Whale feces

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"Whale pump" - the role played by whales in nutrient recycling in the oceans (based on Fig. 1 of Roman & McCarthy (2010) ) WhalePump.jpg
"Whale pump" the role played by whales in nutrient recycling in the oceans (based on Fig. 1 of Roman & McCarthy (2010) )

Whale feces, the excrement of whales, has a vital role in the ecology of oceans, [2] earning whales the title of "marine ecosystem engineers." This significant ecological role stems from the nutrients and compounds found in whale feces, which have far-reaching effects on marine life.

Contents

Nitrogen and iron chelate released by cetacean species offer significant benefits to the marine food chain and contribute to long-term carbon sequestration. Additionally, whale feces contains a wealth of information about the health, natural history, and ecology of individual animals or groups. This source of information includes DNA, hormones, toxins, and various other chemicals. Studying whale feces provides valuable insights into the lives of these marine creatures, aiding scientists in understanding their behaviors, diets, and overall well-being. Furthermore, the nutrients released through whale feces play a vital role in marine ecosystems, supporting phytoplankton growth, enhancing the food chain, and contributing to the overall health of the oceans.

In addition to feces, the digestive system of sperm whales produces ambergris, a solid, waxy, flammable substance of a dull grey or blackish color which can be found floating on the sea or washed up on the coast. [3]

Description

Whales excrete plumes of liquid feces that are flocculent in nature, consisting of loose aggregations of particles. [2] [4] These feces, often found floating on the sea surface after being excreted underwater before it dissociates, contain undigested hard objects such as squid beaks. [2] [5] Fecal samples are characterized by color, odor, texture, and buoyancy, providing valuable information about the health and ecology of whales. [6] Flatulence has been recorded in whales. [5]

Ecological significance

Whales transport more nitrogen through their feces in the Gulf of Maine than all of the rivers in that system combined.

Briana Abrahms [7]

Nutrient cycling and carbon sequestration

One of the crucial roles of whale feces is in nutrient cycling, particularly nitrogen circulation in the ocean. Whales transport more nitrogen through their feces in certain regions than all the rivers combined, enriching both primary and secondary productivity. Additionally, the iron-rich feces of krill-eating whales encourage phytoplankton growth, benefiting the marine food chain and sequestering carbon dioxide for extended periods. The Southern Ocean, rich in nutrients but iron-deficient, experiences increased phytoplankton blooms due to whale feces, acting as a significant carbon sink.

The phenomenon of whales defecating near the water's surface reverses the typical flow of nutrients in the ocean's biological pump, contributing to the "whale pump." Whales feed at deeper levels where krill is found, and their fecal matter, rich in iron, rises to the surface. This action enhances phytoplankton productivity and supports fish populations. Whales, along with krill, form a positive feedback loop, where their populations contribute to the recycling of iron, further boosting phytoplankton growth.

A study in the Gulf of Maine extrapolated from modern levels nitrogen recycling in the sea due to marine mammals, such as cetaceans and seals, prior to the advent of commercial culling, estimating a former level thrice that of supply of nitrogen fixed from the atmosphere. Even today, despite reduction of marine mammal populations and increase in nitrogen uptake from the atmosphere and nitrogen pollution, the local clustering of marine mammals plays a significant role in maintaining the productivity in the regions they frequent. [1] The enrichment is not only in primary productivity but also secondary productivity in the form of abundance in fish populations. [2]

The study assumes that whales tend to defecate more commonly in the upper part of the water column, which they frequent for breathing; additionally the feces tend to float. Whales feed at deeper levels of the ocean where krill is found. [1] The fecal action of whales thus reverses the usual flow of nutrients of the ocean's "biological pump" due to the downward flow of "marine snow" and other detritus from surface to bottom. The phenomenon has been termed the "whale pump". [2]

The Gulf of Maine study also found that the view of whales and other marine mammals as competitors for fishing, advocated by some nations, is incorrect as whales play a vital role in maintaining the productivity of phytoplankton and consequently the fish. Culling marine mammal populations threatens the nutrient supply and the productivity of fishing grounds. [2]

In addition, the feces of krill-eating whales is rich in iron. [5] The release of iron from whale feces encourages the growth of phytoplankton in the sea, [5] which not only benefits the marine food chain, but also sequesters carbon for long periods of time. [5] When phytoplankton, which is not consumed in its lifetime, perishes, it descends through the euphotic zone and settles down into the depths of sea. Phytoplankton sequesters an estimated 2 billion tons of carbon dioxide into the ocean each year, causing the ocean to become a sink of carbon dioxide which holds an estimated 90% of all sequestered carbon. [8] The Southern Ocean is amongst the largest ranges for phytoplankton and has the characteristic of being nutrient-rich in terms of phosphate, nitrate and silicate, while it is iron-deficient at the same time. [9] Increases of nutrient iron results in blooming of phytoplankton. Whale feces is up to 10 million times richer in iron than the surrounding sea water and plays a vital role in providing the iron required for maintaining phytoplankton biomass on the earth. [9] The iron defecation of just the 12,000 strong sperm whale population in the Southern Ocean results in the sequestration of 200,000 tonnes of atmospheric carbon per year. [9]

A study of the Southern Ocean found that whales not only recycled iron concentrations vital for phytoplankton, but also formed, along with krill, a major source of sequestered iron in the ocean, up to 24% of the iron held in the surface waters of Southern Ocean. Whales formed part of a positive feedback loop and if whale populations are allowed to recover in the Southern Ocean, greater productivity of phytoplankton will result as larger amounts of iron are recycled through the system. [10]

Accordingly, whales are referred to as "marine ecosystem engineers". [11]

A study conducted in the Fernando de Noronha Archipelago of the southwest Atlantic Ocean, revealed the feces and vomit of Spinner dolphins (Stenella longirostris) formed part of the diet of twelve species of reef fish from seven different families. The most prolific consumer was the black triggerfish or black durgon (Melichthys niger), which could even discern the postures dolphins assumed prior to voiding and positioned themselves for effective feeding. All these offal eating fish species are recorded plankton eaters and it is considered that this type of feeding may represent a change in its usual diet, i.e. drifting plankton. [12]

Whales, along with other large animals, play a significant role in the transport of nutrients in global ecological cycles. Population reduction of whales and other large animals has severely affected the efficacy of pump mechanisms which transport nutrients from the deep sea to the continental shelves. [13]

Whale feces as indicators of health and ecology

Nitrogen release by cetacean species [1]
SpeciesNitrogen excreted
(kg/day)
Baleen whales
Right whale 15.9
Humpback whale 9.42
Fin whale 15.0
Sei whale 8.32
Minke whale 2.94
Toothed whales
Pilot whale 0.036
Atlantic white-sided dolphin 0.15
Common dolphin 0.09
Harbour porpoise 0.05

Whale feces contain DNA, hormones, toxins and other chemicals which can give information on a number of aspects of the health, natural history and ecology of the animal concerned. Feces have also provided information on the bacteria present in the gastro-intestinal tract of whales and dolphins.

Indicator for diet composition

A 2016 research study used fecal analysis of wild orcas, which spent the summer season in the Salish Sea, for quantitively estimation of prey species. The analysis was consistent with earlier estimates based on surface prey remains. The study found that salmonids comprised over 98.6% of the identified genetic sequences with Chinook and Coho salmon species as the most important prey species. [14]

As indicator for population decline

A research study, published in 2012, on impacts of overfishing and maritime traffic on a wild population of the Southern Resident Killer Whales of the western seaboard of North America, was based on the chemical analysis of fecal specimens of orcas. The study aimed to find out the reasons for orca decline for which three causes were hypothesized - disturbance by boats and ships, lack of food, and, long-term exposure of toxins which accumulate in whale fat, namely DDT, PBDT and PCB. [15]

Fecal samples of orca were detected with the help of a trained spotter dog, a black labrador retriever, named "Tucker", from a firm Conservation Canines. The dog could detect fresh scat from orcas while following in a boat 200 to 400 meters (660 to 1,310 ft) behind a pod of orcas. Fecal samples collected were tested for the presence and quantity of DNA, as well as stress, nutrition and reproductive hormones, and toxins such as PBDE, PCB, and DDT congeners. [16]

The fecal samples were analyzed over time and co-related to boat densities over time and the quantity of Fraser River Chinook salmon, the main constituent of orca diet in those regions. Boat densities and the salmon abundance over time were estimated independently. [16] Glucocorticoids in orcas rise when the animal faces psychological tension or starvation. The study found that prey is maximum in August, at which time, boats are most abundant. Conversely, the availability of salmon was minimum in late fall when the level of marine boat traffic was also the least. Glucocorticoid levels were highest in the fall when there was a shortage of prey and maximum during August at the height of availability of food. [16]

Similarly, thyroid hormones co-relate to nutritional stress, enabling animals to lower metabolism rates to better conserve declining nutrition. The Southern Resident Killer Whales arrive in the study area in spring after having fed on salmons from early spring spawning on other rivers when their thyroid hormone levels are highest. The hormone levels decline as the animals arrive in the study area, plateau during the time of fish availability and decline further during the period of nutritional scarcity. [16] The toxin analysis was ongoing at the time of publication of research. So far, presence of congeners of the three toxins in whale feces are found to be proportionate to the levels of these chemicals measured in samples of orca flesh during biopsy. The results indicate that restoring the abundance and quality of available prey is an important first measure to restoring orca populations in the area under study. [16]

Biodiversity indicator

An analysis of feces of two dolphin and one whale species led to the discovery of a new species of Helicobacter, namely Helicobacter cetorum , the bacteria being associated with clinical symptoms and gastritis in the cetaceans. [17]

See also

Related Research Articles

<span class="mw-page-title-main">Blue whale</span> Baleen whale, largest animal ever known

The blue whale is a marine mammal and a baleen whale. Reaching a maximum confirmed length of 29.9 m (98 ft) and weighing up to 199 t, it is the largest animal known ever to have existed. The blue whale's long and slender body can be of various shades of greyish-blue on its upper surface and somewhat lighter underneath. Four subspecies are recognized: B. m. musculus in the North Atlantic and North Pacific, B. m. intermedia in the Southern Ocean, B. m. brevicauda in the Indian Ocean and South Pacific Ocean, and B. m. indica in the Northern Indian Ocean. There is a population in the waters off Chile that may constitute a fifth subspecies.

<span class="mw-page-title-main">Cetacea</span> Infraorder of mammals

Cetacea is an infraorder of aquatic mammals belonging to the order Artiodactyla that includes whales, dolphins and porpoises. Key characteristics are their fully aquatic lifestyle, streamlined body shape, often large size and exclusively carnivorous diet. They propel themselves through the water with powerful up-and-down movement of their tail which ends in a paddle-like fluke, using their flipper-shaped forelimbs to maneuver.

<span class="mw-page-title-main">Orca</span> Largest living species of dolphin

The orca, or killer whale, is a toothed whale and the largest member of the oceanic dolphin family. It is the only extant species in the genus Orcinus and is recognizable by its black-and-white patterned body. A cosmopolitan species, they are found in diverse marine environments, from Arctic to Antarctic regions to tropical seas.

<span class="mw-page-title-main">Plankton</span> Organisms living in water or air that are drifters on the current or wind

Plankton are the diverse collection of organisms that drift in water but are unable to actively propel themselves against currents. The individual organisms constituting plankton are called plankters. In the ocean, they provide a crucial source of food to many small and large aquatic organisms, such as bivalves, fish, and baleen whales.

<span class="mw-page-title-main">Whale</span> Informal group of large marine mammals

Whales are a widely distributed and diverse group of fully aquatic placental marine mammals. As an informal and colloquial grouping, they correspond to large members of the infraorder Cetacea, i.e. all cetaceans apart from dolphins and porpoises. Dolphins and porpoises may be considered whales from a formal, cladistic perspective. Whales, dolphins and porpoises belong to the order Cetartiodactyla, which consists of even-toed ungulates. Their closest non-cetacean living relatives are the hippopotamuses, from which they and other cetaceans diverged about 54 million years ago. The two parvorders of whales, baleen whales (Mysticeti) and toothed whales (Odontoceti), are thought to have had their last common ancestor around 34 million years ago. Mysticetes include four extant (living) families: Balaenopteridae, Balaenidae, Cetotheriidae, and Eschrichtiidae. Odontocetes include the Monodontidae, Physeteridae, Kogiidae, and Ziphiidae, as well as the six families of dolphins and porpoises which are not considered whales in the informal sense.

<span class="mw-page-title-main">Phytoplankton</span> Autotrophic members of the plankton ecosystem

Phytoplankton are the autotrophic (self-feeding) components of the plankton community and a key part of ocean and freshwater ecosystems. The name comes from the Greek words φυτόν, meaning 'plant', and πλαγκτός, meaning 'wanderer' or 'drifter'.

<span class="mw-page-title-main">Zooplankton</span> Heterotrophic protistan or metazoan members of the plankton ecosystem

Zooplankton are the heterotrophic component of the planktonic community, having to consume other organisms to thrive. Plankton are aquatic organisms that are unable to swim effectively against currents. Consequently, they drift or are carried along by currents in the ocean, or by currents in seas, lakes or rivers.

<span class="mw-page-title-main">Marine mammal</span> Mammals that rely on marine environments for feeding

Marine mammals are mammals that rely on marine (saltwater) ecosystems for their existence. They include animals such as cetaceans, pinnipeds, sirenians, sea otters and polar bears. They are an informal group, unified only by their reliance on marine environments for feeding and survival.

<span class="mw-page-title-main">Biological pump</span> Carbon capture process in oceans

The biological pump (or ocean carbon biological pump or marine biological carbon pump) is the ocean's biologically driven sequestration of carbon from the atmosphere and land runoff to the ocean interior and seafloor sediments. In other words, it is a biologically mediated process which results in the sequestering of carbon in the deep ocean away from the atmosphere and the land. The biological pump is the biological component of the "marine carbon pump" which contains both a physical and biological component. It is the part of the broader oceanic carbon cycle responsible for the cycling of organic matter formed mainly by phytoplankton during photosynthesis (soft-tissue pump), as well as the cycling of calcium carbonate (CaCO3) formed into shells by certain organisms such as plankton and mollusks (carbonate pump).

<span class="mw-page-title-main">Toothed whale</span> Parvorder of cetaceans

The toothed whales are a clade of cetaceans that includes dolphins, porpoises, and all other whales with teeth, such as beaked whales and the sperm whales. 73 species of toothed whales are described. They are one of two living groups of cetaceans, the other being the baleen whales (Mysticeti), which have baleen instead of teeth. The two groups are thought to have diverged around 34 million years ago (mya).

<span class="mw-page-title-main">Filter feeder</span> Animals that feed by straining food from water

Filter feeders are aquatic animals that acquire nutrients by feeding on organic matters, food particles or smaller organisms suspended in water, typically by having the water pass over or through a specialized filtering organ that sieves out and/or traps solids. Filter feeders can play an important role in condensing biomass and removing excess nutrients from the local waterbody, and are therefore considered water-cleaning ecosystem engineers. They are also important in bioaccumulation and, as a result, as indicator organisms.

<span class="mw-page-title-main">Cape Cod Bay</span> Large bay of the Atlantic Ocean adjacent to the U.S. state of Massachusetts

Cape Cod Bay is a large bay of the Atlantic Ocean adjacent to the U.S. state of Massachusetts. Measuring 604 square miles (1,560 km2) below a line drawn from Brant Rock in Marshfield to Race Point in Provincetown, Massachusetts, it is enclosed by Cape Cod to the south and east, and Plymouth County, Massachusetts, to the west. To the north of Cape Cod Bay lie Massachusetts Bay and the Atlantic Ocean. Cape Cod Bay is the southernmost extremity of the Gulf of Maine. Cape Cod Bay is one of the bays adjacent to Massachusetts that give it the name Bay State. The others are Narragansett Bay, Buzzards Bay, and Massachusetts Bay.

<span class="mw-page-title-main">Cetology</span> The study of whales, dolphins, porpoises, and other cetaceans

Cetology or whalelore is the branch of marine mammal science that studies the approximately eighty species of whales, dolphins, and porpoises in the scientific infraorder Cetacea. Cetologists, or those who practice cetology, seek to understand and explain cetacean evolution, distribution, morphology, behavior, community dynamics, and other topics.

High-nutrient, low-chlorophyll (HNLC) regions are regions of the ocean where the abundance of phytoplankton is low and fairly constant despite the availability of macronutrients. Phytoplankton rely on a suite of nutrients for cellular function. Macronutrients are generally available in higher quantities in surface ocean waters, and are the typical components of common garden fertilizers. Micronutrients are generally available in lower quantities and include trace metals. Macronutrients are typically available in millimolar concentrations, while micronutrients are generally available in micro- to nanomolar concentrations. In general, nitrogen tends to be a limiting ocean nutrient, but in HNLC regions it is never significantly depleted. Instead, these regions tend to be limited by low concentrations of metabolizable iron. Iron is a critical phytoplankton micronutrient necessary for enzyme catalysis and electron transport.

<span class="mw-page-title-main">Iron fertilization</span> Ecological concept

Iron fertilization is the intentional introduction of iron-containing compounds to iron-poor areas of the ocean surface to stimulate phytoplankton production. This is intended to enhance biological productivity and/or accelerate carbon dioxide sequestration from the atmosphere. Iron is a trace element necessary for photosynthesis in plants. It is highly insoluble in sea water and in a variety of locations is the limiting nutrient for phytoplankton growth. Large algal blooms can be created by supplying iron to iron-deficient ocean waters. These blooms can nourish other organisms.

<span class="mw-page-title-main">Ocean fertilization</span> Type of climate engineering

Ocean fertilization or ocean nourishment is a type of technology for carbon dioxide removal from the ocean based on the purposeful introduction of plant nutrients to the upper ocean to increase marine food production and to remove carbon dioxide from the atmosphere. Ocean nutrient fertilization, for example iron fertilization, could stimulate photosynthesis in phytoplankton. The phytoplankton would convert the ocean's dissolved carbon dioxide into carbohydrate, some of which would sink into the deeper ocean before oxidizing. More than a dozen open-sea experiments confirmed that adding iron to the ocean increases photosynthesis in phytoplankton by up to 30 times.

<span class="mw-page-title-main">Planktivore</span> Aquatic organism that feeds on planktonic food

A planktivore is an aquatic organism that feeds on planktonic food, including zooplankton and phytoplankton. Planktivorous organisms encompass a range of some of the planet's smallest to largest multicellular animals in both the present day and in the past billion years; basking sharks and copepods are just two examples of giant and microscopic organisms that feed upon plankton.

<span class="mw-page-title-main">Lipid pump</span>

The lipid pump sequesters carbon from the ocean's surface to deeper waters via lipids associated with overwintering vertically migratory zooplankton. Lipids are a class of hydrocarbon rich, nitrogen and phosphorus deficient compounds essential for cellular structures. This lipid carbon enters the deep ocean as carbon dioxide produced by respiration of lipid reserves and as organic matter from the mortality of zooplankton.

<span class="mw-page-title-main">Viral shunt</span>

The viral shunt is a mechanism that prevents marine microbial particulate organic matter (POM) from migrating up trophic levels by recycling them into dissolved organic matter (DOM), which can be readily taken up by microorganisms. The DOM recycled by the viral shunt pathway is comparable to the amount generated by the other main sources of marine DOM.

<span class="mw-page-title-main">Marine food web</span> Marine consumer-resource system

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