On Aug 9, 2018, at 8:55 AM, Greg Rau <gh...@sbcglobal.net> wrote:"From undulating surface to inky black depths, Earth’s oceans are littered with the carcasses of tiny life-forms called phytoplankton that in life form the basis of the marine food chain.These microscopic ghosts contain a reservoir of carbon estimated at a staggering 662 gigatons—200 times greater than the amount stored in all living plants and animals—that could come back to haunt us if unleashed from its watery grave as planet-warming carbon dioxide.Some of the carbon-containing molecules in these plankton remnants will remain locked away for millions of years on the seafloor, but some will break down and enter the atmosphere as carbon dioxide. A huge portion will continue to circulate freely in the ocean for generations. But exactly which molecules are destined for which fate—and therefore how much of this vast carbon pool is headed for the atmosphere via ocean warming, acidification, sunlight or digestion by microbes—is an outstanding question. Answering it requires a clearer picture of the structure of the molecules that contain this carbon. An international team of scientists has now taken the first “photographs” of these molecules in an effort to start parsing that out. This first glimpse suggests that while a catastrophic breakdown and release of carbon seems unlikely, there is much left to understand about the behavior of oceanic carbon."GR - Some inexcusable errors here. Carcasses of phytoplankton do not constitute 662 Gt C, but rather dissolved organic carbon (DOC) derived from biomass (mostly marine) constitute some 700 Gt C in the ocean (IPCC 2013, Fig. 6.1). Living marine biomass is only 3 Gt. Meantime, living biomass on land is some 500 Gt C. So no way is DOC "200 times greater than the [C] amount stored in all living plants and animals". Nevertheless, we indeed need to make sure that the DOC doesn't "come back to haunt us" such as if climate change accelerates DOC respiration. For further perspective, the ocean contains 38,000 Gt C in dissolved inorganic form, dwarfing any other reservoir in contact with the atmosphere (850 Gt C). I.e it's pretty clear where nature likes to store C; shall we follow her lead or try to do something different?--
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On Aug 9, 2018, at 9:28 AM, Wil Burns <w...@feronia.org> wrote:
From: carbondiox...@googlegroups.com <carbondiox...@googlegroups.com> on behalf of Thomas Goreau <gor...@globalcoral.org>
Sent: Thursday, August 9, 2018 12:20:19 PM
To: Greg Rau
Cc: Carbon Dioxide Removal; edi...@sciam.com; alysha....@geo.uzh.ch; l...@zurich.ibm.com; Soil Age
Subject: [CDR] Ocean carbon versus land carbon sequestration
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On Aug 9, 2018, at 10:57 AM, Greg Rau <gh...@sbcglobal.net> wrote:Alysha in not a member of CDR so I'm forwarding her response to the CDR list.Greg
From: Alysha Coppola <alysha....@geo.uzh.ch>
To: Thomas Goreau <gor...@globalcoral.org>
Cc: Greg Rau <gh...@sbcglobal.net>; Carbon Dioxide Removal <carbondiox...@googlegroups.com>; "edi...@sciam.com" <edi...@sciam.com>; "l...@zurich.ibm.com" <l...@zurich.ibm.com>; Soil Age <soil...@googlegroups.com>; Chris Sciacca <c...@zurich.ibm.com>
Sent: Thursday, August 9, 2018 12:32 PM
Subject: Re: Ocean carbon versus land carbon sequestration
Hi All,I agree there are some errors, but we did not see a proof before it when out. Our paper wasn’t about decomposition of DOC with warmer temperatures, but about visualizing these compounds to give clues about it’s persistence in the ocean.Yes, I agree it should be specified that we’re talking about the dissolved organic carbon pool. These “carcasses (i.e. dead) of phytoplankton” should be explicitly stated as dissolved organic carbon, which forms the majority of phytoplankton/living biomass forms the DOC pool. But we’re talking about the same thing here. This is to have a catchy title for the general audience.The 662 Gt is from Hansel et al., 2009 paper. And the 200 times is from this paper as well-holding greater than 200x the carbon inventory of marine biomass. This is an error.I agree- and as I was quoted in the article- this carbon is ancient, and from our paper it shows that the structure might explain it’s recalcitrance in the deep ocean. With increasing temperatures, we may reimeralize some of this DOC- but not this old carbon in the deep. The temperature change hasn’t reached past 1000m, and this most recent study only found a 7 Gt decrease from temperatures of 1oC warming in labile and semi-labile pools.The labile and semi-labile pools are a small percentage of the total DOC, which is mostly refractory according to Hansell’s definition.And I agree- there’s that 4 per mil initiative to store carbon in soils.
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On Aug 9, 2018, at 2:02 PM, Margaret Torn <mst...@lbl.gov> wrote:I will chime in with two more cents, about soil C and DOC, just to clarify something:Thomas G wrote that "Dissolved organic carbon is very resistant to decomposition, it is composed of residues inedible to bacteria that lasts for thousands of years but forms slowly." Was this for soil DOC or ocean? For soil, this kind of generalization is not meaningful. DOC can be a large range of compounds. If you have to generalize, it is more generally the case DOC is the pool of soil that turns over most quickly, on order of hours - weeks. Once soil OC is sorbed to minerals or protected in aggregates, it may persist for centuries to millennia as he wrote.The question about marine biomass is not whether most of it turns over quickly. The way you would get a sink is if some fraction sinks to deeper water where it tends to persist--and if that fraction is large enough to create a large sink. I'm not saying it will sink and I'm not advocating that approach. I just wanted to point out that the fact that most near-surface ocean OC turns over quickly is not sufficient grounds for saying it won't work.Thanks
On Thu, Aug 9, 2018 at 1:57 PM, Greg Rau <gh...@sbcglobal.net> wrote:
Alysha in not a member of CDR so I'm forwarding her response to the CDR list.Greg
Cc: Greg Rau <gh...@sbcglobal.net>; Carbon Dioxide Removal <carbondioxideremoval@googlegroups.com>; "edi...@sciam.com" <edi...@sciam.com>; "l...@zurich.ibm.com" <l...@zurich.ibm.com>; Soil Age <soil...@googlegroups.com>; Chris Sciacca <c...@zurich.ibm.com>
Sent: Thursday, August 9, 2018 12:32 PM
Subject: Re: Ocean carbon versus land carbon sequestration
Hi All,I agree there are some errors, but we did not see a proof before it when out. Our paper wasn’t about decomposition of DOC with warmer temperatures, but about visualizing these compounds to give clues about it’s persistence in the ocean.Yes, I agree it should be specified that we’re talking about the dissolved organic carbon pool. These “carcasses (i.e. dead) of phytoplankton” should be explicitly stated as dissolved organic carbon, which forms the majority of phytoplankton/living biomass forms the DOC pool. But we’re talking about the same thing here. This is to have a catchy title for the general audience.The 662 Gt is from Hansel et al., 2009 paper. And the 200 times is from this paper as well-holding greater than 200x the carbon inventory of marine biomass. This is an error.I agree- and as I was quoted in the article- this carbon is ancient, and from our paper it shows that the structure might explain it’s recalcitrance in the deep ocean. With increasing temperatures, we may reimeralize some of this DOC- but not this old carbon in the deep. The temperature change hasn’t reached past 1000m, and this most recent study only found a 7 Gt decrease from temperatures of 1oC warming in labile and semi-labile pools.The labile and semi-labile pools are a small percentage of the total DOC, which is mostly refractory according to Hansell’s definition.And I agree- there’s that 4 per mil initiative to store carbon in soils.On Aug 9, 2018, at 9:20 PM, Thomas Goreau <gor...@globalcoral.org> wrote:
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On Aug 9, 2018, at 5:12 PM, Denise Ward <denis...@gmail.com> wrote:
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On Aug 10, 2018, at 3:26 AM, Robert Tulip <rtuli...@yahoo.com.au> wrote:Dear Thomas,Your claim that "the solutions to runaway global warming lie in the soil and terrestrial vegetation, not the oceans" appears to conflict with a dominant natural cooling mechanism of our planet.As I mentioned in reply to comments from Greg Rau, a paper published in Science available at Dust in the wind drove iron fertilization during ice age, found that “iron fertilization of Southern Ocean plankton can explain roughly half of the CO2 decline during peak ice ages”. This scale of impact, removing about 50 parts per million of CO2, could potentially be replicated in time frames relevant to anthropogenic climate change, especially since this increase in primary productivity due to dust also involves increased deposition of carbon to the ocean floor, as explained by Hendy.The massive increase in ocean primary productivity in the ice ages, when CO2 level fell by 100 ppm, did not produce anoxia, or the other hypothetical adverse effects that people have posited, as indicated in benthic sediments. The amount of unused nutrient in the High Nutrient Low Chlorophyll regions of the world ocean, more than sixty million square kilometres in size, is enough to significantly increase the ocean primary biomass, with likely flow-on benefits for biodiversity and cooling.Clearly there is much more need for research, especially computer modelling and field tests. The rationale is that working out the best ways to mimic the natural cooling feedback amplifiers of the ice age, for example using iron salt aerosol, could well remove more carbon than the decarbonisation plans of the Paris Accord, at a fraction of the cost and risk.Robert Tulip
From: Thomas Goreau <gor...@globalcoral.org>
To: Greg Rau <gh...@sbcglobal.net>
Cc: Carbon Dioxide Removal <carbondiox...@googlegroups.com>; "edi...@sciam.com" <edi...@sciam.com>; "alysha....@geo.uzh.ch" <alysha....@geo.uzh.ch>; "l...@zurich.ibm.com" <l...@zurich.ibm.com>; Soil Age <soil...@googlegroups.com>
Sent: Friday, 10 August 2018, 5:20
Subject: [CDR] Ocean carbon versus land carbon sequestration
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On Aug 10, 2018, at 8:56 AM, Brian Cady <brianc...@gmail.com> wrote:I thought iron limited oceanic areas totalled about 20% of the world's oceans, or 14% of the world's area"HNLC regions cover 20% of the world’s oceans and are characterized by varying physical, chemical, and biological patterns."Brian
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On Aug 14, 2018, at 7:24 AM, Charles Greene <ch...@cornell.edu> wrote:Note the following quote from the “Dust in the Wind” website that was cited:"Although Martin had proposed that purposeful iron addition to the Southern Ocean could reduce the rise in atmospheric CO2, Sigman noted that the amount of CO2 removed though iron fertilization is likely to be minor compared to the amount of CO2 that humans are now pushing into the atmosphere.”“The dramatic fertilization that we observed during ice ages should have caused a decline in atmospheric CO2 over hundreds of years, which was important for climate changes over ice age cycles,” Sigman said. “But for humans to duplicate it today would require unprecedented engineering of the global environment, and it would still only compensate for less than 20 years of fossil fuel burning.”
On Aug 10, 2018, at 6:26 AM, 'Robert Tulip' via Carbon Dioxide Removal <CarbonDiox...@googlegroups.com> wrote:
Dear Thomas,Your claim that "the solutions to runaway global warming lie in the soil and terrestrial vegetation, not the oceans" appears to conflict with a dominant natural cooling mechanism of our planet.As I mentioned in reply to comments from Greg Rau, a paper published in Science available at Dust in the wind drove iron fertilization during ice age, found that “iron fertilization of Southern Ocean plankton can explain roughly half of the CO2 decline during peak ice ages”. This scale of impact, removing about 50 parts per million of CO2, could potentially be replicated in time frames relevant to anthropogenic climate change, especially since this increase in primary productivity due to dust also involves increased deposition of carbon to the ocean floor, as explained by Hendy.The massive increase in ocean primary productivity in the ice ages, when CO2 level fell by 100 ppm, did not produce anoxia, or the other hypothetical adverse effects that people have posited, as indicated in benthic sediments. The amount of unused nutrient in the High Nutrient Low Chlorophyll regions of the world ocean, more than sixty million square kilometres in size, is enough to significantly increase the ocean primary biomass, with likely flow-on benefits for biodiversity and cooling.Clearly there is much more need for research, especially computer modelling and field tests. The rationale is that working out the best ways to mimic the natural cooling feedback amplifiers of the ice age, for example using iron salt aerosol, could well remove more carbon than the decarbonisation plans of the Paris Accord, at a fraction of the cost and risk.Robert Tulip
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Sent: Friday, 10 August 2018, 5:20
Subject: [CDR] Ocean carbon versus land carbon sequestration
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