW-16-08 40

Disclaimer:
This publication does not constitute an endorsement of any commercial product or intend to be an opinion beyond scientific or other results obtained by the National Oceanic and Atmospheric Administration (NOAA). No reference shall be made to NOAA, or this publication furnished by NOAA, to any advertising or sales promotion which would indicate or imply that NOAA recommends or endorses any proprietary product mentioned herein, or which has as its purpose an interest to cause the advertised product to be used or purchased because of this publication.

The recommended citation for this report is:
Etnoyer PJ, Shuler AJ, Frometa J, Lauermann A, & Rosen D (2017). Cruise Report for ‘Patterns in Deep-Sea Corals’ Expedition 2016: NOAA ship Shearwater SW-16-08. NOS NCCOS 233, NOAA National Ocean Service, Charleston, SC 29412. 21 pp.Cover image credit: Marine Applied Research and Exploration/NOAA.

June 2016 - Cruise Report for ‘Patterns in Deep-Sea Corals’ Expedition 2016: NOAA ship Shearwater SW-16-08 41

Cruise Report for ‘Patterns in Deep-Sea Corals’
Expedition 2016: NOAA ship Shearwater SW-16-08

Peter Etnoyer1

, Andrew Shuler2

, Janessy Frometa2

, Andrew Lauermann3

, Dirk Rosen3

1 NOAA National Centers for Coastal Ocean Science, 219 Fort Johnson Rd., Charleston, SC 29412
2 JHT, Inc, 219 Fort Johnson Rd., Charleston, SC 29412
3
Marine Applied Research and Exploration. 1230 Brickyard Cove Road #101, Richmond, CA 94801

June 2016 - Cruise Report for ‘Patterns in Deep-Sea Corals’ Expedition 2016: NOAA ship Shearwater SW-16-08 42

Table of Contents

1. Expedition Overview………………………………………………………………………………………………..1
2. Narrative of Cruise Results………………………………………………………………………………………1
2.1 Objective 1: recover previously deployed temperature loggers …………………………….1
2.2 Objective 2: conduct ROV seafloor surveys ……………………………………………………….1
2.3 Objective 3: collect live Acanthogorgia sp. corals for laboratory studies ………………1
3. Discussion………………………………………………………………………………………………………………..2
4. Acknowledgements…………………………………………………………………………………………………..2
5. References ……………………………………………………………………………………………………………….2
6. Tables………………………………………………………………………………………………………………………3
7. Figures …………………………………………………………………………………………………………………….6
8. Appendices ……………………………………………………………………………………………………………10
Appendix A: Operational Notes……………………………………………………………………………..10
Appendix B: Individual temperature logger site information, images and data. …………..12

Cruise Report for ‘Patterns in Deep-Sea Corals’ Expedition 2016: NOAA ship Shearwater
SW-16-08

1. Expedition Overview

The 2016 ‘Patterns in Deep-Sea Corals’ expedition set out aboard the NOAA Ship Shearwater inAugust to study the distribution, ecology, and health of deep-water (30-300 m) gorgonian corals in response to the 2015 El Niño event. The research team consisted of staff from NOAA National Centers for Coastal Ocean Science (NCCOS) and Marine Applied Research and Education (MARE; Table 1). The study used the remotely operated vehicle (ROV) Beagle to recover previously deployed temperature loggers (Caldow et al. 2015) and to conduct video transects for the purpose of density estimation and health assessments.
The primary scientific objectives of the expedition were to: 1) recover temperature loggers that were deployed in the spring and fall of 2015 in order to assess temperature anomalies; 2) characterize deep- sea coral ecosystems in newly mapped areas of the Channel Islands National Marine Sanctuary

(CINMS) (Figures 1-4); and 3) collect live Acanthogorgia sp. corals for laboratory studies on temperature.

2. Narrative of Cruise Results

The expedition’s scientific objectives were successfully met thanks in large part to good weather and few technical difficulties. In addition to the scientific objectives, several outreach activities were completed during the expedition, including. A dockside presentation for six people in Santa Barbara Harbor, and an at sea day for seven people, during which they were able to come aboard the NOAA Ship Shearwater and participate in a ROV dive. The VIP party included representatives from Conservation International, Rockefeller Foundation, Coral Reef Watch, and others. 2.1 Objective 1: Recover previously deployed temperature loggers The ROV recovered all four temperature loggers from depths ranging between 20-100 m. Data was successfully downloaded from each logger, and plotted across time (Figure 5 and Appendix A). Temperatures averaged between 14-15 0C at 20 m, with a maximum of 19 0C in July. Temperatures at 50 m exceeded 15 0C on average, but never reached the 19 0C threshold observed at 20 m.

Temperatures showed little temporal variation at 100 m, and ranged between ~10-12 0C. In the future, this temperature data will be analyzed in more detail in order to identify trends and anomalies. This analysis will also incorporate temperature data collected from CTD casts near the Channel Islands, and
other sources.

2.2 Objective 2: Conduct ROV seafloor surveys

Of the 14 ROV dives conducted over the course of the expedition, the majority took place over the newly mapped areas north and south of Santa Rosa Island (Figures 2-4; Table 3). The total bottom time was 17 hours and 51 minutes, during which 30 video transects were completed (Table 4). Video data collected during the ROV transects will be analyzed in order to determine species composition, health and densities of deep-water corals. This data will become publicly available within one year through the NOAA Deep Sea Coral Data Portal (https://deepseacoraldata.noaa.gov/). 2.3 Objective 3: Collect live Acanthogorgia sp. corals for laboratory studies The team successfully collected two live colonies of Acanthogorgia sp. octocorals from 200 m. Upon retrieval from the ROV, each colony was split into six fragments. Coral fragments were shipped to both the Claremont College in California, and the Deep Coral Ecology Laboratory in Charleston, SC.

The live corals arrived at their respective institutions within 24 h of shipment, and were successfully acclimated into an aquarium environment (Figures 7-8). While the original goal was to collect four small colonies, the colonies collected were large enough to provide enough material for laboratory
experimentation.

3. Discussion
The successful recovery of all temperature loggers is an important accomplishment, particularly since three of the four loggers were deployed from a ship. Additionally, we were able to successfully download data from all temperature loggers, indicating that they hold up well under the conditions and
duration of our deployment. It is important to point out that the temperature logger deployed at the shallowest depth (20 m) had substantial overgrowth by encrusting fauna, whereas overgrowth was minimal in the other three loggers. Therefore, future deployments of these devices at depths shallower than 50 m should consider providing some means to deter fouling, with either external housing or anti-fouling paint.

The ROV dives focused on habitat characterization and dive time was split between transects and exploration. This split approach allowed the science team to obtain quantitative information on the coral communities during transects, as well as provided time to explore the newly-mapped environment more freely. The use of dedicated transects also facilitated the process of estimating octocoral density, by ensuring consistent speed, altitude, and direction.
The collection of live corals from deeper than 50 m is another important accomplishment of this expedition. One of the dives was dedicated exclusively for specimen collections, and this approach was critical in reducing undue stress to the organisms. Future collections of live material should consider a
similar approach.

4. Acknowledgements
The authors would like to acknowledge the support and guidance of the Channel Islands National Marine Sanctuary staff especially Chris Caldow, Julie Bursek, and Ryan Freedman. It is also important to note the skill and expertise of the crew of the NOAA Ship Shearwater, specificallyCaptain Terrance Shinn, First Mate Charles Lara, and Lieutenant junior grade Elizabeth Mackie. Equally as important were team members Steve Holz and Rick Botman of Marine Applied Research and Exploration for their critical support to this mission. These individuals were instrumental to the smooth deployment and operation of the ROV Beagle and the success of this expedition.

5. References
Caldow, C., P. J. Etnoyer, L. Kracker. 2015. Cruise Report for ‘Patterns in Deep-Sea Corals’
Expedition: NOAA ship Bell M. Shimada SH-15-03. NOAA Technical Memorandum NOS NCCOS
200. 15 pp. Silver Spring, MD.
OSPAR. 2010. Background Document for Coral Gardens. Publication number 486. OSPAR
Biodiversity Series. https://www.ospar.org/documents?v=7217

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8. Appendices

Appendix A: Operational notes

July 31, 2016. Mobilization began at 0830 at Santa Barbara Harbor. JHT/NOAA staff members
loaded science gear and purchased food. MARE staff members loaded and set up the ROV and
associated equipment. After mobilization was complete, Rosen and Etnoyer provided an outreach
event for six current and potential MARE donors on the NOAA Ship Shearwater dock, which
included a presentation of the mission goals.

August 1, 2016. The expedition got off to a rough start, as the vessel hit a piling and bent the tracking
pivot irreparably. Ed Liquorek, the brother of a local angler, fabricated a new pivot. The NOAA Ship
Shearwater left the dock at 1300 and transited to the north side of Anacapa Island, arriving by 1530.
The ROV was deployed by 1630 to retrieve temperature loggers at 20 m. The ROV encountered a
large black seabass as soon as the ROV reached bottom. The team retrieved two temperature loggers
(B and P) during the first dive. A large air bubble seeped into the main tether compensator overnight.
Lauermann and Rosen had purged the bubble prior to the ROV deployment, but it reappeared after the
20 m dive, 55 m dive (logger D retrieval), and 110 m dive (logger C retrieval at NMFS sled site). This
marked the first use of HD video for the live feed from the ROV. The focus was acceptable, but the
color appeared washed out at times. Overall, it was much improved over standard definition. The
final ROV dive of the day was completed by 2000 and the manipulator skid was removed since all
temperature loggers had been recovered. The NOAA Ship Shearwater transited to South Santa Rosa
to anchor overnight.

August 2, 2016. The tether compensator was purged of air in transit to the north side of Santa Rosa.
The ROV was first deployed at 0800. Three dives were conducted through the course of the day, for a
total of 12 transects of 15-minute duration each, in addition to general exploration at three different
sites. The three dives were at 80 m, 70 m and 65 m. The tether needed to be purged after each dive,
because the piston completely bottomed out after each dive. To improve the quality of the HD feed
and video, the white balance was adjusted using white plastic bags on the clump shroud. This
improved the color of the video. During the dives, some Adelogorgia gorgonians were noted on
ridges, along with an abundance of Eugorgia gorgonians, both of which appeared healthy. In addition
to these corals, the team noted a few spots with many lingcod, copper, starry, and a few gopher
rockfish, bocaccio and sheephead. ROV pilots noted that moving the vertical thruster forward this
winter helped make the ROV perform better straight up and down, and moving the altimeter forward
improved auto-altitude function over moderate terrain. The HMI lights on the ROV became erratic
through the course of the day and did not stay on. With the low light HD camera, and the reds of the
tungsten light still allowing for good photos to be captured, the need for the HMIs was questionable.
The ROV team used a new AA Beacon, and it performed adequately down to 70 m. The ROV was
recovered and operations were concluded by 1800. The NOAA Ship Shearwater anchored at
Johnsons’ Lee, Santa Rosa for the evening. Elephant seals were heard billowing throughout the night.
August 3, 2016. The weather remained good allowing for continued exploration of new SE Santa
Rosa sites. The ROV was first deployed at South Santa Rosa at 0800 and conducted four dives with
14 transects of 15-minute duration at four different localities at depths of 95m, 105m, 85m and 90m..
Many corals were observed, several at densities consistent with Coral Gardens (1/m2 over distances of
at least 100 m) (OSPAR 2010). There was some noticeable injury to gorgonians from zooanthids,
some toppled colonies were documented, as well as two white nudibranchs, and a crab photographed
utilizing sponges. These dives also documented several ledges and uplifted shelves that made great
coral habitat. Fish documented on these dives included two cowcod, a wolf eel, and many rockfish.
The last dive of the day had good visibility (30 m) at 0200. During dive operations there was one
ROV power outage, however, the team recovered from this within 2 min. The main pressure balance
oil filled junction was still taking in air, but not as much as previous days, though the piston bottomed
out each dive. The use of HMIs was abandoned. Weather deteriorated throughout the day.

August 4, 2016. Deployed ROV at South Santa Rosa at 0800. ROV Beagle completed dives over
areas that had previously been mapped with backscatter and contained substantial hard-bottom
habitats. One dive started at 85 m, and another dive at 110 m. Conducted four transects of 15-minutes
duration near South Santa Rosa during these two dives. A few potential coral gardens were identified,
but several of these showed signs of injury and yellow zooanthid overgrowth. Then the ship moved to
220 m to collect two live Acanthogorgia sp. colonies. The ROV camera flooded with oil and as a
result the first attempt was aborted. The ROV team then replaced the flooded HD camera with a Sidus standard definition video camera and finished the job. The second attempt resulted in the collection of two Acanthogorgia colonies. Upon successful collection of these colonies, the ROV was recovered and back aboard by 1500. The NOAA Ship Shearwater transited to Ventura Harbor and arrived at 1700.

August 5, 2016. In an effort to further the outreach efforts of the expeditions, VIPs Boltz, Hannah, Teplitz, Ledvina, Graham, Chacin, Robertson, and MARE Director of Donor Relations Phil Stevens, boarded the ship by 0800, and departed for Anacapa Island to explore the Anacapa/Footprint essential fish habitat (EFH) by 0900. The team deployed the ROV at Footprint and conducted an approximately two hour dive up to the NMFS sled, then moved to the lee side of Anacapa, near the net in order to let the VIPs operate the ROV under supervision of the ROV team. Each guest steered the ROV for 4-5 min, which received an enthusiastic response. The NOAA Ship Shearwater returned to Ventura by 1700 to drop off the VIPs, and then the vessel returned to Santa Barbara for its next expedition.

Appendix B: Individual temperature logger site information, images and data.
Shallow target: Loggers B (Star-Oddi logger, silver) and P (Hobo logger, black)
Site: AI-1
Line: 100
Depth: 21 m
Latitude: 34.017364
Longitude: -119.440728
Deployment Method: Shipside
Deployment Date: November 12, 201515

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United States Department of Commerce
Wilbur Ross
Secretary of Commerce
National Oceanic and Atmospheric Administration
Benjamin Friedman
Deputy Under Secretary for Operations
and Acting Administrator
National Ocean Service
Russell Callender
Assistant Administrator

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