Annie Crawley, the videographer and photographer on SEAPLEX with Project Kaisei, has posted her first video! It looks great, and you can see us in action.
Annie Crawley, the videographer and photographer on SEAPLEX with Project Kaisei, has posted her first video! It looks great, and you can see us in action.
Posted in Media
We’re all decompressing and unpacking and getting used to life on shore. (What? We have to do our OWN dishes?!) But looking at our amazing photos makes the transition to normal life much easier. Check out the SEAPLEX set on Scripps’ Flickr page and the Project Kaisei Flickr (includes photos from the vessel Kaisei as well) for a look back at SEAPLEX highlights.
Here’s some of my favorites:
Assuming that no one suddenly has some extra time and the computers are still set up, this is the last blog from the SEAPLEX cruise. However, please join the Google Group so that we can let you know if there are new blog postings about results or other SEAPLEX related news. Thanks so much for following the trip!
Miriam Goldstein writes:
Last night at around 3 a.m., I was awakened by Lara whispering that the best thing ever was happening outside and that I really, really wanted to get up. I staggered outside in my stripy pajamas and was greeted by fiery bioluminescence erupting from our wake and from each whitecap all the way to the horizon. Above in the perfectly dark sky, the stars mirrored the glowing sea. I have no words for the beauty and the glory of it.
When I was growing up near the Gulf of Maine, my parents cautioned us to never turn our backs to the ocean. They meant that we shouldn’t get caught by surprise by a big wave or a rip tide, but I think this advice should extend to the lovely parts of the ocean as well as the scary parts. The ocean is the cradle of life on Earth, filled with infinite variability, and we’ve only explored a tiny fraction of it. There are so many mysteries to explain, so many depths to plumb. Even the humblest seaside tidepool contains animals barely known to science.
So to all who followed along with SEAPLEX, and who are intrigued by the big, wet, and blue – please don’t turn your backs to the ocean. Perhaps someday missions like SEAPLEX will become obsolete, and ocean science will be done for the sheer joy of discovery instead of the necessity of
understanding what our species has wrought.
But for now, we are landing with three weeks of hard work safely stowed in hard drives and formalin-filled jars, and will retire to our respective labs to understand what exactly we found.
We’ll continue to post sporadic updates to this blog as they occur. Many thanks to all who followed along and commented on our adventures. Many more thanks to our supporters: Scripps Institution of Oceanography at UC San Diego, UC Ships funds, Project Kaisei, Scripps Center for Marine Biodiversity and Conservation, Mullin Fund, and San Diego Association of Women in Science. And the most thanks to the captain and crew of the R/V New Horizon, without whom we would have been truly adrift.
Flying squid are difficult to photograph. However, SEAPLEX did wish to
satisfy the many requests for images of them leaping from the water. You
need to look closely. It honestly does not due the event justice.
Posted in Marine Organisms, New Horizon, People
Our second post today is from Pete Davison.
He writes:
The past two weeks of the SEAPLEX cruise have been spent far offshore in oligotrophic (nutrient-poor) water. In the California Current closer to shore, the nutrients required for plant growth are present in the surface water. This cold, nutrient-rich water has been recently upwelled from the deep by the action of winds blowing south along the coast. The growth of phytoplankton near the surface depletes the nutrients as the water warms up. Primary productivity is a measure of the rate of growth of phytoplankton. It is typically measured in grams of carbon per square meter per day. The carbon comes from photosynthesis as the plants change CO2 to O2 with energy from the sun. The winds eventually push the warmer, nutrient-depleted surface water offshore to the west. The position of the SEAPLEX trawls has been marked on a satellite map of annual primary productivity from our study area in the image below.
Phytoplankton are consumed by zooplankton, which are in turn eaten by larger predators. Changes in the pattern of food availability delineate pelagic habitat changes, and are reflected in the communities of animals that live there. The amount of available food also determines the quantity of animals (biomass) that can be supported in the habitat.
We have been collecting very small volumes of zooplankton and fish at Stations 2, 3, and 4 that correspond to the low productivity of the habitat we are sampling in comparison to Station 1 in the California Current. We have also been catching different species of animals that reflect the new habitat that we are sampling. This is clear in the photo below.
We separate the fish from the zooplankton at sea before preservation because two groups of animals are often studied by different scientists. From the map, annual primary productivity at Station 1 is ~1 gram of carbon per square meter in comparison to ~0.3 grams of carbon per square meter at Station 4. We would expect a ratio of ~3.3 in the catch volume (assuming that the standing stock of animals is equal to annual growth). It can be seen that Station 1 had roughly four times the zooplankton volume and twice the fish volume as were found at Station 4. This is pretty close to our expectations.
Map of primarpy productivity in the Eastern North Pacific Ocean. The SEAPLEX cruise track is overlayed on the map. Station 1 is in the California Current region, an area of high primary productivty. Stations 2, 3, and 4 are in the North Pacific Gyre, an area of low primary productivity.
Samples collected on the SEAPLEX cruise. The samples were divided into zooplankton (left) and fish (right). The jars in the back are from one trawl at station 1 in the California Current. The jars in the front are from a similar trawl (same duration, same speed, same net, etc.) from Station 4 in the North Pacific Gyre.
Posted in Marine Organisms, Science
The SEAPLEX cruise gets into port in Oregon today, where I believe that they are having a press conference. There will be another press conference next week after everyone is back in San Diego.
Our first post today is from Jesse Dubler.
He writes:
What Can Our Readers Do to Make a Difference?
There are many ways to make a difference on this issue of plastic marine debris even though you may never have the opportunity to come out here to the gyre personally. I would encourage our readers to begin by visiting National Ocean and Atmospheric Administration’s (NOAA) excellent Marine Debris 101 website. As an alternative, you may want to check my own specialized clearinghouse that I have been developing over the past year, which focuses on disseminating information specifically related to microplastic marine debris. As this clearinghouse is very much under development, I would definitely welcome additional data not yet posted or volunteers to tackle various aspects under development.
If you would like to do something more tangible, you could check to see if you have a Coastal Cleanup Day event scheduled near you this coming September. In attending this one-day event, you will be joining thousands of other volunteers worldwide to pick up marine debris. You could also volunteer to collect nurdles, also known as industrial preproduction plastic pellets, on your local beach and ship them to Japan where their chemical properties would be analyzed and posted online under the auspices of project
International Pellet Watch.
For those with the business acumen, there may be promise in cleaning up some of the gyre. For instance, there is a possibility under investigation by Project Kaisei to detoxify and liquify the plastic debris into a source of fuel that would ultimately subsidize the clean-up. Further studies of the volume of the debris as well as the behavior of plastics in this area are necessary to better formulate a concrete action plan. That said, there have been instances where debris has been profitably converted into energy as seen with ghost nets in Hawaii and the New England region.
Of course, if you are in the unique position of being able to generate or otherwise provide funding for additional scientific expeditions to study the gyre in Pacific (or any of the other six gyres, for that
matter), such research would be enormously helpful in better understanding this global phenomenon.
Posted in People
Our second blog today is from Jesse Powell.
He writes:
Pop quiz! What’s the largest migration on Earth? Is it the wildebeest of the African plains, or perhaps a marine bird like the sooty shearwater seasonally migrating from New Zealand to North America, or maybe the migration of the gray whales from Baja California to Alaska? In fact it is none of these. The largest migration on Earth, in terms of total biomass migrating, or number of individuals migrating, is the daily migration of plankton and small fishes from depth to the surface and back again. This phenomenon is called diel vertical migration, or DVM for short, and is by far the largest migration on Earth. Each night, plankton and small fishes (aka micro-nekton) come to the surface from a depth of a few hundred meters. They come to the surface to feed on phytoplankton and on other zooplankton. Before day breaks these same zooplankton will descend again to the depths, usually 200 to 800 meters (656 to 2625 feet) below the surface.
Let’s consider a specific case of a copepod 2.5 millimeters (0.1 inches)in length that migrates 350 meters (1148 feet). Three-hundred and fifty meters? I hear you scoffing! Granted it doesn’t sound like a long distance. However, when you realize that 350 meters equals about 140,000 body lengths for a migrating copepod, then you realize that this is equivalent to me walking from downtown San Diego to Santa Barbara every evening for dinner, and then walking back. And migrating plankton do this every day of the year–roughly equivalent to me walking around the world, more than twice, every year! Literally trillions of individual animals participate in this nightly mass migration. Also consider that a significant portion of the ocean’s biomass participates in this nightly migration, so we’re talking about hundreds of millions of tons of biomass. It quickly becomes clear that DVM is larger than all of the other great migrations combined.
Why do they do it? Well, it’s pretty clear that zooplankton and micro-nekton come to the surface layer (e.g. top 100 meters (328 feet) to feed. That’s where the phytoplankton are, and therefore, that’s where most of the food is. But this doesn’t explain why they descend with the coming day. Why spend all that energy moving up and down vast distances when you could simply stay at the surface and gorge on the
all-you-can-eat-buffet? The best answer is predators. During the day, light renders zooplankton and small fishes much more visible to their predators. DVM is an adaptive behavior that probably evolved independently in many taxa, or groups of zooplankton and fishes, over many, many generations. Several interesting corroborating observations support the light/predator hypothesis. First, during a solar eclipse, migrating zooplankton and fishes will start to migrate to the surface, only to turn around when the solar eclipse ends. Tricky! Second, when a parcel of water containing migrating zooplankton passes over a shallow seamount during the day, the zooplankton are unable to descend to darkness, and are consequently massacred by planktivorous fish. A total bloodbath. Finally, and most convincingly, is the observation that in those rare areas where predators are found predominantly at depth during the day, and at the surface at night, the local zooplankton prey will reverse their migration (e.g. reverse-DVM) in reaction to the new predation pressures. So, ultimately, we believe that DVM is driven by predation pressures. I guess I’d walk back to San Diego, too, if there was a strong possibility of me being eaten in Santa Barbara.
I hope you have all found this little diversion into the secret lives of critters interesting! I’ll leave you with a couple pictures from a recent manta net tow. This manta tow was remarkable in that we collected a huge number of zooplankters, and that the sample was composed mainly of only two species of small crustaceans. You can see in the pictures a clear, smaller copepod species, and also a beautiful iridescent blue amphipod. I’ve never seen this amphipod species before. When the cod-end from the manta net came up filled with what looked like blue paste, I was sure that we had captured a big blob of grease or waste. Instead, imagine our surprise when we saw these!
Contents from the cod end of one of today’s manta tows filled with blue amphipods.
Close up of the manta sample. The small clear crustaceans are copepods. The blue ones are amphipods.
Posted in Marine Organisms, Science
The SEAPLEX cruise is almost over! They will be in Newport tomorrow, and then most of the science party will be back in San Diego on Saturday. I am not sure what the fate of the blog will be after the cruise. There definitely will not be daily updates. However, I think that there are plans for the blog to remain active as one way of sharing the information gathered on the cruise with the public, so please continue to check in with us!
Our post today is from Miriam Goldstein.
She writes:
From Walden Pond to the North Pacific Gyre
We’ve left the gyre – the water temperature has dropped several degrees and the wind and waves have kicked up. I’ve had two disappointments today – I’ve had to go back on seasickness medication after a glorious two-week break, and we’ve had to cease sampling in order to make Newport on time. All of a sudden, I’m reduced from frantically processing samples to lying limply on a bean bag chair. This makes me contemplative, and I thought it was time to ask why people care so much about plastic in the North Pacific Gyre.
Most ocean scientists I’ve talked to don’t understand why marine debris compels the public attention. With so much bad news all around – coral reefs bleaching, sharks careening towards extinction – why care about some trash in an isolated part of the ocean that few have even seen? On the practical side, (unlike, say, global climate change), plastic trash doesn’t require any specialized knowledge to understand. Everyone generates trash, and everyone’s seen litter at the beach or in a park. And plastic is also never found in nature, so any plastic floating in the ocean must have been put there by humans.
But I think there’s something more emotional and deeper going on here to generate such strong public interest. Plastic is symbolic of our times. From its advent in the 1950s, plastic has been an integral part of our shiny industrialized lives. Plastic has brought wonderful things like disposable contact lenses and waterproof paper, but plastic has also brought disposable items made from a permanent material. In the United States, people are deluged with cheap plastic consumer goods that aren’t meant to last, but to be thrown out and bought again.
Plastic litter in the middle of the oceanic wilderness is shocking because it makes human impacts on the earth explicit, and violates our idea of what is natural. The ocean is a very alien and unhuman environment, hostile to human life and populated by strange and exotic beasts. So seeing the undeniable action of humans in the midst of the vast unpopulated sea is far more appalling than seeing it in a forest or a field. People want to know that there are wildernesses out there somewhere, and if even the open sea is no longer a wilderness, what is?
Most scientists would probably say that there are no truly wild places left. Humans are mighty – we can trawl every seamount, climb every mountain, and perturb the atmosphere itself. Everything on earth, from the deepest oceanic abyss to the highest mountain, is touched by human influence. But seeing that influence just floating out here in the middle of nowhere makes our power painfully obvious, and the consequences of the industrial age plain. It’s not a pretty sight.
Six of the hundreds of sample jars collected during the SEAPLEX cruise.
The ocean was calm within the North Pacific Gyre, but the swells picked up as the New Horizon heads north to Newport, Ore. on August 19.
Posted in New Horizon, People, Science
Our second post today is from Meg Rippy.
Meg writes:
Hello everyone, Meg Rippy here. I realized recently that I haven’t really described why I’m out here in the North Pacific subtropical gyre, other than a brief mention that I study marine bacteria. Let’s correct that, shall we? First, a bit about marine bacteria. Typically when we think about bacteria we conjure up images of infected wounds, colds, and other unpleasantness. Most bacteria, however, are beneficial. They can be thought of as the recyclers of the ocean because they play an important role in decomposing dead matter, which releases inorganic nutrients that other living organisms need to grow. Without bacteria nutrient concentrations in the ocean would decrease, the phytoplanktonthat form the base of ocean food webs (like plants do in terrestrial systems) would be less abundant, and zooplankton, fish, birds, and mammals would have less to eat. The ocean needs its bacteria folks, so leave the Lysol at home
.
Besides playing an incredibly important role in marine food webs, the bacteria in our oceans are also extremely abundant and diverse. On average there are around one million bacteria living in every milliliter of seawater and no two bacterial species within that milliliter are exactly the same. Efficient recycling of dead matter requires an entire community of bacteria with complementary metabolisms that break down different compounds. Some of these bacteria specialize in the colonization of particulates and some are free living in the water column. A subset of the marine bacteria that specialize in particle colonization are called biofilm formers. They form thick coatings on solid objects. My work on the SEAPLEX cruise directly concerns these biofilming bacteria, which may opportunistically colonize plastic debris as well as organic matter. If these bacteria colonize plastic, then bacterial communities in high plastic areas could contain more biofilm formers than is typical for the open ocean. This could possibly perturb ocean nutrient cycling and/or food webs, but we don’t really know how. The role of bacteria as the ocean’s primary recyclers makes it important for us to find out.
It is also important to point out that some biofilm bacteria serve as cues for the settlement of invertebrates like polychaetes (marine worms) and mussels. In this light, plastic and associated bacterial biofilms could serve as a transport mechanism for coastal invertebrates, bringing non-native (invasive) species into the gyre and possibly to distant shores. Non-native organisms can be extremely problematic for local ecosystems because some invasives survive better than local species and can take over an area, drastically altering the local food webs that depend upon native species. The association between plastics, bacteria, and invertebrate fouling has been one of my focuses these past few weeks. So far we have collected large pieces of plastic from the small boat and smaller pieces via dip netting. The bacterial communities on these plastic pieces will be examined back on shore using genetic analyses that type bacterial groups using known DNA markers. Miriam Goldstein plans to examine the associated invertebrate fouling communities. So far we have already seen mussels, bryozoans, gooseneck barnacles, and an amazing number of small
crabs on our plastic samples. It will be really exciting to combine this information on invertebrate fouling with the bacterial data later this year.
The SEAPLEX team: (front row, left to right) Jesse Dubler, Andrew Titmus, Pete Davison, Doug Woodring, Karin Malmstrom, Miriam Goldstein, Darcy Taniguchi, Meg Rippy, and Chelsea Rochman. (back row, left to right) Timbo Stilliger, Jesse Powell, Mario Aguilera, Jim Leichter, Lara Dickens, Matt Durham, and Josh Jones.
Posted in Marine Organisms, New Horizon, People, Science
All sampling on the SEAPLEX cruise has stopped. They are experiencing some rougher weather (6 feet swells). This means that the ship can’t travel quite as quickly, so they don’t have time to slow down even more to sample if they want to make it to Newport on time. So now, they are packing and anxiously awaiting the time when they will be near enough to shore to have internet access again!
Our first post today is from Darcy Taniguchi.
Darcy writes:
Hello yet again outside world! This is Darcy Taniguchi, writing to you from the R/V New Horizon as our cruise winds down and we head closer to port. After all these blogs, I’m sure you have seen mentioned several times our various standard sampling instruments—the manta net, Matsuda-Oozeki-Hu trawl (aka Oozeki trawl), bongo net, and CTD. I am sure that you have read some of the other information about these pieces of equipment. However, I will use this blog
entry tell you what data we obtained from each one.
First, the manta net. Oh the manta net. This piece of equipment has become sort of the bread and butter for several people on this cruise. It samples at the surface, so it is used to catch particles and organisms which are floating at or very near the surface. In it, we have managed to capture such things as numerous types of crustaceans, gelatinous salps, glowing lantern fish, and, of course, multi-colored plastic pieces.
Next, the bongo net. This instrument is also used to collect zooplankton, just like the manta net. However, it is used to catch organisms deeper in the water. On this trip, the bongo net has been able to catch many little crustaceans, such as the often abundant copepods and krill, as well as glistening comb jellies and perhaps the occasional piece of plastic.
Now, the Oozeki trawl. This is another kind of net, but it is bigger than a bongo or a manta, with a frame about the size of a Smart Car. The target depths to which this equipment is deployed is between 150 and 800 meters (492 to 2625 feet). At these different depths, the net has come up with various types of interesting, sometimes rarely observed, fish, although, there are other (unlucky) organisms which have also been pulled on deck—pyrosomes that exhibit bioluminescence, jellies that you have to squint to see, and squid with googly eyes, to name a few.
Last, but most certainly not least, is the CTD, which stands for conductivity-temperature-depth. The CTD is a real workhorse in oceanography, being used in the realms of marine chemistry and geology, physical and biological oceanography to look at the structure of various properties of the water with depth. Besides the sensors for temperature and conductivity (used to determine salinity), the CTD can also be outfitted with equipment to measure oxygen, light from the surface, fluorescence (from things like phytoplankton), nitrate, and water clarity. These sensors are on a large, cylindrical frame that is also outfitted with special bottles called Niskin bottles. These bottles have caps on either end that are closed with a click of a button at whatever depth the scientists on board wish to snap them shut, thus collecting water from that chosen depth, which is later sampled. Thus, the CTD can provide immediateinformation about the different regions in the ocean described by these variables as well as for the collection of water within regions of interest.
With these different pieces of equipment, we are cooperatively trying to collect various types of organisms at different depths within the ocean, as well as put them in the context of the structure of the water column with depth. These instruments are by no means unique to our expedition but instead are tools which can be and have been used in a wide variety of studies. Nevertheless, we hope that they have done well on this particular cruise in collecting enough information to begin to help us determine what effects, if any, plastic may be having on organisms of the north Pacific gyre.

Captain Wes Hill on the bridge of the R/V New Horizon during the SEAPLEX research cruise.
Posted in Marine Organisms, New Horizon, People, Science
Here are the winning haikus, along with the authors. We didn’t know who wrote which one until after we sent them the results.
TIED FOR 1st PLACE
–Whales spout plastic tears. Behold a New Horizon! Hope dawns with the sun. — Karin Malmstrom
–Happy fish swims free. Meets the deep Oozeki trawl. Sample jar 1-3. — Pete Davison
2nd PLACE
–Along the currents. Drift plankton and trash alike. Our New Horizon. — Matt Durham
TIED FOR 3rd PLACE
–Our strong sturdy ship. Just a mote in a moon beam. In Pacific night. — Jesse Powell
–Steel and mesh descend. With peculiar appetite. Catching aliens. — Josh Jones
Sushi night on the R/V New Horizon
Posted in People
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