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A Picture is Worth a Thousand Worms | Steve Sabo & Kersey Sturdivant | TEDxNewport


this was not possible 30 years ago

capturing vivid imagery of cryptic

organisms at and beneath the ocean floor

and that’s what we do we use innovative

technology to image the seafloor but we

don’t just take pictures of the seafloor

that’s true Steve we use these images to

make quantitative analyses that allow us

to better understand the functioning of

the sea floor within the larger

perspective of the ocean and then we use

the data that we collect to make

innovative data visualizations that

allow anybody not just scientists like

ourselves access to this unique and

interesting ecosystem wait Steve let’s

take a step back before we delve too

much and to the innovative work that we

do it’s important that people understand

how critical the ocean and the sea floor

are for the speck of space dust we call

our planet we humans are terrestrial

creatures and as a result much of our

perspectives about the earth are shaped

from our interactions and visual

observations on land however when we

take a step back and look at the earth

as a whole we realize that the earth is

a pale blue dot and that’s because

despite our terrestrial eccentric

mindsets much of our planet is covered

by the ocean given the vast spatial

extent of the oceans on earth surface it

should come as no surprise that this

vast body of water plays a key role in

life on our planet including the lives

of humans ocean processes influence all

of humanity where the residents of the

coast or inland via the regulation of

climate local weather patterns economic

impact and food security among others we

are inherently dependent on the help of

a global ocean ecosystem

which beneath its surface exists at a

far greater scale than its visible on a

globe and at the very bottom of the

ocean is the seafloor I’m predominant

habitat serving a variety of functions

and hosting its own brand of unique and

interesting life if the oceans cover

seventy percent of our planet then

inherently seventy percent of the

earth’s surface is the seafloor and in

the larger scheme of the ocean the

seafloor holds great importance for

ocean health the seafloor is home to

many unique and diverse environments

such as seagrass Meadows kelp bars then

communities and coral reefs these

dynamic areas service safe haven

nurseries for young ocean life and

contribute greatly to ocean productivity

however despite their well-documented

importance these habitats are not the

predominant bottom type of the seafloor

coral reefs make up less than point one

percent of total ocean bottom put that

into perspective that’s roughly half the

size of the country of France and

combined coral reefs sea grasses and

kelp bars make up less than one percent

of the total seafloor so what else is

there what makes up that 99% most of the

sea floor looks something like this it’s

a habitat of soft sediment that’s

largely composed of small scale features

such as tubes burrows and mounds but

despite this relatively muted appearance

this large area of Earth’s surface holds

huge importance for the functioning and

help of the ocean think of the soft

bottom sea floor as the lungs of the

ocean these areas serve as a sump for

ocean pollutants and a recycling plant

for ocean nutrients it’s easy to

conceptualize the importance of seafloor

environments

kelp forests and coral reefs because we

can easily visualize the complexity and

diversity of the structures and

organisms that exist there however when

we compare those areas to the soft

bottom sea floor while there are some

features on the seabed most of the

structural complexity exists beneath the

opaque surface of the sea floor making

this cryptic environment and it Taurus

Lee difficult to observe but if you’re

fortunate enough to peek beneath the

seafloor you observe a dynamic world

full of complexity and diversity one

which is often not immediately obvious

when viewing the seafloor from only the

surface the best way to think about what

you’re seeing is to imagine you’re at

the bottom of the ocean and you’re

peering into the sea floor from a

profile perspective analogous to as if

you’re holding up an ant farm and

looking through the side and when you

look beneath the seafloor you see

animals burrowing through and excavating

the sediment tubes being formed and

destroyed at the sea floor surface and a

number of physical and chemical changes

occurring in the sediment column we can

see from the changing colors in the

sediment that has these animals weave

their way to the sedimentary fabric the

influence and effect that they have on

sediment quality think worms in a garden

to put it into a familiar context so we

know that the sea floor is important but

what are the methods that we employ that

allow us to better study and understand

this environment most of the seafloor

exists at ocean depths that are far

greater than that which we can send a

diver down to and very little ocean

science actually involves physically

sending someone down to the bottom to

overcome the fragility of the human body

the development and application of

remote sensing techniques was a

necessity in order to better understand

this

environment for 150 years we largely

sampled the seafloor bolide

traditionally if we wanted to understand

what was going on with the animals in

the sediment we would have to collect a

sediment grab and lead lines would be

lowered to the bottom and a length of

the line documented to determine the

depth leta pas graffia the seafloor

these methods are reductionist and offer

very poor resolution but advances in

technology have allowed us to make a

more holistic assessment of our seafloor

observations single beam and more

recently multi-beam sonar offer much

higher resolution imagery of the depth

and topography of the sea floor and the

development of a sediment profile

imaging camera or spy cam allows us a

more clear picture of what’s going on

with the animals in the sediment now

I’ve already shown sediment profile

images in this talk but to give you a

better sense of how the system works as

the spy system is lowered to the seabed

a weighted trigger activates the camera

capturing a plan view image of the sea

floor the system continues to the sin

until contacts in the bottom upon

contact tension is released from the

cable allowing a weighted camera prism

to lower and penetrate the sea floor an

undisturbed profile image of the

sediment column is captured allowing

scientists to document biological

activity chemical processes and physical

changes at and beneath the ocean floor a

huge benefit of this technology is that

it allows us to document and observe the

functioning and behavior of the

organisms without removing them from

their habitat the sea floor and when we

do that we’re able to make really

distinct observation about sea floor

help typically healthy sea floors are

characterized by a rust red brown color

that extends deep beneath the sea floor

surface indicating these areas are

oxygen rich and contain large and

diverse life by contrast unhealthy sea

floors

our dark gray black color these areas

contain little to no oxygen lack

diversity and have very little to no

large organisms now I can show you a

graph or table indicating why the sea

floor to the left is healthy and why the

sea floor to the right is unhealthy or i

could couple that data with images and

make that point much more succinctly and

that’s what we do we take our

quantitative data and we paired with

images and we give people a better

understanding about how the sea floor is

functioning when we do that we’re also

able to assess how the sea floor

responds to and recovers from

disturbance this movie is depicting an

area of the sea floor that’s

experiencing was commonly known as an

ocean dead zone or an area of the sea

bottom where there’s little to no oxygen

when oxygen is removed from the sea

floor bacteria take over the bacteria or

the filaments white lines you’ll see

moving through the sediment on the sea

floor surface and on the face plate of

the prism these bacteria thriving during

this ocean dead zone which is

prohibiting larger organism from

surviving and you can tell how happy the

bacteria are by the amount of organic

matter they’re producing which you can

see sloshing down the base plate of the

prism so over time when oxygen returns

to the seafloor these bacteria scurry

back down into the sediment and these

areas we populated by larger organisms

such as worms clams and crustaceans this

profusion of new technology has led to a

flood of data that we can now mine such

as the example at Kersey just presented

well Steve we are after all visual

organisms and the true power of this

technology is that it allows us to

present our work about the seafloor and

a format that everyone understands a

picture now in the past when we would

send our equipment down and explore some

new area of the ocean we would recover

it and then spend weeks months sometimes

even years combing through this data by

hand eventually compiling it together

into thick bound reports like this I

think my friend Steve heat could

recognize that if you’re trying to

explain something about the seafloor to

someone who doesn’t have a PhD in ocean

science this probably isn’t the best way

to do it these are important for

scientists and regulators because it has

information relating to our field

methods complex explanations of

chemistry but when it comes to a

narrative device to tell a story about

our oceans they fall tragically short

and even worse when these documents are

delivered to a client they sit in an

archive on a shelf gathering dust locked

away from people that might be

interested in the information that they

contain I mean I do this stuff for a

living and I don’t want to read this

kersey do you want to write this not in

the least bit I didn’t think so in 1998

one of our Ted for father’s name David

Gallo presented a talk in monterrey

during this talk he showed us some

wonderful video that come from his Elvin

and Jason submersibles he showed us

bioluminescent jellyfish giant sulfur

vents at the bottom of the sea floor

spewing gas from the Earth’s core into

the ocean he showed us giant tubeworms

that colonized these sulfur vents but

one of the really interesting things

that Gallo hit on happened when he was

showing us a 3d reconstruction of the

sea floor and one of his submersibles

driving through it David said that he

wanted to take this seafloor environment

back to the laboratory because right now

we see it in bits and pieces we see the

other a sound or photographs or as video

or as data from a chemical sensor but we

haven’t yet put it together into one

interesting

and that’s exactly what we’re trying to

do instead of seeing the pages from some

report we want to show people the

synthesis of that data because as it

turns out flipping through pages of

report cross-referencing figures tables

different data points and charts that

we’ve printed it’s not the most

intuitive way to explore something as

vast or complex as the sea floor now

we would print maps and use these a

storytelling tool we present them next

to charts and data xand captions and

maybe have a little paragraph next to

explaining something about this map but

so here you see a map of Massachusetts

Bay just north of us and instead of just

placing the data down next to it we’ve

made this map interactive so that I can

click on different areas in it and I can

see where we’ve sampled and I can see

those sediment profile images that

kersey discuss with us earlier in

context I can see the next two

biological chemical geological data I

can even see shipwrecks and I think

that’s pretty cool this sort of

visualization has served as the

workhorse for our analysis team it

serves as the primary storytelling tool

or us to explain our findings to an

audience but it falls short because it’s

too deep and as we know the c-4 is not a

two-dimensional flat surface and

certainly the volume of water that sits

on top of the sea floor is not flat in

fact it’s two miles deep on average

across our globe so what we’ve done here

holds a lot of potential because it

contours and ridges in the ocean it

allows you to see things in three

dimension and make connections that you

might not otherwise do it contains all

the same data that are two dimensional

map did but it allows us to go beyond

that go into the third dimension it

allows us to draw the picture upwards

and talk about the water column it lets

us see temperature differences from the

top to the seafloor it lets us see

changes in salinity which is essentially

the saltiness of the ocean and the

really cool thing about technology like

this is that it’s built using basic and

common building blocks things that you

can find in your web browser so I don’t

need to spend thousands of dollars on an

expensive computer system I don’t need

to buy complicated software licenses I

can just look at it much like Google

Earth

I can just pull up a webpage and see it

I can even bring it up my phone and see

it on the go and if I’m really clever I

can bring it into a virtual reality

framework looks like Kersey’s exploring

the sea floor on the TEDx stage right

now whoa wave of the future dude as you

can see this is a truly immersive

experience this is important because we

can now put our data in the hands of the

interested citizen no longer are we

content to allow our efforts to sit on a

shelf and collect dust that information

can now be made public for anyone

interested to explore for themselves

bringing a dark and mysterious world

into clear focus wherever you are we

love showing people this habitat but

bringing them down to the bottom of the

ocean in person is an expensive and

dangerous endeavor and it’s likely most

of us are not going to go there but now

i’m proud to say that by using advances

in technology we can bring that

mysterious ecosystem back up to you

thank you very much [Applause]

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