The North Pacific Subtropical Gyre (NPSG) is the largest contiguous ecosystem on earth. In oceanography, a subtropical gyre is a ring-like system of ocean currents rotating clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere caused by the Coriolis Effect. They generally form in large open ocean areas that lie between land masses.
The NPSG is the largest of the gyres as well as the largest ecosystem on our planet. Like other subtropical gyres, it has a high-pressure zone in its center. Circulation around the center is clockwise around this high-pressure zone. Subtropical gyres make up 40% of the Earth’s surface and play critical roles in carbon fixation and nutrient cycling.Poretsky, 2009 This particular gyre covers most of the Pacific Ocean and comprises four prevailing ocean currents: the North Pacific Current to the north, the California Current to the east, the North Equatorial Current to the south, and the Kuroshio Current to the west. Its large size and distance from shore has caused the NPSG to be poorly sampled and thus poorly understood.Karl, D. 1999
The life processes in open-ocean ecosystems are a sink for the atmosphere’s increasing . Gyres make up a large proportion, approximately 75%, of what we refer to as the open ocean, or the area of the ocean that does not consist of coastal areas. They are considered oligotrophic, or nutrient poor because they are far from terrestrial runoff.Corno et al, 2007 These regions were once thought to be homogenous and static habitats. However, there is increasing evidence that the NPSG exhibits substantial physical, chemical, and biological variability on a variety of time scales. Specifically, the NPSG exhibits seasonal and interannual variations in primary productivity (simply defined as the production of new plant material), which is important for the uptake of .
The NPSG is not only a sink for in the atmosphere, but also other pollutants. As a direct result of this circular pattern, gyres act like giant whirlpools and become traps for anthropogenic pollutants, such as marine debris. The NPSG has become recognized for the large quantity of plastic debris floating just below the surface in the center of the gyre. This area has recently received a lot of media attention and is commonly referred to as the Great Pacific Garbage Patch.
History of discovery The NPSG is not often sampled because of its distance from the coast and its shortage of marine life. These vast and deep ocean waters, far from the influence of land, have historically been considered the oceanic equivalent of terrestrial deserts, with low standing stocks of biomass and low production rates. This perspective is derived from a dearth of comprehensive investigation of central gyre habitats. Over the past two decades these views have been challenged with a newfound understanding of the dynamics of the NPSG.Dore et al., 2008
During the early days of marine exploration, (1872–1876), on its leg from Yokohama to Honolulu, collected plant and animal specimens as well as numerous seawater samples. The goals of this expedition were to determine the chemical composition of seawater and the organic matter in suspension and to study the distribution and abundance of various communities of organisms. The motivation for studying open ocean ecosystems has changed over time, whereas today more modern studies focus on biodiversity and the effects of climate on ecosystem dynamics. Today, the Hawaii Ocean Time-series (HOT) program has assembled the largest and most comprehensive ecological data set for the NPSG and is scheduled to continue to the next millennium. Programs like HOT have debunked the hypothesis that this ecosystem is static and homogenous, finding that the NPSG exhibits dynamic seasonal patterns separating it from other open ocean systems.
Physical characteristics
The NPSG is the largest of the open ocean habitats and is considered to be the Earth’s largest contiguous biome.(Karl et al., 2002) This great anticyclonic circulation feature extends from 15°N to 35°N latitude and from 135°E to 135°W longitude. Its surface area spans approximately 2 × 107 km2. Its western portion, west of 180° longitude, has greater physical variability than the eastern portion. This variability, where different weather patterns affect subregions differently, is due to the large dimensions of this gyre.
This large variability is caused by discrete eddies, near-inertial motions, and internal tides. Climate patterns such as the North Pacific Gyre Oscillation (NPGO), El Nino/Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO) affect the interannual variability in primary productivity in the NPSG. DiLorenzo et al., 2008 These conditions can have profound effects on biological processes within this habitat, they have the ability to shift sea surface temperature (SST), chlorophyll patterns, nutrient patterns, oxygen concentrations, mixed layer depths, and thus the carrying capacity (amount of life this habitat can carry) of the NPSG.
Nutrient cycling
Low nutrient concentrations and thus a low density of living organisms characterize the surface waters of the NPSG. The low biomass results in clear water, allowing photosynthesis to occur to a substantial depth. The NPSG is classically described as a two-layered system. The upper, nutrient-limited layer accounts for most of the primary production, supported primarily by recycled nutrients. The lower layer has nutrients more readily available, but photosynthesis is light-limited.
In open-ocean systems, biological production depends on intense nutrient recycling within the euphotic (sunlit) zone, with only a small fraction supported by the input of “new” nutrients.Hannides et al., 2009 Previously there was a perception that the NPSG was a marine desert and that “new” nutrients were not commonly added to this system. The outlook has changed, as scientists have begun to have a better understanding of this habitat. Although fairly high rates of primary production are maintained through rapid recycling of nutrients, physical processes such as internal waves and tides, cyclonic mesoscale eddies, wind-driven Ekman pumping, and atmospheric storms may carry in new nutrients.Nicholson et al., 2008
Nutrients that do not get used up on the surface will eventually sink down and nourish the seafloor habitat. The deep benthic habitats of the ocean gyres have been thought to typically consist of some of the most food-poor regions on the planet.(Shulenberger and Hessler, 1974) One of the sources of nutrients to this deep ocean habitat is marine snow. Marine snow consists of detritus, dead organic matter, which falls from the surface waters where productivity is highest and exports carbon and nitrogen from the surface mixed layer to the deep ocean. Data on the abundance of marine snow to the deep ocean floor is lacking in this large ecosystem.Pilskaln et al., 2005 However, Pilskaln et al. found that in the NPSG, marine snow was at a higher abundance than expected and were surprisingly comparable to a deep coastal upwelling system.
Higher nutrient value may be because of Rhizosolenia mats, which also play an important role in contributing to marine snow in subtropical gyres. These are generally multi-species associations of Rhizosolenia species of diatoms. This larger phytoplankton may reach up to tens of centimeters in size. These mats are particularly abundant in the NPSG. Their abundance in this ecosystem suggests a higher flux of nutrients in the NPSG than was predicted in classic theories.
While N is transported deeper by this mechanism, the surface waters are potentially cut off from this source. Nitrogen must be available for life at the surface. In order to account for this lack of nitrogen to the surface, there are organisms that are capable of nitrogen fixation in the NPSG. Trichodesmium is one species capable of nitrogen fixation that is found in many surface plankton blooms. Nitrogen fixation is the process where inert N2 is taken from the atmosphere and converted into a nitrogen compound that is available to organisms for use. In many oligotrophic marine ecosystems, nitrogen fixation is a common source of nitrogen.
Vertically migrating zooplankton can also actively transport nutrients to different zones of the water column. Zooplankton feed in the surface waters at night, and then by day release fecal pellets to the midwaters, which can transport C, N, and P to the deeper waters. In the NPSG the zooplankton community is not static but fluctuates seasonally and is dominated by copepods, euphausiids, and chaetognaths.
Recently, classic theories about the lack of nutrients in the NPSG have been disproven and new theories suggest that the ecosystem actually is dynamic and characterized by strong seasonal, interannual, and even decadal variability It has also been deemed highly sensitive to climate change, scientists have observed increases in water column stratification and decreased inorganic nutrient availability. These changes are proposed as driving mechanisms that are changing the current trend in phytoplankton community structure from eukaryotic to prokaryotic populations, as these simpler organisms can withstand lower nutrient supply. Zooplankton and phytoplankton represent less than 10% of living organisms in this region, and it is now well documented that the NPSG is a “microbial ecosystem”.
Microbial community
Microbial organisms make up the majority of the primary producers in the NPSG. They are autotrophic, meaning they capture their own “food” from sunlight and chemicals, including . These organisms comprise the base of the food chain, and thus their presence in an ecosystem is fundamental. In the NPSG, primary productivity is often described as low.
Before 1978, scientists hypothesized that diatoms dominated plankton populations in the NPSG. The primary consumers were expected to be relatively large mesozooplankton. It is now well known that most of the algae in the NPSG are actually bacteria (unicellular organisms), dominated by cyanobacteria, or blue-green algae. These simple organisms make up the majority of the standing stock of photosynthesizing marine life in this ecosystem. Scientists have also recently discovered Archaea (also a single-celled microorganism, but more similar to a eukaryote than bacteria) genes in the NPSG, suggesting that additional diversity exists in this habitat. Many microorganisms may exist in this gyre because small body size has a competitive advantage in the ocean for resource (light and nutrients) acquisition. In the contemporary view of the NPSG, the microbial food web is always present, whereas the larger eukaryote-grazer food chain is seasonal and ephemeral.
Eukaryotic plankton community
Eukaryotic plankton in the gyre is dependent on “new” nutrients coming in from physical weather patterns. The classic two-layered model discussed in previous sections considers the upper layer to be equivalent to a “spinning wheel,” with little export of nutrients because they are constantly recycled. This model does not allow for the input of new nutrients, which is problematic because this would make any rapid increase, or bloom of phytoplankton impossible. Despite ever-present nutrient limitation in the upper portion, plankton biomass and rates of primary production have considerable temporal variability and do produce blooms in the NPSG.