This Toxic Tar

Spoiler Alert: Our experiments are showing tar balls washing up on our beaches to be toxic to our local sand crabs.  If you are looking for that info, scroll to the Tar’s Toxicity heading at bottom of this post.  If you want get a brief primer on Ecotoxicology, then start right here…

A brief history of poisons: French Regicide to New York City

Françoise Athénaïs de Rochechouart de Mortemart, marquise of Montespan (5 October 1640 – 27 May 1707), mistress of King Louis XIV of France during Affaire des Poisons from the 1670s to the 1680s.  Image Source: Wikicommons

Françoise Athénaïs de Rochechouart de Mortemart, marquise of Montespan (5 October 1640 – 27 May 1707), mistress of King Louis XIV of France during Affair of the Poisons which ran from 1677–1682.. Image Source: Wikicommons

Our modern understanding of toxins in the western world traces back to the proliferation of targeted poisonings across Europe several hundred years ago.  The Europe of 500 years ago was dominated by monarchies where royal houses typically bred with only a handful of other royal houses.  Only a very select few of those offspring were in turn able to become the ultimate ruler (the king or queen) of kingdom X or empire Y.  Those kings and queens tended to hold their position for life.  Add in the fact that the royal courts and/or church didn’t typically take kindly to a next in line for the throne offing the king or even the apparent or king just so they could move into that anointed position.  Would be rulers were therefore in something of a tight spot.  What was a scheming, covetous, inbred to do?  Cue the dramatic music and the rise of the widely popular art of poisoning your older sister or brother in ever uneventful ways and with ever more creative toxins.  This forerunner of our modern field of toxicology spurred numerous clandestine experts who knew of the right amount of substance X and how to deliver them in unseen ways so as to produce the funeral you desired.  Examples ranged from the tabloid Affair of the Poisons (a huge French scandal spanning 1677–1682 that led to the execution of 36 courtesans) to the more “traditional” politically calculated killings such as that of Moscow’s Dmitry Shemyaka in 1453.

It was all very Game of Thrones-esque.

Alexander Gettler (far right) and Charles Norris (seated, left) in the toxicology laboratory located on the third floor of the City Morgue, Bellevue Hospital circa 1922.  Image source: Wikimedia Commons.

Alexander Gettler (far right) and Charles Norris (seated, left) in the toxicology laboratory located on the third floor of the City Morgue, Bellevue Hospital circa 1922. Image source: Wikimedia Commons.

While medieval courtesan intrigue way over in Europe may seem only tenuously related to our modern field of ecotoxicology, it quite literally laid our foundations.  First and foremost this gave us the central underpinnings of toxic exposure.  This concept would eventually become more widely known now as a Dose-Response Curve.  The idea here is that almost any substance can be lethal in high enough quantities.  The corollary is that any poison can cause you no harm if you get exposed to it in small enough quantities.

The classic Dose-Response Curve began to take on the cloak of scientific rigor with the birth of the modern forensics unit in New York City at the turn of the 20th century.  Alexander Gettler became the first professional forensic toxicologist in the United States, employed by New York City between 1918 and 1959.  Gettler, his boss Charles Norris (America’s first medical examiner to work with rigorous, scientific methods), and their colleagues established a laboratory which (among other things) quantitatively explored the Dose-Response Curves for a wide range of substances.  Much effort went into characterizing toxins via the types of toxic response they manifest in the target organism (see my figure below).  If this is even vaguely of interest to you, I’d HIGHLY recommend The Poisoners Handbook by science writer and Pulitzer-Prize winner Deborah Blum.

Three potential Dose-Response Curves.

Three potential Dose-Response Curves.  The dose (x-axis) could be concentration, frequency of exposure, or length of exposure., The response (y-axis) could be anything from a sublethal outcome such as a headache to outright death.

Rachel Carson holding her ecotoxicological treatise Silent Spring.  Image: Rachel Carson Archives

Rachel Carson holding her ecotoxicological treatise Silent Spring. Image: Rachel Carson Archives

The Dose-Response Curve remained more or less tightly grounded in human (and domestic animal) toxicology for several decades more until Rachel Carson’s landmark 1962 treatise Silent Spring.  That book served as a clarion call for exploring the effect of poisons on non-human elements of our biosphere and the potential wide-ranging effects on entire ecosystems that can emanate from the poisoning of a single population.

By 1970, the French toxicologist Dr. René Truhaut had coined the term ecotoxicology.  Truhaut defined ecotoxicology as.

The branch of toxicology concerned with the study of toxic effects, caused by natural or synthetic pollutants, to the constituents of ecosystems, animal (including human), vegetable and microbial, in an integral context.

Soon ecotoxicology programs began springing up across universities worldwide.  I could go on for pages about the rapid evolution of ecotoxicology since 1970 (the discovery of endocrine disruptors, modern whole-system ecotoxicology, etc.) but that is the subject for a future discussion…

The toxic components of crude oil

Large tar ball just deposited at El Matador State Beach.  June 9, 2015.

Large tar ball just deposited at El Matador State Beach. June 9, 2015.

Crude oil is a complex mixture of dozens and dozens of compounds.  We typically think of the diverse array of hydrocarbons that comprise the “oil” itself, but there can be tons of other things hitching a ride and mixed up in the chemical soup that was hanging out underground for millions of years.  These tagalongs include heavy metals, sulfur, etc. and have their own toxic responses But for now, let’s stick to the basic hydrocarbon components as the variety of chemical structures in there is enough to boggle the mind.

As an aside: In graduate school we used to teach up-and-coming ecotoxicologists about toxicity via a series of labs exploring creosote.  Creosote is the tarry substance that we historically impregnated wood with when we wanted a given post or beam to survive the ravages of structure-damaging organisms (boring worms that attack pier pilings, woodpeckers that attack telephone poles, etc.).  That stuff was always crazy toxic and often sparked long discussions about the rainbow of potential poisonous compounds within the creosote that might be responsible for the toxicity we were observing in our instructional, classroom experiments.  But we always ended up coming back to those good ol’ hydrocarbons when push came to shove.  Those hydrocarbons are some amazingly lethal substances, especially when mixed with sunlight.  But back to the the focus of this post…

Representations of Benzene.  Image: Matthias M., CC BY-SA 3.0

Representations of Benzene. Image: Matthias M., CC BY-SA 3.0

The hydrocarbons in crude oil generally come in one of two flavors: alkanes and aromatics.  Alkanes are the less poisonous of the two and are relatively quickly degraded in the environment by the local microbial community or strong sunlight/UV radiation.  Aromatics (molecules centered around 6-carbon rings) could be described as the problem child of the crude oil family.  Aromatics are generally the most toxic fraction of the crude.  The majority of research into the aromatic fraction of oil has centered around the most problematic of these problem children; polycyclic aromatic hydrocarbons (PAHs), molecules with multiple carbon rings.  PAHs have the ability to hang around for a comparatively long time in water and soils (what ecotoxicologists refer to as environmental persistence) as well as within the bodies of critters exposed to crude oil (especially in their fat).

https://en.wikipedia.org/wiki/BTX_(chemistry)#/media/File:Benzene_Toluene_and_ortho-,meta-,and_para-xylene.svg

Examples of the structure of the BTEX hydrocarbons in crude oil. Image source: Wikipedia

The most abundant and well-characterized crude oil PAHs are the so-called “BTEX” molecules: Benzene, Toluene, Ethylbenzene and Xylenes.  Of these, Benzene is the most abundant and best understood.  It is often present in concentrations as high 4 g/l in crude oil and can be at levels close to 1 ppb in seawater near oil or gas seeps (IPCS 1993).  Non-petroleum, natural sources of BTEX include volcanic emissions and forest fires.  We also love to use this solvent (and the other BTEX compounds) in industrial contexts across the globe.

 

Those Poisonous PAHs

Acute toxicity (short term exposure; minutes but usually hours to days) from the BTEX PAHs is well documented upon a wide variety of aquatic critters.  In moderate concentrations, these PAHs can kill things pretty quickly, especially if we are talking about water-dwelling invertebrates (particularly when that water is stratified or relatively confined) or animals breathing in air rich with PAH vapors (such as we found on PCH in the immediate vicinity of the pipeline break on May 19).  Short of killing you, breathing in a comparatively low concentration of these things can induce dizziness, euphoria (this is why teenagers sometimes huff gasoline fumes), nausea, blurry vision and headaches.  Several of us who visited and/or drove past the Refugio spill site on May 20 experienced a rapid (within minutes) onset of headaches and nausea, most likely due to these unusually high concentration of these aromatic compounds in the air.

Chronic toxicity (long term exposure; weeks to years) from BTEX PAHs include damage to the liver, kidneys, heart, lungs, and nervous system of vertebrates.  Impacts span cancer, developmental problems, reproductive failure, endocrine disruption, and even genotoxicity (the screwing up of your genetic code).  Suffice it to say, this is all bad.  Most of these effects have been characterized in model vertebrate systems (aka lab mice and estuary-dwelling fish).  Mechanistic work on the toxicity of exposed invertebrates is getting better every year, but we still lack a good understanding of this for many species.

 

BTEX concentrations in the environment (after Leusch & Bartkow 2010)

Reported concentrations of benzene, toluene, ethylbenzene and xylene (BTEX) in air and water (in parts per billion). After Leusch & Bartkow 2010.

  Benzene Toluene Ethylbenzene Xylenes
Air (μg/m3)
Remote rural area 0.2 – 16 0.5 – 260 0.2 – 1.6 <0.1 – 3
Urban center, heavy traffic Up to 349 Up to 1,310 Up to 360 Up to 775 density
Water (ppb or μg/L)
Surface water: clean <0.1 – 2.1 <1 – 15 <0.1 – 1.8 <0.1 – 1.2
Surface water: contaminated Up to 100 unknown Up to 15 Up to 32
Groundwater: clean <0.1 – 1.8 <1 ‐ 100 <0.1 – 1.1 <0.1 – 0.5
Groundwater: contaminated Up to 330 Up to 3,500 Up to 2,000 Up to 1,340
Drinking water <0.1 – 5 <1 – 27 <1 ‐ 10 <0.1 – 12

Tar’s Toxicity: our recent Refugio oil experiments

With that long-winded preamble, the big question everyone keeps asking us is:

Is all this tar washing up on our beaches toxic?

We are working on this as we speak, but our initial results are instructive.  And the answer seems to be yes.

As I have discussed before, sandy beach-dwelling organisms are particularly at risk in this Refugio spill.  My colleagues, students, and I are now supplementing our field surveys with laboratory experiments.

We have begun to explore the toxicity of the tar landing on our SoCal beaches with our model organism for this spill: the sand crab Emerita analoga.

We have found that both weathered and comparatively fresh tar landing on our local beaches both kills and screws with the normal activity of our sand crabs.

Refugio spill tar is toxic to sand crabs<br>acute mortality

At this early stage, we can’t pinpoint the specific mechanism of toxicity.  But this tar clearly has the potential to kill our sandy beach animals.  We are working on estimates of how many might have been killed or been put at risk of being killed by this oiling of our beaches, but that will take some time.  In the meantime, we can now say that these tar balls pitter-pattering upon our beaches from Santa Barbara to Orange County over these past few weeks are clearly toxic to our local sand crabs, the cornerstones of our sandy beach food web.  This may not be the death knell to these populations, but it clearly was not a good thing for the ecology of our sandy beach ecosystem.

Refugio spill tar is toxic to sand crabs<br>sublethal effects: swimming

In other words, if you were a sand crab princess grumbling in a frustrating holding position as you impatiently waited for your turn to become the next queen, a little bit of strategically placed Refugio tar could easily hasten your ascent to the throne.

Oil Seeps 101

Tar ball strand line at the wrack line at Ventura State Beach on May 30, 2015.

Tar ball strand line at the wrack line at Ventura State Beach on May 30, 2015.

We have been getting lots of inquires about this crazy tarballing going on across Santa Barbara, Ventura, and Los Angeles Counties.  I thought I would give a quick overview of tar balls in our part of the world; the Southern California Bight.

Just-deposited fresh tar ball at Zuma Beach, Los Angeles County.  May 30, 2015.

Just-deposited fresh tar ball at Zuma Beach, Los Angeles County. May 30, 2015.

Oil Seeps In Our History

Natural sandy beach oil seep in Santa Barbara.  Image: USGS.

Natural sandy beach oil seep in Santa Barbara. Image: USGS.

Oil has been deep underground for millions of years, more or less undisturbed.  Indeed our sucking out all that stored carbon and then effectively spitting that carbon up into our atmosphere is the central driver of climate change and (what I like to call) global weirding (aka global warming).  Petroleum is mostly the product of dead plankton and plants, not so much dead dinosaurs as the popular conception normally goes (but I digress…).  Oil and gas essentially build up in porous subsurface rock formations capped by impervious rock.  This creates an oil and/or gas pocket which humans learned to tap beginning in the mid-to-late 1800s.  But long before we ever learned to stick fancy metal straws down into these hydrocarbon rock pools, that “black gold” has been naturally leaking up to the surface since these formations first formed.  These leaks or seeps happen when the overlying rock formations develop fractures or cracks in them, letting the oil or gas flow up to the surface quickly or slowly.  Seeps have played important roles in human society for thousands of years.

Chumash tomol.  Image: from www.missionscalifornia.com

Chumash tomol. Image: www.missionscalifornia.com

Our local seeps in Santa Barbara and Ventura Counties featured most prominently in Chumash culture and technology.  We have evidence of humans using seep tar at least as early as 5,000 B.C.E. with Chumash actively trading their tar with other, distant tribes for at least the past 1,000 years.  Perhaps the most iconic use of the tar seeping from the ground across our region were the Chumash ocean-going tomols.  These Chumash canoes were unusual and not constructed as a watertight vessel per se.  Instead, these vessels were constructed of planks.  Once assembled the final waterproofing included scooping up a bunch of tar from a local seep and then plastering/in-filling of any gaps between planks to create a superior seal and watertight boat.  Spanish explorer Juan Rodriguez Cabrillo was particularly impressed with this technology and noted these unique canoes in the logs of his 1542 exploration of the Ventura and Santa Barbara coasts.  Cabrillo even used Chumash tar to caulk and repair his own vessels.  Our current Chumash people are active in preserving their traditions and culture and continue to construct traditional tomols to traverse the 17+ mile gap from the mainland to our channel islands.

Chumash arrive at Santa Cruz Island in a modern Tomol.  Photo: National Park Service.

Chumash arrive at Santa Cruz Island in a modern Tomol. Photo: National Park Service.

 

Summerland oil piers near Santa Barbara, circa 1901-1903. Image: Title Insurance and Trust / C.C. Pierce Photography Collection, USC Libraries.

Summerland oil piers near Santa Barbara, circa 1901-1903. Image: Title Insurance and Trust / C.C. Pierce Photography Collection, USC Libraries.

Our first definitive confirmation of natural seeps depositing tar balls on our local beaches dates to 1772 and the journal of Padre Pedro Font (a member of Juan Bautista De Anza’s colonizing expedition).  Font noted tar balls on the beach and slow motion seeps pouring asphaltum (which is just what it sounds like) down cliffs and bluffs into the ocean.  With the European settlement of California, more modern extraction and uses of oil began to take hold.  Oil extraction was initially concentrated at and near surface seeps where the emerging tar was scooped up directly, soon to be quarried as we traditionally mine gravel or other rocks.  In those early days of the mid 1800’s, harvested tar was used principally to pave roads, fuel oil lamps, and as a lubricant for heavy machinery.  From 1870-1890 more and more oil and gas wells sprang up as settlers encountered petroleum where they had hoped to find water in their boreholes.  All heck broke loose following the first-in-the-world offshore oil production derricks (via long, wooden piers jutting out into the surf) off of Summerland in 1896.  And the rest, as we say, is history.

Summerland offshore wells near the end of the play of this nearshore reservoir.  Image: Museum of Ventura County.

Summerland offshore wells near the end of the play of this nearshore reservoir. Image: Museum of Ventura County.

An Ongoing Flow

Oil and gas seeps presents themselves both on the terrestrial surface and the ocean bottom.  Flow can be highly variable, changing with seasons, tectonic pressures, temperatures, and a myriad of factors we poorly understand.  This can complicate the source tracking when we are interested in figuring out if a tarring event or individual slick originated from a seep or a spill.

Remotely Operated Vehicle video still showsing a crab near the top of extruding tar on a tar mound in the Santa Barbara Channel. Lack of colonizing sessile organisms suggests that this mound is quite young.  Image source: Lorenson, et al. 2009.

Remotely Operated Vehicle video still showsing a crab near the top of extruding tar on a tar mound in the Santa Barbara Channel. Lack of colonizing sessile organisms suggests that this mound is quite young. Image source: Lorenson, et al. 2009.

A tarwhip extruding from an extensive tar mound offshore Pt. Conception at a water depth of 41 m. The length seen in the photo is estimated to be about 3 m. Several tar whips were observed, all extruding from tar mounds, some of which were clearly broken off, and some that did not retain buoyancy and fell to the ocean floor.

An approximately 3 m-long tarwhip extruding from an extensive tar mound offshore of Pt. Conception at a depth of 41 m. During this dive, many such tar whips were observed, all extruding from tar mounds. Some such whips broke off and floated to the surface while others did not retain buoyancy and fell to the ocean floor. Image source: Lorenson, et al. 2009.

Released oil and gas experiences a wide array of possible fates, including migration to the atmosphere, hanging out in the water column or surface layer, deposition upon the benthos, and degradation/transformation by the microbial community.

The fate of oil from a natural seep in the Santa Barbara Channel.  Image source: Woods Hole Oceanographic Institution (2009).

The fate of oil from a natural seep in the Santa Barbara Channel. Image source: Woods Hole Oceanographic Institution (2009).

Natural Oil Seeps in the Santa Barbara Channel

We have a wide range of naturally oil seeps across Ventura and Santa Barbara Counties.  Examples of known seeps and some of the resulting slicks are below.  You can also check out this killer site from the USGS documenting known seeps across California.

Southern California Bight showing possible oil slicks and seeps.  Colors coded by confidence level where green>red>pink.  Possible oil pollution slicks are seen in yellow tones.  Image source: Fugro NPA Limited satellite mapping services.

Southern California Bight showing possible oil slicks and seeps. Colors coded by confidence level where green>red>pink. Possible oil pollution slicks are seen in yellow tones. Image source: Fugro NPA Limited satellite mapping services.

 

An Ongoing Flow

One of the particular challenges with tracking surface slicks from seeps or spills revolves around the complicated surface currents and eddies we experience in the Santa Barbara Channel.  This is due to both the geography of the Santa Barbara Channel, Point Conception, and the Transverse Range.  As a result, we can get movement in virtually any direction, although we generally get migration eastward and southward during the spring and summer.   To date, the surface slick from the Refugio Oil Spill has primarily migrated offshore with two main lobes, one going more or less straight offshore and a second migrating eastward down the coast.  As of this writing, we have no direct evidence that oil from the Refugio Spill migrated any great distance.  However the tar balling of beaches in Santa Monica Bay and the Ventura coastlines might have been translocated oil from that Refugio source.  Below is an overview of the general surface flow patterns in the Santa Barbara Channel.

Dominant patterns of surface currents in the Santa Barbara Channel.

Dominant patterns of surface currents in the Santa Barbara Channel.

 

 

 

 

 

 

 

 

 

 

 

Seep or Spill?

Example tar ball chromatograms from the Santa Barbara Channel.  Image after 2009.

Example tar ball chromatograms from the Santa Barbara Channel. Chromatograms of selected tarball samples. Total ion chromatogram (TIC) of aliphatic (A) and aromatic (B) fractions; Selected ion monitoring (SIM) chromatograms of m/z 191, Hopanes (C), and m/z 217, Steranes (D,E,F). Compounds identified in Table 2-1. Legend : MAS, monoaromatic steranes; Steranes, C26 to C29 regular steranes; Hopanes, C27 to C35 regular hopanes; BN, 28,30-bisonorhopane; UCM, Unresolved Complex Mixture. 23T, C23-tricyclic terpane; C24, C25, C27, C38, tricyclic terpanes; T, triplet, defined in text; Ts and Tm, defined in text; BN, bisnorhopane; ab29, ab30, ab31 through 35 (S & R epimers), ab-hopanes with carbon numbers; O, Oleanane; and G, Gammacerane. (D, E, F) Mass chromatograms (m/z 217) of C27, C28, and C29 steranes and C27 diasteranes in a selected coastal tar residues representing Families 22, 212, and 32. Legend: S,R = epimers of aaa27, 28, 29 and bb27, 28, 29 steranes. Image after Lorenson, et al. 2009.

The only definitive way to tell if the oil presenting itself on a given beach is from a seep or from an anthropogenic release (i.e. the Refugio Spill) is via chemical forensics.  We do this by “fingerprinting” the oil.  This essentially means grabbing the oil, getting it nice and liquid-y and then running those sample through a machine that can characterize the various chemical compounds.  This analyzer can distinguish biomarkers or the “fingerprint” of amazingly complex organic compounds and the isotopes of individual carbon atoms that comprise a given oil sample.  Frequent targets that will help with distinguishing the source formation include unusually “heavy” d13C, high C35 ab-hopane 22S and 22R epimers compared to C34, and prominent sulfur-containing PAHs, such as dibenzothiophenes.  The last step is to run a sample of the candidate source oil (say from the Refugio Pipeline crude) and see if the two compounds’ peaks overlap.

Although the chemical components are common to essentially all tar balls, their relative proportions will vary with the oil sources.  The chemical “fingerprinting” should use both the ratios of these array of constituents, plus additional markers from both aliphatic and aromatic hydrocarbons (see Hostettler et al., 2004).

The chemical composition of the tarballs also sheds light on their geochemical history. Despite tons of offshore, shallow seeps, and the constant impingement of tar onto the shoreline, little is known about the mechanics of the hydrocarbon formation in the shallow seeps, specific sources of tarballs, or their transport from the marine environment onto the shore.

While not perfect, this “fingerprinting” has been used to track not only the source of oil, but look at how that material has moved across our nearshore seascape.  As we know that tar balls from offshore seeps can be transported significant distances from their sources by ocean currents, oceanographers have used tar ball source tracking to infer circulation patterns and nearshore currents.  This amounts to researchers using oil as effectively a drifter.

The worth of our Beaches

Beach volleyball was birthed on the sands of SoCal.  Pick your beach and you will be sure to find a volleyball story (or at least local gone to the NCAA or the AVP).  This compilation is mostly from the 1960s.

Beach volleyball was birthed on the sands of SoCal. Pick your beach and you will be sure to find a volleyball story (or at least local gone to the NCAA or the AVP). This compilation is mostly from the 1960s.

Sandy Beaches are everything to us here in Southern California, a central pillar of both our cultural identity and economic engine.  They are where we birthed surf culture (on beaches like Huntington and Surfrider), invented beach volleyball (on beaches like Manhattan Beach and Redondo), trained our young people to fight the axis powers of WWII (on beaches across Coronado Island and Mugu Lagoon), have filmed our entertainment for a century (on beaches like Leo Carrillo and Will Rogers), see the manifestation of climate change/sea level most clearly (at Ventura’s Surfer’s Point Beach), pump ourselves up to become the next action movie star or guvernator (this really only ever happens on Venice…check out the Jim’s killer glass if you go), stare over the tops of our sunglasses at scantily clad people (on any beach you can think of this holiday weekend) and first learned how devastating an oil spill can really be (on beaches across Ventura and Santa Barbara Counties in 1969).

Turning Mugu Beach (near the historic pier) into the South Pacific in the era of silent films, 1937.

Turning Mugu Beach (near the historic pier) into the South Pacific in the era of silent films, 1937.

Our most recent, state-wide economic data comes from a colleague (the great Dr. King) up at San Francisco State University way back in 2002 who showed that California’s sandy beaches generate about $21 billion dollars EACH YEAR (in 2002 dollars) in both direct spending and generated taxes.  That’s billion with a “b” and that probably seems more profitable than either a Presidential Election or a WholeFoods kitty-corner to a Bel-Air Yoga Studio.  In sandy beaches we’ve got an ecosystem that is part culture cauldron and part money mill.  The downside is that we don’t seem to give sandy beaches their due when it comes to doing the most minimal things we can to keep them in place and healthy.  We are more than happy to armor our coastline, pave over our dunes, dam our rivers, and stick jetties out into the sea to cutoff or otherwise screw with sand movement, the central lifeblood of our beach systems.  And each year we spend a few tens of millions of dollars on beach nourishment and other forms of beach restoration.  In the world of “Return On Investment” beaches are either a cash cow, an incredibly poorly managed part of our society’s cultural infrastructure, or both.

Sometimes folks from afar tell me that only the wealthy or powerful frequent the beaches here in SoCal.  Nothing could be further from the truth.  Every fall for the past decade, students in my ESRM 462: Coastal and Marine Management Class have conducted face-to-face surveys in Santa Barbara, Ventura, and northern Los Angeles Counties, talking to somewhere between 1,000 and 1,500 people each year.  Our CSUCI Survey of Public Opinion of Coastal Resources is (among other things) a longitudinal survey of opinions and behaviors surrounding sandy beaches.  This instrument has shown us that the vast, vast majority of us go to our sandy beaches all the time (see page 35 here or this link for our last summary of our data.  An updated publication will be out in the next few months spanning a decade of data).  For example, our most recent data from our 2014 surveys showed that when we asked folks to identify the last open space they visited this, 78% of them said “the coast” or something to that effect with 60% explicitly naming one of our local sandy beaches.  When we ask them how often we go to the beach (see below), a third of us go to the beach weekly.  If we up the timeframe, we see that two-thirds of us go monthly and essentially everybody heads out at least a few times (89%) in 2014.

 

beach visitation rates in Santa Barbara, Ventura, & LA<br><sub>2014 CUSCI Coastal Survey, n=1,242</sub>

These beach visitation rates are robust: household income has little to do with explaining this variation.  And while people living in ZIP Codes that touch the coastline are more likely to spend time at the beach, we see very high visitation rates from folks across all SoCal ZIP Codes/geographies.  Similarly, people whose first language is English are as likely to go the best as native Spanish speakers.  The beach really is a resource for us all and part of our shared Californian heritage. The ubiquity of our beaches and our high frequenting of them seems behind the almost visceral response of the public to oil spills on beaches.  I am seeing this exact phenomenon play out at the Refugio Oil Spill.  As we have been sampling our beach monitoring sites in northern Santa Barbara County these past several days, we are constantly bumping into people asking what we are doing and then telling us how angry/sorry/besides themselves they are.  They reiterate the hurt they feel and often will segue into a key beach memory or favorite beach-going activity.  It has struck me that this is very similar to what my family and friends say when we gather for a high school reunion or a wedding or a funeral. Our attachment to beaches here is deep.  This spill, regardless of the size or net ecological impact, has struck folks in their heart.  

Lets get this stuff cleaned up and restore Refugio.

We want our beaches back.