Craig Shesky
Analyst · Malcolm MacDonald with BofA
And that video is available in our slide deck posted on our website. For anybody that may have had video freezing issues, apologies for that. But certainly, the accumulation of baseline data over the last decade plus does represent the most comprehensive deep sea data set ever collected in the Clarion-Clipperton Zone. And it was collected in partnership with many of the world's leading marine research institutions and expert industry contractors. And this data set is generating a lot of excitement among the researchers who have truly acknowledged the rigor and the scale of this science program. This deep data is openly shared to public databases, including the ISA's DeepData library of contractor data, as well as other open-source databases like UNESCO's Ocean Biodiversity Information System, or OBIS, the world's largest catalog of marine organisms. Our environmental impact assessment has a very specific focus to assess the potential impacts of our operations on marine biodiversity and ecosystem function. To this end, our team identified 6 primary concerns related to our operations for further investigation based on discussions with stakeholders. And thanks to these efforts, a far more in-depth understanding of our expected impacts is emerging, and that contradicts much of the speculation by activists and some of the media. Off the back of our 2022 test pilot collection, we've now seen the infield observed data showing that 92% to 98% of sediment mobilized at the seafloor stays within 2 meters of the seafloor and settles locally. This finding is critically important as it addresses speculation that sediment plumes could travel tens of thousands of kilometers or could rise up 4 kilometers to the surface and impact climate change. As noted on last quarter's call, when we did a deep dive into the seafloor plume data, this is a clear example of why -- and why -- excuse me, why the speculation of opposition groups was very wrong. And in-field observed data needs to take precedence over such speculation. We've also made significant strides in assessing the impacts of noise from our test mining, and last week received a comprehensive report from HR Wallingford which outlined how the underwater noise model they have been developing predicts that impairment to the hearing of marine mammals does not occur beyond a distance of 20 meters from the nodule collection activity under the assumption that the animals can swim away. Even without that assumption, the temporary threshold shift is predicted between 20 and 1,100 meters from the mining and permanent threshold shift between 10 and 65 meters. And given that whales don't dive within thousands of meters of a planned nodule collection, we view this as very good news and confident, or very confident that noise concerns will not be a significant impediment. And while some claim that nodule collection would irreversibly destroy abyssal habitats, the reality is that such operations would result in the transformation of patches of seafloor from one habitat type that is ubiquitous in the deep sea to another. Even assuming that all current exploration contracts proceeded to production, only 0.18% of the global seafloor would be transformed in this way. And as our recent offshore campaigns to assess ecosystem recovery showed, life has begun returning to those areas most directly impacted by sediment plumes within 1 year. And several of those primary concerns I just went through are interrelated. For example, if the seafloor plume is limited, as we know it is, it also limits the potential impact on seafloor biodiversity and the relatively low amount of carbon stored in seafloor sediment. As noted above, we now know that 92% to 98% of sediment mobilized at the seafloor rises no more than a couple of meters and settles within hours or days. And as a result, there is no known pathway for this negligible amount of carbon to make its way 4 kilometers up to the surface and reach the atmosphere. And our oceans do indeed store significant amounts of carbon, but less than 5% of this carbon is contained in seafloor sediments. And despite covering almost 90% of the global ocean area, abyssal plains account for a fraction of the total carbon locked away in seafloor sediments, none of which appears to be available for microbial conversion to CO2. As the true environmental impacts of nodule collection become clear, thanks to the wealth of emerging data, activists may continue to spread misinformation, but it's going to be the actual infield observed data that matters to the adults in the room who will be making these key permitting decisions, which brings us to the regulatory update. We were very encouraged by the progress at the most recent ISA meeting in Jamaica, in line with the positive commentary on this industry's inevitability from Secretary General, Michael Lodge, to CNBC earlier this year. The current President of the ISA Council, Mr. Olav Myklebust of Norway, spoke of the substantive advancements made during the March session in his closing remarks. "I'm very pleased with the progress made by the Council. We are moving forward with the development of regulations on the exploitation of deep seabed minerals with strong environmental protection at a good pace." And as noted in our last call, the consolidated regulatory text was released in late February, signaling the transition to the final phase of mining code negotiations. And we at TMC continue to -- intend to launch our application for an exploitation contract over the NORI-D area at some point following this year's July ISA meeting. One of the key decisions on our application is the recommendation from the Legal and Technical Commission, or LTC. And the individuals at the LTC reviewed the application and are all subject matter experts. If consensus on an approval recommendation is not reached, the decision is made by simple majority vote. And if the LTC recommends approval, the Council reviews and, if acceptable, approves the recommendation. 2/3 majority of the ISA Council would be needed to overturn a positive LTC recommendation. And certainly, we expect plenty of back and forth and questions from the LTC both before and following our application. But we feel very good about our ability to have the application stand on its merits during what will be a very well thought out and thorough review process. So on to the project economics. In March 2021, AMC Consultants issued SEC Reg SK 1300 compliant initial assessment of the project economics for the NORI-D area. The initial assessments available in the Investor section of our website, as are the resource statements for both NORI-D and TOML. The initial assessment arrived in a net present value of $6.8 billion for NORI-D at the beginning of last -- excuse me, at the beginning of 2021. Running the same model solely updated for current metal prices, the net present value of NORI-D would be approximately $11.5 billion, and our current market cap would represent just about 4% of that number, despite the very significant milestones already achieved on a project less than 2 years away from expected commercial production, and still a huge discount to pure nickel or copper developers at this stage of pre-production. Now going through the financial results. In the first quarter of 2024, TMC reported a net loss of $25.2 million, or $0.08 per share, compared to TMC's net loss of $13.7 million, or $0.05 per share for the same period in 2023. The net loss for the first quarter of 2024 included exploration and evaluation expenses of $18.1 million versus $7.2 million in Q1 2023, general and administrative expenses of $6.6 million and versus $6.2 million in Q1 2023. Exploration and evaluation expenses increased by $10.9 million in the first quarter of 2024, compared to the same period in 2023. The significant increase is primarily due to an increase in mining, technological and process development of $10.5 million, specifically tied to the increased geotechnical work, which was the majority of the costs incurred this quarter for offshore campaign 8b, which concluded in February, plus some additional expenses incurred on the transportation of nodules to PAMCO's facility in Japan, and some higher personnel costs. This is partially offset by a decrease in environmental study costs, as the costs for campaign 8, which commenced in the fourth quarter of 2023, was completed in the first quarter this year. General and administrative expenses increased slightly by $0.4 million in the first quarter of 2024, compared to the first quarter of 2023. The increase is due to higher amortization of share-based comp and higher consulting fees, offset by lower legal costs. In the first quarter of 2024, the net cash used in operating activities amounted to $11.9 million, compared to $23.5 million for the first quarter of 2023. The large gap between the net loss for Q1 2024 and the net cash used in operating activities for the same period is due to share-based compensation and expenses settled with equity and some changes in working capital. Free cash flow for the first quarter of 2024 was negative $12.1 million, compared to negative $23.5 million in the first quarter of 2023. Free cash flow is a non-GAAP measure, and I point you to the non-GAAP reconciliation table included in this slide deck and on our website. Regarding the balance sheet, as at March 31, 2024, we closed the quarter with $4.0 million in cash, and as we noted, we have sufficient liquidity on hand to continue to meet our working capital and capital expenditure requirements for at least the next 12 months from today. So I'm now going to turn it back over to our Chairman and CEO, Gerard Barron, for some closing remarks, and then from that point, we will take some questions both on the phone line as well as the webcast. Gerard, back over to you.