Winter 2022 science in the Bonner lab
The Rothera 2022 wintering marine team had to take diving out of the equation this winter due to unforeseen circumstances. Diving is a tool that allows marine scientists to access their underwater office and conduct a range of data collection such as the deployment of underwater experiments, species collection, surveys of the seabed along a transect, the use of specialised equipment to measure species responses and much more. In order to gain an accurate understanding of what is happening in Antarctic marine environments, divers need to be up close and personal with their subject. We call this type of work ‘in situ’ observations.
DEBRA, our ROV
Other tools can also be used to sample the marine
environment and contribute towards maintaining long term time series to
document changes over the years. Remotely Operated Vehicles (ROVs) allow the
exploration of marine environments and require a pilot to drive the underwater
robot. Our ROV is called DEBRA, short for deep
environment benthic research apparatus.
DEBRA can dive to depths way beyond our diving limit; our limit is 30
meters where our time permitted on the bottom is only 15 minutes. DEBRA can
dive to 100 meters and can be fitted with a claw or a Go Pro and can stay at
this depth for 3 hours! The claw is manoeuvrable in four axis so it can rotate,
open and close. A series of underwater deployments were deployed in 2017 by
marine biologist Ben Robinson. Rocks and Perspex settlement panels were set
across three depths, 30, 60 and 100 m. The aim was to monitor the settlement of
sessile (non-mobile) invertebrates and to make a comparison across different
depths and compare species diversity between natural versus artificial
substrate. Collecting samples which have been deployed for five years is exceptionally
rare and presents its challenges. First, the ever imposing threat of icebergs
threaten the integrity of these deployments. Icebergs have a deep keel and have
the ability to scour the seabed and take any existing structures along with it.
Second, DEBRA is deployed from a boat down to 100 meters on specific waypoints.
Louis Day driving the boat whilst DEBRA is deployed into the water, view from her front eye (a GoPro).
The boat and DEBRA are subject to wind and tide and great
care has to be made to keep the boat in position using the GPS. A lapse in
concentration can see the boat drifting off and in turn dragging Debra along
the seabed, or worse, wrapping the long electrical tether around the spinning
propellers. As the wind pushes the boat back and forth both the throttle and
steering have to be constantly adjusted to keep the boat in position. The ROV
tether is coiled on a reel at the bow of the boat and needs to be paid out or
wound in as Debs descends or ascends - not enough line out will prevent her
from moving and will transfer any movement from the boat straight to Debra and
therefore makes her very difficult to control. Too much line can tangle around
itself, Debra, rocks on the seabed or the boat engines. The weight of excess
line can also pull her backwards as if being dragged by the boat.
Therefore, ROV operations must be conducted in calm conditions with little swell and wind below 10 knots. Many hours are spent searching for these underwater deployments which are marked with a 1m length of rope and a subsurface buoy. Upon location, the pilot uses precise movements to open the claw, inch forwards and pinch the subsurface rope. This is all visible on a controller screen which is connected to DEBRA via an electrical tether. The claw is closed and the sample is slowly hauled to the surface. Samples are then processed and analysed in the Bonner laboratory. In order to identify bryozoan species, the rocks and panels must be completely dry to distinguish between features. Multiple photos of the settlement panels are stitched together and allow the percentage cover of species to be assessed. Competition between species can be assessed between the panels across the depth transect.
An example of the samples DEBRA collected from 100m, settlement panels with a community of encrusting animals called bryozoans.
We continued to conduct the weekly CTD and water sampling events
over our winter. The CTD measures conductivity (salinity), temperature and
depth. It also measures pigment levels in the water, which shows how much
phytoplankton there is, allowing an assessment of the water primary production.
Productivity changes throughout the seasons with changing sunlight and sea ice.
Collecting this data is extremely valuable to monitor long-term changes. The
more phytoplankton in the water, the more food is available for larger
organisms to feed, supporting complex food webs.
On board one of our RIBS, Erebus, with Louis Day as the Cox and Alice Clement using a winch to collect samples.
In addition to water sampling, biological long term time
series involve the monthly collection of eight dominant invertebrate species.
This time series began in 1997 and aim to document the reproductive patterns of
marine invertebrates in response to environmental factors. For examples,
questions such as ‘if waters warm, will invertebrates be more or less efficient
at producing the next generation?’ can be answered. The utility of multiyear
data will permit the identification of long term signals associated with
climate change. Usually, divers would collect these animals from two sites in
Ryder Bay. This year, we have used a combination of Van Veen grabs, to collect
bivalves that burrow into the sediment and baited traps which attract brittle
stars in particular. Furthermore, the subsurface rope that is used to mark
deployments, collected using the ROV, provide an excellent settlement substrate
for sea squirts and sea cucumbers. Species collected on theses ropes have also contributed
towards the monthly species collection.
The marine team also participate in a project
to monitor marine invertebrate feeding activity. Ordinarily, divers would swim
along a pre-defined transect and visually record feeding in suspension feeders.
The aim is to establish the timing of periods of feeding and non-feeding to
relate the timing of summer feeding activity to that of the seasonal
phytoplankton bloom and dynamics of winter sea ice .The switch from feeding to
non-feeding can occur in a matter of weeks where a whole colony of sessile
invertebrates could transition from feeding to not feeding and vice versa.
Another fantastic tool that can be deployed from our RIBS are Baited Remote Underwater Video Systems (BRUVS for short). These rigs are
deployed either on the sea bed or mid water to sample fish assemblages and
gather data about species which are otherwise mostly illusive when diving due
the disturbance caused by divers. Two
camera are positioned at a fixed distance on each rig. Once a fish is
identified during video playback, trigonometry can be used to calculate the
length of the fish and hence give information about the structure of fish
populations.
In conclusion, the Bonner team has been able to fulfil key
research goals without diving and continue to collect environmental and
biological data to understand how changes will affect polar diversity. The
outcome of this work will provide an insight into the impacts environmental
change will have on the natural world and contribute towards future
conservation measures.
Nice one guys! Sounds like Debra definitely earned her place in the Bonner team photo ;)
ReplyDeleteThanks Jas !!! She certainly put some work in. Imagine if her claw could be engineered to burn into a frame ... Also realised half the photos didn't upload ...oops
DeleteWhy has there been no diving this winter? Great innovative thinking from the team to come up with alternative solutions to continue the essential science though!!
ReplyDelete