Allison Dawn, GEMM Lab Master’s student, OSU Department of Fisheries, Wildlife and Conservation Sciences, Geospatial Ecology of Marine Megafauna Lab 

In last week’s blog, GEMM Lab postdoc Dawn Barlow discussed the uncertain future of upwelling response to climate change and how findings from the Shanks et al., 2009 “Paradigm lost? . . .” study implies that nearshore systems are likely decoupled from offshore upwelling processes. In a follow up to that paper, Shanks and co-authors found that the heterogeneity of coastline morphology (i.e., rocky or sandy) across several Oregon nearshore study sites explained zooplankton retention differences. Indeed, not only are there differences between offshore and nearshore upwelling dynamics, but there are also site-specific factors to consider when it comes to understanding changes in zooplankton retention along the Oregon coast (Shanks et. al, 2010).

I spend a lot of time thinking about what drives the variability in abundance and distribution of zooplankton prey of gray whales at our Port Orford study site over our long-term study period (2015-2022). For this blog, I want to briefly touch on a few interconnected dynamics in this nearshore PCFG gray whale foraging site that may affect their prey availability. Specifically, the interplay between shoreline topography, temperature, and habitat complexity. 

Interplay between shoreline morphology and thermal fronts

Several years before the “Paradigm lost? . . .” paper, Shanks led a study that investigated how holoplankton (a group of plankton in which mysids and amphipods belong) retention varies across three sites near Cape Arago and one site in Port Orford (Shanks et a., 2003). Here the authors noted that the Port Orford Bight causes an “upwelling shadow”, which is a region of water protected from upwelling-favorable winds. This shadow results in a small-scale warm water feature in the lee of the Port Orford Bight, which may serve as an important retention and recirculation zone for primary productivity (Graham et al., 1997). Discovering this “upwelling shadow” was not the intention of this paper, so the depth and breadth of the warm water plume within our study area has yet to be mapped (see Figure 1 for another West Coast example). However, “upwelling shadows” can act as convergence zones associated with greater zooplankton biomass (Morgan & Fisher, 2010; Ryan et al., 2010, Woodson et al., 2007) and thus may be an important feature to consider in our spatial analyses of drivers of prey availability to gray whales in our Port Orford study region.

Figure 1. Example of an “upwelling shadow” in Monterey Bay. Remotely sensed oceanographic convergent zones (top panel) and sea surface temperature (SST; lower panel) changes over time: a) Sept 8th 2003, b) Sept 2nd 2004, c) Sept 26th 2004, and d) May 31st 2005. Each time period demonstrates that the lee side of Point Año Nuevo is consistently warmer than the surrounding area. Figure source: Ryan et al., 2020.

Habitat complexity: rugosity and kelp

Not only could the unique shoreline in Port Orford contribute to zooplankton aggregations, but the subtidal marine environment is characterized by a range of unique habitat types: rocky reef, kelp beds, and sandy bottom habitat. Structural habitat complexity has been well documented in coral reef systems to be strongly linked with zooplankton prey availability and biodiversity of planktonic grazers (Richardson et al., 2017; Darling et al., 2017; Kuffner et al., 2007; Gladstone, 2007). Structural complexity can be measured in various ways, but quantifying rugosity (or surface “roughness”) is a widely accepted approach. However, only a few studies have demonstrated predator response to rugose habitats in Oregon nearshore rocky reefs (Rasmuson et al., 2021), and there is a dearth of knowledge linking rugosity to marine mammal predation (Cimino et al., 2020). 

Rugosity serves several purposes in the marine environment. A rugose habitat creates micro-habitats for predator evasion, provides greater surface area for kelp recruitment (Cruz et al., 2014; Toohey et al., 2007), and generates turbulence that circulates vital micronutrients for filter-feeding zooplankton and ultimately drives foraging effort at fine scales (Ottersen et al., 2010). 

Figure 2. Example images of habitat rugosity as measured by SCUBA transects. A) High-relief coral habitat with B) quantified depth (m) over transect seconds (10 seconds = 1 meter) and C) Low-relief coral habitat with D) quantified depth (m) over transect seconds (10 seconds = 1 meter). Figure source: Dustan et al., 2013.

Rugosity-generated turbidity might also help explain the zooplankton abundance variation we see across our sampling stations in Port Orford. In Lisa’s recent work showing evidence for a trophic cascade, a decline in bull kelp is overall strongly linked to a decline in zooplankton and gray whale foraging in Port Orford. However, there are sampling stations that, despite a significant loss in kelp, still had an abundance of mysids and hosted gray whale feeding activity in 2021 and 2022. Could this mean that those rocky reef stations, which are more rugose than the sandy bottom habitats, produced enough turbulence to support zooplankton prey? This hypothesis is consistent with several studies that found kelp abundance becomes less relevant with increasing habitat complexity (Trebilco et al., 2016; Anderson, 1994; Choat & Ayling et al., 1987; Larson, 1984). 

There certainly may be other physical or oceanographic factors that create turbidity at these stations. However, as my REU mentee Zoe Sax has been investigating, we think that turbidity could be a metric of primary productivity, which supports zooplankton growth. 

Figure 3 is a map of the average secchi disk values, which provide us with a measure of turbidity (the deeper we see the disk the less turbidity) in 2021 at our 12 sampling stations and their relation to kelp cover. 

Last year was a low kelp year, but Mill Rocks still had a few bull kelp canopies. In Mill Rocks where there was rocky reef with kelp, we see secchi values were low (meaning turbidity was high). This is in contrast to the areas in the sandy bottom regions (no kelp, low rugosity: specifically MR16, TC4, TC6, and TC10) with the lightest values, meaning low turbidity. 

Then, in Tichenor Cove specifically, we see that station TC1 has very little kelp but high turbidity; interestingly this site was a favored foraging spot for gray whales in 2021 and happens to be the closest station to the “upwelling shadow” I described earlier. I hope to conduct rugosity measurements in the near future so we can investigate these linkages further.

Figure 3. Map of two study sites, Tichenor Cove and Mill Rocks, with twelve sampling stations in Port Orford, OR and their average secchi disk values (meters) in 2021. Kelp abundance shown in light green polygons. 

Conclusion

This focus on topography, temperature, and habitat complexity to understand zooplankton variation does not discount that upwelling is an important factor for Oregon nearshore ecology. Menge & Menge 2013 found that upwelling accounted for ~50% of ecological variance in rocky intertidal regions. However, these findings occurred across large spatial areas of about 100 km, while our TOPAZ  sampling in Port Orford is on a much finer scale. Variation in ecological patterns at different, hierarchical scales are well-documented (Levin, 1992; Ottersen et al., 2010). Uncovering the “mosaic of processes”, as Shanks et al., 2003 describes, that drives nearshore zooplankton dynamics is equally challenging as it is fascinating, and I look forward to sharing more results from my Master’s work soon.

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References

Anderson, T. W. (1994). Role of macroalgal structure in the distribution and abundance of a temperate reef fish. Marine ecology progress series. Oldendorf, 113(3), 279-290.

Choat, J. H., & Ayling, A. M. (1987). The relationship between habitat structure and fish faunas on New Zealand reefs. Journal of experimental marine biology and ecology, 110(3), 257-284.

Darling, E. S., Graham, N. A., Januchowski-Hartley, F. A., Nash, K. L., Pratchett, M. S., & Wilson, S. K. (2017). Relationships between structural complexity, coral traits, and reef fish assemblages. Coral Reefs, 36(2), 561-575.

Dustan, P., Doherty, O., & Pardede, S. (2013). Digital reef rugosity estimates coral reef habitat complexity. PloS one, 8(2), e57386.

Gladstone, W. (2007). Selection of a spawning aggregation site by Chromis hypsilepis (Pisces: Pomacentridae): habitat structure, transport potential, and food availability. Marine Ecology Progress Series, 351, 235-247.

Graham, W. M., & Largier, J. L. (1997). Upwelling shadows as nearshore retention sites: the example of northern Monterey Bay. Continental Shelf Research, 17(5), 509-532.

Kuffner, I. B., Brock, J. C., Grober-Dunsmore, R., Bonito, V. E., Hickey, T. D., & Wright, C. W. (2007). Relationships between reef fish communities and remotely sensed rugosity measurements in Biscayne National Park, Florida, USA. Environmental biology of fishes, 78(1), 71-82.

LARSON, R. J., & DeMARTINI, E. E. (1984). SAN ONOFRE, CALIFORNIA. Fishery Bulletin, 82(1-2), 37.

Levin, S. A. (1992). The problem of pattern and scale in ecology. Ecology, 73(6), 1943-1967.

Londoño Cruz et al. (2014) Londoño Cruz E, Mesa-Agudelo LAL, Arias-Galvez F, Herrera-Paz DL, Prado A, Cuellar LM, Cantera J. Distribution of macroinvertebrates on intertidal rocky shores in Gorgona Island, Colombia (Tropical Eastern Pacific) Revista de Biología Tropical. 2014;62(1):189–198. doi: 10.15517/rbt.v62i0.16275

Menge, B. A., & Menge, D. N. (2013). Dynamics of coastal meta-ecosystems: the intermittent upwelling hypothesis and a test in rocky intertidal regions. Ecological Monographs, 83(3), 283-310.

Morgan, S. G., & Fisher, J. L. (2010). Larval behavior regulates nearshore retention and offshore migration in an upwelling shadow and along the open coast. Marine Ecology Progress Series, 404, 109-126.

Ottersen, G., Kim, S., Huse, G., Polovina, J. J., & Stenseth, N. C. (2010). Major pathways by which climate may force marine fish populations. Journal of Marine Systems, 79(3-4), 343-360.

Rasmuson, L. K., Blume, M. T., & Rankin, P. S. (2021). Habitat use and activity patterns of female deacon rockfish (Sebastes diaconus) at seasonal scales and in response to episodic hypoxia. Environmental Biology of Fishes, 104(5), 535-553.

Richardson, L. E., Graham, N. A., Pratchett, M. S., & Hoey, A. S. (2017). Structural complexity mediates functional structure of reef fish assemblages among coral habitats. Environmental Biology of Fishes, 100(3), 193-207.

Ryan, J. P., Fischer, A. M., Kudela, R. M., McManus, M. A., Myers, J. S., Paduan, J. D., … & Zhang, Y. (2010). Recurrent frontal slicks of a coastal ocean upwelling shadow. Journal of Geophysical Research: Oceans, 115(C12).

Shanks, A. L., McCulloch, A., & Miller, J. (2003). Topographically generated fronts, very nearshore oceanography and the distribution of larval invertebrates and holoplankters. Journal of Plankton Research, 25(10), 1251-1277.

Shanks, A. L., & Shearman, R. K. (2009). Paradigm lost? Cross-shelf distributions of intertidal invertebrate larvae are unaffected by upwelling or downwelling. Marine Ecology Progress Series, 385, 189-204.

Shanks, A. L., Morgan, S. G., MacMahan, J., & Reniers, A. J. (2010). Surf zone physical and morphological regime as determinants of temporal and spatial variation in larval recruitment. Journal of Experimental Marine Biology and Ecology, 392(1-2), 140-150.

Toohey, B. D., Kendrick, G. A., & Harvey, E. S. (2007). Disturbance and reef topography maintain high local diversity in Ecklonia radiata kelp forests. Oikos, 116(10), 1618-1630.

Trebilco, R., Dulvy, N. K., Stewart, H., & Salomon, A. K. (2015). The role of habitat complexity in shaping the size structure of a temperate reef fish community. Marine Ecology Progress Series, 532, 197-211.

Woodson, C. B., Eerkes-Medrano, D. I., Flores-Morales, A., Foley, M. M., Henkel, S. K., Hessing-Lewis, M., … & Washburn, L. (2007). Local diurnal upwelling driven by sea breezes in northern Monterey Bay. Continental Shelf Research, 27(18), 2289-2302.

Imogen Lucciano, Graduate student, OSU Department of Fisheries, Wildlife, & Conservation Sciences, Geospatial Ecology of Marine Megafauna Lab.

One year ago, I packed up my 11-year-old daughter, Mavis (for the purposes of this blog, I’ll refer to her as “my sidekick”), our two dogs, and all our books and we moved to Oregon. I was thrilled to arrive and begin my graduate studies in cetacean ecology and bioacoutics with the GEMM lab and the Marine Mammal Institute. It has not been an easy set of tasks to achieve high standards in graduate school while maintaining a constant presence as a single mother, but I am honestly having the time of my life. I am involved in an amazing graduate program and I get to do it with my sidekick cheering me on and making my life feel very whole. This is why I am excited to write this blog reporting on the progression of my thesis and the incredible animals that I have the pleasure of studying: the fin whale.  

Fin whales (Balaenoptera physalus) are the second largest cetacean on the planet and are present in nearly all temperate and polar oceanic regions of the world (1). For my master’s thesis, I will focus solely on the fin whales within a detectable range of our team’s research area off the Oregon coast. In the Northern Hemisphere, fin whales are known to grow up to 23 meters in length and weigh up to 40-50 metric tons (2). They have a slender profile and can be further identified by their hook-shaped dorsal fin in addition to a V-shape on their back referred to as a “chevron” (Fig. 1). Fin whales are a baleen whale in the rorqual family, which have adapted lunge feeding as their primary foraging method (3). This species of whales is also classified as endangered (1), making them a key focal species for research in our modern times of shifting conditions in ocean environments.

Although I am working to correlate the acoustic detections of fin whales across space and time with environmental drivers (like temperature and chlorophyll concentration), as an aspiring cetacean bioacoustician, one of my other burning related questions is: How can fin whale vocalizations be utilized to differentiate populations across the oceans? Perhaps my analysis of fin whales off the Oregon coast can contribute to the pool of researchers studying this species worldwide to help understand drivers of fin whale vocalization variability.

Fin whales can travel great distances, yet their unique vocal renditions of repetitive pulse calls at either a 20 Hz or 40 Hz frequency have geographic patterns (4). These renditions are stereotyped by inter-pulse interval (IPI), which is the rate at which the pulses are detected (5). What’s even more interesting is that unlike many other large baleen whale species, there is little evidence of seasonal behavior and vocalization patterns (5) (Figs. 2 & 3). This suggests that fin whales might not make repetitive annual migrations to accommodate foraging and reproduction. Are these animals prey driven with exemplary senses for finding prey over incredibly large distances in the ocean? Are fin whales consistently present off the Oregon coast? What are their names? Bob, Lucinda, Frederick? There is much to ponder here.

This past summer the Holistic Assessment of Living marine resources off Oregon (HALO) team recovered its first six months of continuously collected acoustic data from three hydrophones moored at designated source locations off the Newport coast. Around the same time, I transplanted my sidekick and myself in Ithaca, New York for the summer, so I could spend my summer days learning to identify and log baleen whale calls among other acousticians at the K. Lisa Yang Center for Conservation Bioacoustics at Cornell University. This work would contribute to my preparation for the analysis of the HALO acoustic data.

I was less than a month into this work when my sidekick ended up spending an entire week with us in the lab because the counselors at her summer camp all caught COVID-19. My sidekick is a dedicated book worm and had no problem keeping herself busy while we all worked, however, she is young and vivacious and so she would often share her music and jokes with the group. I recall (with an uncontrollable smirk on my face) one of her songs called the “Oof” song (Video 1), that is literally a repetitive beat with the onomatopoeia, “oof” being played over and over again. When it started playing I looked up from my computer to see a row of researchers sitting next to Mavis all bobbing their heads to the repetitive tone of “oof”, a tone that hilariously reminded us of a sped-up version of the repetitive pulse of fin whale song. From that point on, “oof” has involuntarily become a part of our language among this group of acousticians.

The summer blazed by, Fall is here, and my sidekick and I are back in Oregon. I am in the process of organizing our collected HALO data to accommodate analysis of baleen whales, including fin whales. At this point I am already able to see fin whale calls in our data (Fig. 4). Subsequently, I will spend the next few months analyzing these data to determine the patterns of fin whale calls over time at our three observation sites (on the shelf, the shelf edge, and off the shelf). Within this analysis I will also look to define the vocal repertoire of fin whales over our six-month study period, which will allow me to report on the frequency where they are primarily detected and the IPI with which the pulses occur.

Moving forward, the HALO team will continuously retrieve and replace the three hydrophones to collect our acoustic data, returning a rich long-term dataset of the study area. I am eager to learn whether the fin whale IPI will remain the same in this location or show changes according to shifts in upwelling or seasonally, assuming they remain in the Northern California Current and do not migrate away. I will continue to assess the acoustic patterns of fin whales over the next year to describe their distribution patterns. All the while with the “oof” song stuck in my head and with my vivacious book worm head banging in the background.

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References

(1) Fin Whale. NOAA Fisheries. https://www.fisheries.noaa.gov/species/fin-whale.

(2) Aguilar, A. & Garcia-Vernet, R. 2018. Encyclopedia of Marine Mammals, Third Edition: Fin Whale, Balaenoptera physalus, Pg 369-371. Academic Press, ISBN 978-0-12-804327-1.

(3) Shadwick, R. et al. 2019. Lunge feeding in rorqual whales. Physiology, 34: 409-418. https://journals.physiology.org/doi/epdf/10.1152/physiol.00010.2019.  

(4) Oleson, E. et al. 2014. Synchronous seasonal change in fin whale song in the North Pacific. Plos ONE, 9 (12). https://doi.org/10.1371/journal.pone.0115678.

(5) Morano, J. et al. 2012. Seasonal and geographical patterns of fin whale song in the western North Atlantic Ocean. The Journal of the Acoustical Society of America, 132 (1207): 1207-1212. https://doi.org/10.1121/1.4730890.

(6) Helble, T. et al. 2020. Fin whale song patterns shift over time in the central North Pacific. Frontiers of Marine Science, 2 (Marine Megafauna). https://doi.org/10.3389/fmars.2020.587110.  

(7) Weirathmueller, M. et al. 2017. Spatial and temporal trends in fin whale vocalizations recorded in the NE Pacific Ocean between 2003-2013. Plos ONE, 12 (10): e0186127. https://doi.org/10.1371/journal.pone.0186127.

Allison Dawn, GEMM Lab Master’s student, OSU Department of Fisheries, Wildlife and Conservation Sciences, Geospatial Ecology of Marine Megafauna Lab 

The 8th year of Port Orford Gray Whale Foraging Ecology Project (TOPAZ/JASPER) has come to an end and it feels truly bittersweet. Last Friday, the team hosted our annual community presentation to close out the project and I was filled with pride to see them confidently convey all they learned over this summer to an audience of family, friends, and community members.

Figure 1: Team B.W.E poses for the annual team photo after the community presentation alongside Tom Calvanese (field station manager) and Lisa Hildebrand (previous project lead). 

I am amazed by all that you can accomplish in one summer, especially with an enthusiastic and adaptable team. I’ve compiled a “by the numbers” table (Fig. 2) that summarizes our hard work this season. 

Figure 2: Port Orford Gray Whale Forage Ecology (GWFE) field season 2022 by the numbers.

Every Spring, the GEMM lab works diligently to hire a solid team of students for this project, which just finished its 8^th consecutive year. These students are initially total strangers who come together to live and work at the Port Orford field station on a project that is as physically and mentally tasking as it is rewarding. Although attention to all the daily details is critical, without a genuine desire to form strong connections and learn from each other – the real “glue” for teamwork – this project would not be as successful as it has been. Like the teams before them, team Big Whale Energy (B.W.E.) started off with little to no gray whale knowledge, sea kayaking experience, zooplankton ID, theodolite operation, or other skills that this project demands. The learning curve required of these students in such a short time is steep, but each year these bright, young scientists prove that with patience, determination, and a positive mindset you can gain not only valuable skills but lifelong connections. 

I also experienced a learning curve as this was my first year leading the project solo. While Leigh and Lisa trained me well last year, and were always a phone call away, there are certain skills that can only truly be honed with experience, many of which must be learned through the inevitable curve balls each new field season brings. During the six week project, Team B.W.E. grew as individuals and as a team as we encountered every challenge with a positive mindset and creative adaptation – from learning new knots to secure our downrigger line, to creating new songs while patiently watching for whales. I know I speak for all of us when I say we are so grateful for everything this 2022 field season experience has taught us about both the process of scientific research and ourselves.

During our community presentation, Leigh wonderfully conveyed how informative and exciting long term data sets can be, especially because 8 years is long enough for us to begin to observe cycles. We have been able to observe cycles in both the ecological changes in Port Orford and in the succession of students who have taken part in the project. Last year, the ecological habitat suitability seemed to have reached a new low, while this year we have seen more kelp and an uptick of whale activity as compared to 2021. We are hopeful this change is indicative of an ecosystem recovery. The cycle of returning project leads and previous interns (both virtual and in person) allows for a meaningful interchange of wisdom, memories, and excitement for the future of this project.

Figure 3: Mosaic of memories for Team B.W.E.

Thank you Team B.W.E. for helping me grow as a leader, contributing to the GEMM lab legacy, and making the 8th year of this project a great success. 

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By Charlie Ells, incoming freshman, Environmental Science major, College of Arts & Sciences at University of Oregon, GEMM Lab intern

Hi! My name is Charlie Ells and I’m an intern at the Port Orford field station. I’m part of the 8th Gray Whale Foraging Ecology Research Team, named this year Team B.W.E (Big Whale Energy!)

Figure 1: Logo I made for the team using Canva. 

The inspiration for our team name originated when the cliff team first spotted a whale named Buttons. Luke, another intern, saw Buttons through the Theodolite and said that he had “Big Whale Energy.” Luke was correct. Pictured below is Zoe, a fellow intern whose blog you might have read a couple weeks ago, and Buttons, an adult gray whale who surprised us both when he appeared out of nowhere behind us while in the kayak. The image doesn’t do him justice, but Buttons is absolutely awesome (and I mean that in the literal definition of the word). Buttons is huge; when he surfaces, it is almost like he is showing off. Buttons pulls a lot more of his body out of the water than seems necessary. His blows are deafening, sounding like an 18-wheeler’s brakes applied with full force. He often exhibits a behavior called ‘sharking’, which is when a whale turns on its side on the surface, bringing a part of their fluke out of the water (see GEMM lab video of sharking behavior). The behavior helps gray whales feed in shallow areas, and was named so because someone thought the whale’s fluke looked like a shark’s fin.

Figure 2: Kayak team gets a surprise visit by Buttons. No craft, whether it has a motor or not, should get this close to a whale. See this GEMM lab website with vessel guidelines and more information. In this case, we had seen Buttons at a safe distance (>100 yards) moments before, and moved in the opposite direction we had seen him going to avoid disturbing him. But Buttons had other plans.

Not only does B.W.E apply to the large whale that Buttons is, but it also encapsulates how much more whale activity we’ve seen this year compared to last year. So far, we have over 17 hours of whale observation time this season, which is 15 hours more than the team had in total last year. We’ve ID’d three unique whales using our study area, learned about some of them on the IndividuWhale website, and collected some great behavior data. Meet Rugged, the first whale I ever photographed. She’s young, and a bit smaller than the other adults, but she’s full of personality (to the extent that we can observe a whale’s personality, anyway). 

Figure 3: Rugged. Photo taken from the beach.

Figure 4: Rugged shows us her fluke as she dives behind the jetty.

Rugged likes to feed for a relatively long time; while some whales have searched and left quickly, she often hangs around the foraging grounds for hours. When Rugged travels, she tends to fluke, meaning she brings the end of her tail out of the water (Figure 4), pretty often. She sometimes blows three times in a row, and spends more time at the surface than others typically do. Look closely at Figure 3 and you can see a propeller scar, which is sadly new this year but at least these identification marks help us spot her more easily. So far, Rugged has been a regular customer at this season’s Mill Rocks buffet, where she feasts on a variety of zooplankton. We’ve seen her the most frequently of any whale this season, and when she shows up, she can be counted on to stick around and offer us the opportunity to collect a lot of nice whale behavior data.

My favorite part of the TOPAZ project data collection efforts are the photographs of whales I’ve captured. The camera is my favorite piece of our gear, and since using it so much this summer I’ve been seriously considering investing in one for myself. For any photography nerds, the camera is a Canon EOS 90D with a 400mm telephoto lens and auto-stabilization. Using this camera on challenging subjects, like a whale that can travel over a kilometer in a couple minutes, has taught me a lot about photography. I’ve learned a lot of situation-specific tricks as well as some general knowledge I’d like to share. I found that using such a long lens can introduce enough camera shake to ruin a shot. To prevent this, simply cranking the shutter speed up does wonders. In the main menu, I change the shutter speed to something like 1/1000, which means the shutter is open for 1/1000th of a second, minimizing the effect of the shake. I’ve also discovered that with a subject that is only in frame for a second (such as a whale), there just isn’t enough time to manually focus the camera before it’s gone. There are two solutions here: rely on auto-focus, which is fine with this camera, but might not be sufficient on others, or use manual focus before your subject is in frame. This second trick has helped me get much better whale pictures than when I first started this internship, and I use it all the time now.

Capturing these pictures of the whales is a thrilling process. First, the wait. Second, the moment of panicked excitement when someone spots a blow. Third, the breathless callouts of where the whale is and the direction it’s heading. Fourth, the mad scramble to get the whale in frame, in focus, and open the shutter in the few seconds before it returns to the depths. This last step is tough — I end up with more photos of empty water, rocks I mistake for the whale, and blurry nothingness than usable ID photos. But when I do end up with a good picture, it’s a great feeling. 

Figure 5: My best picture yet. This is Rugged, showing off what my teammates have dubbed “RainBlow.” 

Figure 6: Dotty, the third whale we ID’d this season. I hustled to the Battle Rock shoreline to get a better angle of this whale, as the sun was causing too much glare from the Cliff site to obtain a good ID photo.

This internship has affirmed my favorite part of conservation, which is the blending of science and art to inform and inspire. One of the things that first got me into science, besides my excellent science teachers, was watching YouTube videos. People like Mark Rober, Steve Mould, Veritasium, and Physics Girl take the scientific process and turn it into creative, accessible, and understandable videos. These artists and scientists have gifted me so much inspiration, which I personally think is one of the most valuable things you can be given. Inspiration can propel you forward, motivate you, and help you take those first steps towards your goal. This internship has propelled my first steps (via kayak strokes) toward my career goals. I’m looking forward to taking these lessons with me as I go off to U of O to study Environmental science. I created the video below in an attempt to capture our work, show off some highlights, and give people the same inspiration that I was given. I hope you enjoy it. This is Team Big Whale Energy, signing off!

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By Luke Donaldson, incoming OSU freshman, Department of Forestry, GEMM Lab intern

When I was a toddler, my grandma took me to the Face Rock viewpoint in Bandon, Oregon during summer to look for migrating whales. Even though we never spotted a blow or fluke, it was a great memory, one that helped spark my ever-growing interest in biology and the environment.

As soon as I was old enough, I volunteered to help scientists at the South Slough National Estuarine Research Reserve (SSNERR) work on a variety of research projects, including European green crab (Carcinus maenas) removal in the Coos Estuary. The removal process of the invasive European green crabs from the Coos estuary is similar to current culling efforts of purple sea urchins (Strongylocentrotus purpuratus) by the Oregon Kelp Alliance (ORKA) of here in Port Orford. Both efforts hope to reduce the negative ecological impacts caused by a lack of natural predators on the Oregon coast. Without natural predators, green crabs and sea urchins dominate food sources and reproduce exponentially in their respective ecosystems. In Port Orford, the decline in population of several species of sea stars since 2013 has led to an abundance of sea urchins, an estimated 350 million alone at Orford Reef (Sommer & Kastelnik, 2021). Read Lisa Hildebrand’s blog for more information about how the cycles of potential phase shifts between sea urchins and kelp impact both the ecology and economics along the Oregon coast. 
In addition to collecting long term data on gray whale activity and zooplankton abundance, the TOPAZ/JASPER projects have accumulated a yearly inventory of bull kelp canopies in order to record biogeographic changes and monitor areas of concern related to urchin abundance.

After multiple opportunities to hone my skills on the theodolite during our two training weeks, I spent several hours at our cliff observation site helping map kelp beds (read more about the theodolite and its purposes in Nichola’s recent blog). Not only does operating the theodolite require practice and careful precision, but weather also poses a challenge to mapping the surface expression of kelp effectively. Sunlight itself strains the eye and causes a glare in the theodolite objective lens. Wind gusts, tidal changes and swell can all distort kelp patches, so consistent timing is essential. Some areas of Tichenor Cove and Mill Rocks are obstructed by sea stacks, vegetation, and man-made structures, so for these areas we use a Garmin GPS to mark waypoints via kayak to create the perimeter of each kelp patch. With over 1,500 fixes and 120 kelp patches mapped, it was our first formal assessment of kelp this year within our two study areas, Tichenor Cove and Mill Rocks (Figure 1). While kelp cover in Tichenor appears to have increased a little since 2021, the kelp in Mill Rocks shows a great recovery.

Not only is the kelp different between study years and areas, but our zooplankton catches are also showing signs of recovery. The large kelp beds of Mill Rocks support a sustained population of zooplankton, unlike in 2021 or in Tichenor Cove. Last year’s GEMM lab intern Damian Amerman-Smith noted the decline of kelp also appeared to correlate with decreased zooplankton abundance and gray whale foraging activity in Port Orford. However, not only does Mill Rocks yield higher amounts of zooplankton this year, but their average size, especially the mysid Holmesmysis sculpta, appears larger this year than in 2021.  

Consequently, this increase in food availability may be the cause of our higher frequency of gray whale observations in Mill Rocks this year. Despite the continued abundance of sea urchins in our study areas, I am optimistic that the current amount of kelp compared to past year’s data might be indicating a recovery of the ecosystem (Figure 2).

The first gray whale that we observed this year was consistently foraging within the kelp beds of Mill Rocks, which was very encouraging for our team. Through this internship I have learned many interesting things about kelp, including how kelp supplies more than just primary productivity, but also a wide range of services directly and indirectly to gray whales. In addition to being a foundation species of Oregon’s coastal ecosystems, bull kelp specifically provides zooplankton with nutrient-rich detritus, protection from predators, and a buffer from strong ocean currents (Schaffer & Feehan, 2020). Kelp provides gray whales not only with habitat for their prey, but keeps them hygienic as well. Gray whales have been observed “kelping”, where they brush against kelp with their skin like a loofah (Morris, 2016). Although kelping is relatively under-investigated, there are claims that this behavior can double as another foraging method (Busch, 1998). When swimming through kelp, gray whales may scrape off tiny crustaceans clinging to the kelp fronds. It has also been noted that gray whale mothers will hide their calves in kelp to conceal them from predators (Busch, 1998).

Ask anyone who has been to Port Orford and they will attest to the abundance and diversity of marine fauna that thrive in the nutrient-rich coastal waters. I hope this will continue, and that we will see a stable bull kelp canopy kelp ecosystem return here in Port Orford. Stay tuned for more results when the team maps kelp canopies again at the end of August!

Figure 3. Kayak sampling at a large patch of kelp in Mill Rocks. Photo credit: Nichola Gregory

This Gray whale foraging ecology (GWFE) internship has prepared me for college in many ways. Being able to study this dynamic ecosystem is any marine science intern’s dream; and, my decision to pursue Natural Resources as my major has been affirmed through this summer’s field and lab experience. It inspires me to focus on ecology and possibly attend graduate school in the future. The college-like environment of living at the field station has conditioned me for dorm life in the fall; and, the opportunity to meet leading experts in a variety of marine science fields has expanded my knowledge of possible career pathways. With the inspiration and guidance of Dr. Leigh Torres, field station manager Tom Calvanese, team leader Allison Dawn, and the rest of the whale team, I am excited to begin my journey as a natural resource student and future scientist.

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References

Busch, R. (1998). Gray Whales: Wandering Giants. Orca Book Publishers.

Feehan, C. J., Grauman-Boss, B. C., Strathmann, R. R., Dethier, M. N., & Duggins, D. O. (2017, October 25). Kelp detritus provides high-quality food for sea urchin larvae. Association for the Sciences of Limnology and Oceanography. Retrieved August 13, 2022, from https://aslopubs.onlinelibrary.wiley.com/doi/10.1002/lno.10740

Kastelnik, T. (2021, August 18). Kelp. Oregon Kelp Alliance. Retrieved August 10, 2022, from https://www.oregonkelp.com/

Morris, A. (2016, October 17). We Can’t Kelp But Smile At This Incredible Humpback Footage. Awesome Ocean. Retrieved August 12, 2022, from http://awesomeocean.com/whales/cant-kelp-smile-humpback-whale-footage/

Schaffer, J. A., Munsch, S. H., & Cordell, J. R. (2020, January 21). Kelp Forest Zooplankton, Forage Fishes, and Juvenile Salmonids of the Northeast Pacific Nearshore. American Fisheries Society. Retrieved August 3, 2022, from https://afspubs.onlinelibrary.wiley.com/doi/10.1002/mcf2.10103Sommer, L. (2021, March 31). In Hotter Climate, ‘Zombie’ Urchins Are Winning And Kelp Forests Are Losing. NPR. Retrieved August 3, 2022, from https://www.npr.org/2021/03/31/975800880/in-hotter-climate-zombie-urchins-are-winning-and-kelp-forests-are-losing#:~:text=In%202013%2C%20 sea%20star%20 wasting,Red%20List%20of%20Endangered%20Species.&text=With%20their%20predator%20largely%20gone%2C%20purple%20urchins%20boomed

By Nichola Gregory, B.S. Earth Science, College of Earth, Ocean, & Atmospheric Sciences, GEMM Lab Port Orford Intern

As a recent OSU graduate from the College of Earth, Ocean, and Atmospheric Sciences (CEOAS), I gained both knowledge regarding oceanographic and biological concepts through my coursework, and also a passion to be involved in projects that work towards bettering the natural world. Currently, I am pursuing a GIS (Geographic Information System) certificate from Portland Community College. The choice to continue my education with this certification was driven by its applicability as well as my desire to equip myself with skill sets that are applicable in addressing questions in marine science. This desire leads to the primary reason I was drawn to the TOPAZ/ JASPER projects that I am fortunate to be a part of this summer. These projects located in Port Orford have allowed me to become more familiar with various softwares and instruments used within marine sciences, and the instrument that I have been most excited to learn more about this summer is the theodolite.

My first introduction to the theodolite was during my biology of marine mammals course in Newport where PhD student Lisa Hildebrand (then Master’s student and graduate student leader of the Port Orford project since 2018) visited us in Depoe Bay with the instrument. That day, I was intimidated yet intrigued by how theodolites work and learned from Lisa that it can be used to create ‘tracklines’ of gray whale movements. 

Now that the 2022 field season is underway, I’ve spent the last couple weeks at the Port Orford Field Station under the guidance of Master’s student Allison Dawn where I have gained familiarity with operating the theodolite (or as we affectionately call it, the Theo). I have also learned how vital of a tool it can be in helping us understand the habits and ecology of PCFG gray whales that visit the Oregon coast. 

Figure 1: Four out of five members of the 2022 team pictured during cliff training. From left to right: Charlie watches whales with binoculars, Zoe learns how to use Pythagoras software for trackline creation, and Allison instructs me on how to use the theodolite. Photo credit: Luke Donaldson

Figure 2: A basic diagram of a digital theodolite. Top “Theo” pictured is facing out toward the object while the bottom “Theo” shows the user side. Diagram credit: Johnson Level & Tool Mfg. Co

Theodolites became popular in the early 1800’s and have been used for land surveying since. They combine optical plummets, a bubble level, and graduated circles to find vertical and horizontal angles while surveying. For a more visual introduction to theodolite and some of its uses, check out this link to a youtube video.  

When the cliff team begins the day, their primary objective is to set up the theodolite and be prepared to track the locations and movements of gray whales. First, the surveying point (which is used to ensure repeatability of station location) is placed on the ground to position the tripod and theodolite. Then, once the tripod is set up and theodolite attached, leveling the instrument takes place. The 3 screws on the base plate of the Theo allow for leveling, which is of utmost importance so that the instrument is perfectly level with the horizon. The Theo has two bubble levelers to promote accuracy while moving the tripod legs as well as the leveling screws. Once the instrument is level, we complete the “start fix”, which is our first data point for each day and used as our reference point. The telescope includes an eyepiece for the user and an objective lens with internal mirrors to magnify the object(s) being viewed. Now we are ready to start fixing whale locations! And while the set up involved with “Theo” can be difficult to remember and tedious (leveling specifically) it has become somewhat automatic after a few weeks of practice.  

After a productive day with many whale fixes, a small map (Figure 3) is made on the associated computer program “Pythagoras”. This map shows the station (“Theo”), the reference point, and the relative location and coordinates of each fix made. The tracklines are then analyzed to learn more about movement and behavior of specific whale individuals (read Lisa’s blog  here for more information!). We also carefully outline kelp patches with many “fixes” so we can create maps of kelp cover in our study areas. This year we are seeing more bull kelp compared to 2021, but stay tuned for more details about these changes from intern Luke Donaldson’s upcoming blog!

Figure 3: An example of a trackline map made in Pythagoras after gray whale fixes are made. This specific trackline shows a whale coming into Mill Rocks to forage, moving past the cliff station toward Tichenor Cove, and then making its way back to Mill Rocks. 

Due to this amazing instrument, the GEMM lab has non-invasively tracked many whales over the many previous field seasons. Two whales that this year’s team has grown particularly fond of are named “Buttons” and “Rugged”. Both have visited Port Orford numerous times over the past couple weeks, giving us the chance to get practice with creating tracklines while also capturing up-to-date ID photos. Buttons is regularly documented along the Oregon coast and is such a local favorite that there is an honorary Port Orford Public Library Card in his name! Rugged also showed up two weeks ago with a brand new marking that is likely a propeller scar. In addition to seeing a greater number of kelp patches, we have already obtained more whale trackline data than the entirety of  last year’s season. I hope this means we are observing a recovering ecosystem, and a positive future for Port Orford, through the lens of the Theodolite.

Figure 4: A photo captured of Rugged, our first whale sighting of the 2022 season. Photo credit: Allison Dawn 

After being in Port Orford for a couple weeks now, with the first few days of proper sampling behind me, I can tell my time here will be time well spent. Not only have I become familiar with a new instrument, I have learned a great deal in how science in the field is conducted and how broad a project can become. Specifically, I am impressed by the volume of data that is collected at the 12 unique kayak sampling stations on any given field day –secchi depth, water depth & chemistry, underwater footage, and zooplankton. These data complement the data cliff team provides, which, in addition to whale movement data, includes Beaufort Sea State, tidal height, and weather. I now appreciate how important it is to gather as much information as possible in order to find connections between the environment, gray whales, and their prey, even if those connections are not obvious to us today. 

Another lesson I’ve found invaluable during this experience is my growing belief in myself and abilities. Prior to this summer, I had minimal experience on the water, mostly limited to rivers and lakes. But after being in Port Orford for a few weeks, I have learned that something that once seemed daunting can become enjoyable. I think almost every young person in science finds themselves in a state of “imposter syndrome” at some point, where despite great education and experiences, they fall short in self confidence. Time spent on the cliff, kayak and lab has helped affirm that marine science is where I belong. Perhaps even more impactful are the experiences I have had while navigating the learning curve of these skills. I hope to keep this growth-mindset and push through future experiences that feel awkward or scary in order to reach my goals and find my place in marine sciences. 

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References

All about theodolites. Levels, Laser Levels and Measuring Tool Mfg Company Johnson Level. (n.d.). Retrieved August 1, 2022, from https://www.johnsonlevel.com/News/TheodolitesAllAboutTheodo

 Leonid Nadolinets, Eugene Levin, Daulet Akhmedov. 12 Jun 2017, Theodolites from:

Surveying Instruments and Technology CRC Press

Retrieved August 1, 2022, from

https://www.routledgehandbooks.com/doi/10.4324/9781315153346-3
NMAH: Surveying & geodesy: Theodolite. NMAH | Surveying & Geodesy | Theodolite. (n.d.). Retrieved August 2, 2022, from https://amhistory.si.edu/surveying/type.cfm?typeid=19